IODA-MED

Transcription

IODA-MED

Compte-rendu de
fin de projet
Projet ANR-11-BS56-005
IODA-MED
Programme Blanc2011
A
B
IDENTIFICATION .............................................................. 2
RESUME CONSOLIDE PUBLIC ................................................ 2
B.1
B.2
B.3
C
Instructions pour les résumés consolidés publics ....................... 2
Résumé consolidé public en français ........................................ 3
Résumé consolidé public en anglais.......................................... 5
MEMOIRE SCIENTIFIQUE ..................................................... 7
C.1
C.2
C.3
C.4
C.5
C.6
C.7
C.8
Résumé du mémoire .............................................................. 8
Enjeux et problématique, état de l’art ...................................... 8
Approche scientifique et technique ........................................... 9
Résultats obtenus ................................................................ 10
Exploitation des résultats...................................................... 13
Discussion .......................................................................... 13
Conclusions......................................................................... 14
Références.......................................................................... 14
D LISTE DES LIVRABLES .......................................................15
E IMPACT DU PROJET ..........................................................17
E.1
E.2
E.3
E.4
Indicateurs d’impact ............................................................ 17
Liste des publications et communications................................ 18
Liste des éléments de valorisation.......................................... 30
Bilan et suivi des personnels recrutés en CDD (hors
stagiaires) .......................................................................... 32
Ce document est à remplir par le coordinateur en collaboration avec les partenaires du projet. L’ensemble des
partenaires doit avoir une copie de la version transmise à l’ANR.
Ce modèle doit être utilisé uniquement pour le compte-rendu de fin de projet.
Référence du formulaire : ANR-FORM-090601-01-01
A IDENTIFICATION
Acronyme du projet
Titre du projet
Coordinateur du projet
(société/organisme)
Période du projet
(date de début – date de fin)
Site web du projet, le cas échéant
IODA-MED
Innovative Observing and Data Assimilation
systems for severe weather in the Mediterranean
Evelyne Richard
Laboratoire d’Aérologie, CNRS & Université de
Toulouse
1 Octobre 2011
30 Septembre 2015
http://mesonh.aero.obs-mip.fr/mesonh/iodamed/
Rédacteur de ce rapport
Civilité, prénom, nom
Téléphone
Adresse électronique
Date de rédaction
Mme Evelyne Richard
05 61 33 27 64
[email protected]
01/03/2015
Si différent du rédacteur, indiquer un contact pour le projet
Civilité, prénom, nom
Téléphone
Adresse électronique
Liste des partenaires présents à la
fin du projet (société/organisme et
responsable scientifique)
1. Laboratoire d’Aérologie (LA), E. Richard
2. Groupe d’étude de l’Atmosphère
Météorologique (GAME), V. Ducrocq
3. Laboratoire Atmosphères, Milieux,
Observations Spatiales (LATMOS), C. Flamant
B RESUME CONSOLIDE PUBLIC
Ce résumé est destiné à être diffusé auprès d’un large public pour promouvoir les résultats du projet, il ne fera donc
pas mention de résultats confidentiels et utilisera un vocabulaire adapté mais n’excluant pas les termes techniques. Il
en sera fourni une version française et une version en anglais. Il est nécessaire de respecter les instructions ci-dessous.
B.1 INSTRUCTIONS POUR LES RESUMES CONSOLIDES PUBLICS
Les résumés publics en français et en anglais doivent être structurés de la façon suivante.
Titre d’accroche du projet (environ 80 caractères espaces compris)
Titre d’accroche, si possible percutant et concis, qui résume et explicite votre projet selon une logique grand public : il
n’est pas nécessaire de présenter exhaustivement le projet mais il faut plutôt s’appuyer sur son aspect le plus
marquant.
Les deux premiers paragraphes sont précédés d’un titre spécifique au projet rédigé par vos soins.
Titre 1 : situe l’objectif général du projet et sa problématique (150 caractères max espaces compris)
Paragraphe 1 : (environ 1200 caractères espaces compris)
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Le paragraphe 1 précise les enjeux et objectifs du projet : indiquez le contexte, l’objectif général, les problèmes traités,
les solutions recherchées, les perspectives et les retombées au niveau technique ou/et sociétal
Titre 2 : précise les méthodes ou technologies utilisées (150 caractères max espaces compris)
Paragraphe 2 : (environ 1200 caractères espaces compris)
Le paragraphe 2 indique comment les résultats attendus sont obtenus grâce à certaines méthodes ou/et technologies.
Les technologies utilisées ou/et les méthodes permettant de surmonter les verrous sont explicitées (il faut éviter le
jargon scientifique, les acronymes ou les abréviations).
Résultats majeurs du projet (environ 600 caractères espaces compris)
Faits marquants diffusables en direction du grand public, expliciter les applications ou/et les usages rendus possibles,
quelles sont les pistes de recherche ou/et de développement originales, éventuellement non prévues au départ.
Préciser aussi toute autre retombée= partenariats internationaux, nouveaux débouchés, nouveaux contrats, start-up,
synergies de recherche, pôles de compétitivités, etc.
Production scientifique et brevets depuis le début du projet (environ 500 caractères espaces compris)
Ne pas mettre une simple liste mais faire quelques commentaires. Vous pouvez aussi indiquer les actions de
normalisation
Illustration
Une illustration avec un schéma, graphique ou photo et une brève légende. L’illustration doit être clairement lisible à
une taille d’environ 6cm de large et 5cm de hauteur. Prévoir une résolution suffisante pour l’impression. Envoyer
seulement des illustrations dont vous détenez les droits.
Informations factuelles
Rédiger une phrase précisant le type de projet (recherche industrielle, recherche fondamentale, développement
expérimental, exploratoire, innovation, etc.), le coordonnateur, les partenaires, la date de démarrage effectif, la durée du
projet, l’aide ANR et le coût global du projet, par exemple « Le projet XXX est un projet de recherche fondamentale
coordonné par xxx. Il associe aussi xxx, ainsi que des laboratoires xxx et xxx). Le projet a commencé en juin 2006 et a
duré 36 mois. Il a bénéficié d’une aide ANR de xxx € pour un coût global de l’ordre de xxx € »
B.2 RESUME CONSOLIDE PUBLIC EN FRANÇAIS
Suivre impérativement les instructions ci-dessus.
LA PREVISION DES PRECIPITATIONS MEDITERRANEENNES INTENSES
Un verrou majeur : une mauvaise connaissance des conditions atmosphériques dans
l’environnement marin
En automne, les pourtours de la Méditerranée occidentale sont régulièrement exposés à des
épisodes de précipitations intenses et des phénomènes de crues éclairs. Des efforts
considérables ont été réalisés ces dernières années pour en améliorer la prévision et des
progrès significatifs ont pu être obtenus grâce au développement de modèles numériques à
haute résolution, permettant de partiellement résoudre les nuages convectifs. Malgré ces
progrès, la précision des précipitations prévues demeure encore insuffisante pour qu’elles
soient efficacement utilisées par les systèmes de prévisions des crues qui en zone de relief
sont particulièrement sensibles à de faibles erreurs de localisation spatiale. Parmi les
différents facteurs limitant la prévisibilité des événements de précipitations intenses (HPE),
les incertitudes relatives à l’état initial des modèles jouent un rôle majeur. Ceci est d’autant
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plus vrai pour les systèmes Méditerranéens dont les précurseurs amont se développent en
mer, dans des régions sous échantillonnées par les systèmes d’observations opérationnels. Le
projet IODA-MED visait à améliorer la prévisibilité des HPEs grâce à la réduction des
incertitudes pesant sur les états initiaux des modèles
La campagne HyMeX 2012 : des observations inédites pour mieux comprendre et mieux
prévoir
Afin de mieux comprendre et mieux prévoir les situations de HPE, IODA-MED a proposé i)
de renforcer les systèmes d’observations existants en collectant des observations
supplémentaires et non conventionnelles dans l’environnement marin amont des HPE, ii) de
mieux exploiter les observations existantes en accroissant le nombre observations introduites
dans le système d’assimilation, iii) d’explorer le potentiel offert par l’assimilation de
nouveaux types d’observations, et particulièrement de celles liées au cycle de l’eau et iv) de
faire progresser la qualité du système d’assimilation en améliorant son adaptation aux fines
échelles. IODA-MED s’intègre dans le cadre du programme de recherche international
HyMeX dédié à l’étude du cycle hydrologique en Méditerranée. Il a constitué une
contribution majeure à la première phase d’observations intensives (HyMeX-SOP1)
organisée à l’automne 2012 et consacrée à l’étude des précipitations intenses et des crues
éclairs. IODA-MED a bénéficié d’un contexte de fortes collaborations tant nationales
qu’internationales.
Résultats majeurs
Parmi les nombreux résultats du projet, nous soulignerons
- la construction de la première base de données regroupant l’ensemble des paramètres
atmosphériques pertinents pour l’étude des précipitations intenses dans la région
méditerranéenne.
- l’amélioration du système d’assimilation du modèle opérationnel de prévision du temps
de Météo-France grâce à une meilleure exploitation des observations de routine ainsi
qu’à la prise en compte d’observations non standard
- la démonstration que cette amélioration se traduit par de meilleures prévisions des
précipitations intenses
- une meilleure compréhension des processus physiques associés aux épisodes de fortes
précipitations et l’identification de ceux qui sont encore mal représentés dans les
modèles.
Production scientifique
Le projet a donné lieu à 28 publications dans les meilleures revues de la discipline et plus
d’une centaine de communications à des conférences internationales. Cet effort s’est
accompagné de diverses actions de valorisation ; deux articles dans des journaux grand
public, des conférences de presse ainsi que de nombreuses communications dans les media
(radio, TV, web).
Illustration
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Simulation numérique de l’épisode de pluie intense du 24/09/2012. Le système convectif (iso-volume
20 dBZ de pseudo réflectivité radar coloré en fonction de l’altitude) se développe sur le Massif Central.
Il est alimenté dans les basses couches par un flux d’air marin très humide (en gris-bleu, rapport de
mélange > 14g/kg). Au pied des Cévennes, la convergence des vents marins (lignes de courant en
jaune) se combine au soulèvement orographique pour déclencher la convection.
Informations factuelles
Le projet ANR-11-BS56-005 intitulé IODA-MED est principalement un projet de recherche
fondamentale.
Ses résultats sont toutefois susceptibles d’impacter les activités
opérationnelles des services météorologiques. Ce projet a regroupé trois partenaires : le
Laboratoire d’Aérologie (LA, UPS/CNRS, coordinateur), le Laboratoire Atmosphères,
Milieux, Observations Spatiales (LATMOS, UPMC/UVSQ/CNRS ) et le Groupe d’étude de
l’Atmosphère Météorologique (CNRM-GAME, Météo-France/CNRS) Le projet a débuté le
1er Octobre 2011 et s’est déroulé sur une période de 48 mois. Le financement de l’ANR s’est
monté à 648 398€ pour un coût total de 7 084 269 €.
B.3 RESUME CONSOLIDE PUBLIC EN ANGLAIS
Suivre impérativement les instructions ci-dessus.
FORECASTING HEAVY PRECIPITATION EVENTS IN THE MEDITERRANEAN
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A major issue: The inaccurate knowledge of atmospheric conditions in the upstream
marine environment
During the autumn, the western Mediterranean often suffers heavy precipitation, flooding,
and devastating flash-floods. Considerable efforts have been made in recent years to
improve the skill of the forecasts for such severe events and significant progress was
obtained thanks to the development of high-resolution convection permitting models (CPM).
However, society’s demands for predictive quality still remain largely unsatisfied and more
accuracy is required, in terms of amount, timing, and location of rainfall. Among the various
factors limiting the predictability of heavy precipitation events (HPE), uncertainties in model
initial states play a major role. This is particularly true for the Mediterranean systems for
which upwind precursors often develop offshore in maritime areas under-sampled by the
operational observation networks. The central objective of IODA-MED was to improve HPE
predictability by reducing the uncertainties on the initial state of the model.
The 2012 HyMex field campaign : a unique data set for better understanding and better
forecasting
To better understand and better forecast HPEs IODA-MED proposed i) to collect additional
and non-conventional observations in the marine upwind environment of the HPEs ii) to
make better use of routinely available observations in the mesoscale data assimilation
systems iii) to explore the potential of assimilating new observation types, especially
observations related to the water cycle, and iv) to advance the quality of the mesoscale data
assimilation systems. IODA-MED was a major contribution to the first intensive observing
phase of HyMeX, HyMeX SOP1, organized in autumn 2012 and devoted to the study of
intense precipitation and flash floods. IODA-MED took advantage of the strong national and
international cooperation developed in the wider context of HyMeX
Major results
Some highlights of the project:
- the construction of the first data base which gathers all the atmospheric parameters
relevant for the study of heavy precipitation in the Mediterranean area.
- the improvement of the assimilation system of the operational numerical weather
prediction model of Météo-France thanks to a better use of routine observations and the
use of additional non-standard observations
- the demonstration that this improvement leads to better precipitation forecasts
- a better understanding of the physical processes involved in heavy rain episodes and
the identification of those which are still ill-represented in the models
Scientific production
The project resulted in 28 peer-reviewed publications, most of them in partnership, and more
than 100 communications at international conferences. This effort was accompanied by
various valorisation activities: two articles in journals for the general public, contributions to
press-conferences and many communications in the media (radio, TV, web).
Illustration
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Numerical simulation of the 24/09/2012 heavy precipitation event. The convective system (20 dBZ
pseudo-radar reflectivity iso-volume colored as a function of height) develops over the Massif Central.
It is fed in by marine moist low-level inflow (in grey, water vapor mixing ratio >14g/kg). Convection
triggers at the foothill of the Cévennes where convergence of marine flows (streamlines in yellow)
combines with orographic lifting.
Fact sheet
The ANR-11-BS56-005 project, entitled IODA-MED is primarily a fundamental research
project. However its results may impact the operational activities of weather services. Three
partners were involved in the project: Laboratoire d’Aérologie (LA, UPS/CNRS, coordinator),
Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS, UPMC/UVSQ/CNRS ),
and Groupe d’étude de l’Atmosphère Météorologique (CNRM-GAME, Météo-France/CNRS)
The project started in October 2011 and lasted for a period of 48 months. The ANR funding
was 648 398€ for a total cost of 7 084 269 €.
C MEMOIRE SCIENTIFIQUE
Maximum 5 pages. On donne ci-dessous des indications sur le contenu possible du mémoire. Ce mémoire peut être
accompagné de rapports annexes plus détaillés.
Le mémoire scientifique couvre la totalité de la durée du projet. Il doit présenter une synthèse auto-suffisante rappelant
les objectifs, le travail réalisé et les résultats obtenus mis en perspective avec les attentes initiales et l’état de l’art. C’est
un document d’un format semblable à celui des articles scientifiques ou des monographies. Il doit refléter le caractère
collectif de l’effort fait par les partenaires au cours du projet. Le coordinateur prépare ce rapport sur la base des
contributions de tous les partenaires. Une version préliminaire en est soumise à l’ANR pour la revue de fin de projet.
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Un mémoire scientifique signalé comme confidentiel ne sera pas diffusé. Justifier brièvement la raison de la
confidentialité demandée. Les mémoires non confidentiels seront susceptibles d’être diffusés par l’ANR, notamment
via les archives ouvertes http://hal.archives-ouvertes.fr.
Mémoire scientifique confidentiel : non
C.1 RESUME DU MEMOIRE
Ce résumé peut être repris du résumé consolidé public.
C.2 ENJEUX ET PROBLEMATIQUE, ETAT DE L’ART
Présenter les enjeux initiaux du projet, la problématique formulée par le projet, et l’état de l’art sur lequel il s’appuie.
Présenter leurs éventuelles évolutions pendant la durée du projet (les apports propres au projet sont présentés en C.4).
The Mediterranean area concentrates the major natural risks related to the water cycle,
including heavy precipitation and flash-flooding during the autumn. Our ability to predict
such high-impact events remains weak because of the contribution of very fine-scale
processes and their non-linear interactions with the larger scale processes. Advances in the
identification of the predominant processes and particularly of their interactions at the
different scales are indispensable if these events are to be forecast better and uncertainties on
the prediction of their evolution (e.g. frequency, intensity) in the future climate reduced.
These issues are of primary importance not only to provide a tangible basis for early warning
procedures and mitigation measures designed to avoid loss of life and reduce damage, but
also to assess their impacts on the terrestrial and marine ecosystems, some of which may be
irreversible.
A unique opportunity to improve our capabilities to predict these high-impact weather
events is provided by HyMeX (Hydrological cycle in Mediterranean Experiment, Drobinski
et al, 2014). HyMeX, initially instigated by the French community, is an international
research programme aiming at a better quantification and understanding of the water cycle
in the Mediterranean with a strong emphasis on intense events. A key component of this
programme is a field experiment which monitors all relevant atmospheric, oceanic, and
hydrological variables at different time scales. The observational strategy is built upon
nested periods of observations ranging from 10 years (LOP, Long Observing Period, still ongoing), during which the existing observational networks is enhanced, to a few months
(SOPs, Special Observing Periods) corresponding to the deployment of additional observing
systems. HyMeX SOP1 took place in autumn 2012 and focussed on the heavy precipitation
events (HPEs) of the western Mediterranean basin (Ducrocq et al, 2014).
During the autumn, the western Mediterranean often suffers heavy precipitation, flooding,
and devastating flash-floods. Daily precipitation above 200 mm is not rare during this
season, in some cases reaching values as exceptional as the 700 mm recorded in September
2002 during the Gard catastrophe in France. These torrential rain episodes can occur all
along the western Mediterranean coasts including in northern Africa (e.g. Algiers in
November 2001) but are more frequently observed in north eastern Spain, south eastern
France and northern Italy. Large amounts of precipitation can accumulate over periods of
several days in which frontal disturbances are slowed down and strengthened by the relief,
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but huge rainfall totals can also be recorded in less than a day when a mesoscale convective
system (MCS) stays over the same area for several hours. Whereas the large scale
environment propitious to heavy precipitation is relatively well known, the mechanisms
responsible for the anchoring of the precipitation system over a specific area are still poorly
understood. Furthermore, the conditions which occasionally transform a severe event into an
exceptional one remain to be elucidated.
Considerable efforts have been made in recent years to improve the skill of the forecasts for
such severe events and significant progress was obtained thanks to the development of highresolution convection permitting models (CPM). However, society’s demands for predictive
quality still remain largely unsatisfied and more accuracy is required, in terms of amount,
timing, and location of rainfall. The following explanations are commonly put forward to
explain the limited skill of Numerical Weather Prediction (NWP) models: i) inaccuracy of
initial and/or boundary conditions, ii) inappropriate representation of some physical
processes or their interaction, iii) intrinsic limitations on the predictability of atmospheric
flows. The details and relative weight of each contribution remain to be investigated and are
a central issue of HyMeX. However, at the mesoscale there is a corpus of recent studies (e.g.
Khairoutdinov and Randall, 2003, Aksoy et al., 2009, Stensrud and Gao, 2010) stressing the
crucial role of initial condition uncertainties.
C.3 APPROCHE SCIENTIFIQUE ET TECHNIQUE
The IODA-MED objective was to improve the HPE predictability by reducing the
uncertainties of the model initial state. This was achieved i) by collecting additional and
non-conventional observations in the marine upwind environment of the HPEs, ii) by
making better use of routinely available observations in the mesoscale data assimilation
systems, iii) by exploring the potential of assimilating new observation types, especially
observations related to the water cycle, and iv) by advancing the quality of the mesoscale
data assimilation systems
Preliminary studies have shown that the upwind initial state uncertainties are a particularly
crucial issue for the HPEs affecting the north-western Mediterranean. In this area, the
situations conducive to heavy precipitation occur when a deep upper-level trough or closed
cyclone is located just west of the threat area and generates a southerly to easterly flow
which transports the warm moist air masses from the Mediterranean Sea towards the coasts.
The properties and characteristics of the upwind marine low-level flow are essential to
determine the strength, timing and precise location of the subsequent precipitation at the
coast. However, descriptions of the upwind environment are strongly hampered by the
scarcity of meteorological observations in maritime areas. Collecting and assimilating denser
observations of this sensitive feature were one of the most challenging tasks of the first
HyMeX SOP.
Further improvement could be expected from including in the data assimilation systems
observations that are not or are only sub-optimally taken into account operationally, such as
the observations from cloudy or precipitating areas. Quite frequently, the MCSs that affect
north western Mediterranean coasts come into existence offshore and their precursors can be
9/33
detected early in the satellite and radar imagery. However, the true potential of these remote
sensing data had hardly been exploited so far owing to inadequate assimilation techniques.
Data assimilation for the new generation of convective-scale weather prediction models,
where kilometre-scale resolution permits explicit simulation of deep moist convection, is
indeed a new area of research. The non-linearity of cloud processes and the complexity of
microphysical parameterizations raise several issues with respect to the traditional data
assimilation schemes: both background and observational errors are currently poorly
understood at convective scales and, for hydrometeors, the linearization of the related
observation operators is far from straightforward. Moreover, alternative data assimilation
algorithms may be needed and, considering the probabilistic nature of the predictive
problem, ensemble-based methods appear attractive. Experience was very scarce and there
was a strong need for new methods and/or new combinations of observations to be explored.
The IODA-MED project focused on the HyMeX activities which were carried out in terms of
observing and assimilation systems in the French community. However, it is clear that
IODA-MED was part of a much wider effort, which includes other national and international
HyMeX components. At the national level, HyMeX is strongly supported by CNRS/INSU
and Météo-France through the MISTRALS programme. At the international level, HyMeX
has been endorsed by the Joint Scientific Committee of the World Weather Research Program
(WWRP) promoting worldwide research focused on improving the accuracy, lead time and
utilization of weather prediction. HyMeX research on the global hydrological cycle and
prediction of its evolution with climate change is carried out under the umbrella of the
GEWEX and CORDEX programs of the World Climate Research Program (WCRP).
C.4 RESULTATS OBTENUS
Positionner les résultats par rapports aux livrables du projet et aux publications, brevets etc. Revisiter l’état de l’art et
les enjeux à la fin du projet.
Besides the coordination activity (Task1), the project was structured into four main tasks.
Task 2 dealt with the observations which were collected during the HyMeX SOP1. Task 3
was dedicated to the observation operators, the purpose of which was to express
observations and model outputs in a similar space. These operators were a pre-requisite for
the assimilation but also provided the relevant tools for verification. The implementation of
the assimilation based on new observation types was performed within Task 4. This task also
ensured the production of real time analyses and forecasts that provided the necessary
guidance for the field operations. Finally, Task 5 was in charge of the data visualization
platform and data base. These four tasks were coordinated by a small group of people who
also ensured the coordination with the HyMeX International Steering Science Committee
and working groups.
Task 2: Observing systems
The observing strategy designed to tackle the broad scientific objectives of HyMeX called for
complementary surface-based, airborne and space-borne observations. The observing
systems key to this proposal were a subset of a much larger instrumental detachment (see
Ducrocq et al, 2014 for an exhaustive description) and were intended to provide a collection
10/33
of non-standard observations both (i) over the Mediterranean Sea in order to monitor
relevant moisture/wind conditions upstream of HPE regions and (ii) in the stratiform parts
of convective storms.
IODA-MED contribution to the experimental set up comprised the operation of: (i) four wind
profiler radars installed in Corsica, Eastern Pyrenees, and in the Rhône valley, (ii) a ground
based water vapour lidar installed in Menorca, (iii) the two SAFIRE (Service des Avions
Français Instrumentés pour la Recherche en Environnement) research aircraft: the ATR 42
equipped with the airborne water vapour lidar LEANDRE 2, and the FALCON 20 equipped
with microphysics probes and the airborne RASTA radar, and (iv) a Lightning Mapping
Array (LMA) belonging to New Mexico Tech and deployed in the Cévennes area.
The SOP1 field campaign which took place from 5 September to 6 November 2012 was quite
successful (Ducrocq et al, 2014). Out of 16 Intensive Observing Periods, 11 were dedicated to
HPEs and allowed collecting an unprecedented data set of HPEs occurring in Spain, France
and Italy. In total, the ATR 42 and FALCON 20 flew 26 and 19 missions respectively. All the
IODA-MED data have been processed, quality-checked and are included in the data base
(see Ducrocq et al, 2014; Bousquet et al 2015; and Defer et al, 2015 for a comprehensive
description of the collected observations).
Besides the intrinsic value of each data set (illustrated for instance in Chazette et al, 2016a
and b for the water vapour lidars, Saïd et al, 2016 for the wind profilers), the synergy
between the different instruments allowed high-value-added products to be derived. For
instance, the combination of the F20 in situ microphysical data together with the airborne
RASTA radar and ground based radar observations provided information over the full
spectrum of hydrometeors, from primary ice crystals to large raindrops or hailstones
(Ribaud et al, 2016a). Similarly, combining LMA and radar-derived microphysical data
Ribaud et al, 2016b show that lightning initiation and propagation mostly occur in media
characterized by the presence of graupel. Within Task 2, a large effort was also devoted to
instrument calibration and validation through several instrument inter-comparisons (e.g. Di
Girolamo et al, 2016, Bousquet et al., 2016, Bock et al, 2016, Chazette et al, 2014a, 2016a).
Task 3: Observing operators and verification
The aim of Task 3 was to provide accurate and efficient observation operators for use in both
data assimilation and forecast verification. A series of non standard foreword operators
have been developed. These include ground-based and airborne lidar water vapour mixing
ratio, wind profiler reflectivity, radar refractivity (Caumont et al, 2013), polarimertic radar
variables (Augros et al, 2016), lightning variables (Pinty et al, 2013, Lagouvardos et al, 2013),
radiometer-derived moisture (Caumont et al, 2016), and brightness temperature from the
Microwave Humidity Sounder (MHS, Rysman et al, 2016) In addition, a methodology was
developed to take into account in the assimilation scheme the cloud-affected Infra-red
Atmospheric Sounding Interferometer (IASI) radiances which are operationally discarded
(Martinet et al, 2014).
The forward operators were extensively used in the forecast verification and model
validation. They allowed specific model deficiencies and/or limits to be identified. For
11/33
instance, the operators developed for the polarimetric radar variables indicate that the model
reproduces fairly well the vertical distribution of the mean variables but not their variability.
They also reveal the weakness of the current microphysical scheme to accurately represent
the hydrometeors properties within the melting layer (Augros et al, 2016). Another
interesting result was established using different MHS water vapour channels. Thanks to the
appropriate operators, Rysman et al, 2016 highlight that very deep convection (ie convection
associated with tropopause over shooting) is fairly well detected by cloud permitting
models but remains strongly underestimated.
Task 4: Assimilation and forecast
In Task 4, a major effort was the development of the AROME-WMED forecast system,
similar to the operational AROME system but with a larger domain extending further
southward to cover the whole western Mediterranean and with a longer forecast range (48h).
Furthermore, in the AROME-WMED assimilation the spatial density of the microwave
satellite observations was increased together with the number of the number of GPS
observations. Additional observations such as Spanish surface data and temperature and
wind from the CNES constant level balloons were also included. AROME-WMED ran in
real-time for 8 months from 1 September 2012 onwards. Its outputs were essential to
conduct SOP1 and prepare the flight missions. A thorough assessment of the real time
AROME-WMED performance can be found in Fourrié et al, 2015.
The same modelling system was used to perform a reanalysis and reforecast of the SOP1
period. It now includes all the additional observations: ground-based Lidar water vapour
observations in Candillargues and a Menorca , ii) airborne Lidar LEANDRE II water vapour
observations along the SAFIRE/ATR42 flight tracks, iii) high-resolution radiosoundings from
operational sites in France and Spain and HyMeX -dedicated radiosoundings launched
during SOP1 over France and Italy, iv) dropsondes observations launched from SAFIRE/F20
and in-situ observations from the three research aircraft (SAFIRE/ATR42 and F20,
KIT/DO128), v) reprocessed wind profiler observations, vi) reprocessed delays from more
than 1000 GPS receivers over France, Spain, Portugal and Italy, vi) radar data from six
AEMET operational radars over Spain, vii) additional sea surface temperature observations
from ship and Argo floats. Systematic comparisons carried out for the entire SOP1 indicate
that the re-forecast significantly outperforms the real-time forecast. Moreover, data denial
experiments, for which one of the above-listed dataset was removed from the reanalysis,
clearly show the benefit of assimilating high-resolution radiosonde data instead of the
operational raw radiosonde observations, and to a lesser extent the benefit of assimilating the
Spanish radar data and the LEANDRE II data, respectively. Due to the huge amount of
reprocessed data, the production of the reanalysis took longer than anticipated. Results
appear very promising and although not totally finalized yet many more publications are on
the way.
In parallel, several studies focused on the data assimilation system itself and in particular on
the modelling of background errors. One way to add flow dependency to the background
errors is to make use of ensemble of assimilations with a large number of members in order
to diagnose the statistical structure of background errors at the convective scale for several
high precipitating events. Recent results show that precipitating areas match non-Gaussian
12/33
behaviour of the errors (Legrand et al., 2016). Another aim of these experiments was to
develop and to implement optimal filtering methods that remove sampling noise from these
covariances, using either spatial smoothing or localization (Ménétrier et al., 2015).
Task 5: Visualization platform and data base
The
data
visualization
platform
(http://sop.hymex.org/)
and
data
base
(http://mistrals.sedoo.fr/HyMeX/) are not specific to the IODA-MED observations as they
allow to display and download all HyMeX observations, respectively. The ANR support
was essential to achieve this goal. Both products are widely used by the international
HyMeX community (more than 500 hundred registered users and more than 1000 data
requests per year). It is clear that the observations will continue to be used much longer after
the end of the project. The data base – being one of the most comprehensive data sets of
heavy precipitation events at the mid-latitudes - is a very unique product.
C.5 EXPLOITATION DES RESULTATS
IODA-MED being primarily a fundamental research project, high priority was given to
publications and communications at the international level. So far, 28 peer-reviewed
publications were (or are to the point of being) published and more than 100
communications were given in international workshops or conferences. A main achievement
for the project visibility will be the publishing of a HYMEX-SOP1 special issue in the
Quarterly Journal of the Royal Meteorological Society (QJRMS), in which roughly half of the
papers are related to the IODA-MED activities.
C.6 DISCUSSION
Discussion sur le degré de réalisation des objectifs initiaux, les verrous restant à franchir, les ruptures, les
élargissements possibles, les perspectives ouvertes par le projet, l’impact scientifique, industriel ou sociétal des
résultats.
The expected results of IODA-MED– as listed in the proposal - were the following:
• the acquisition of a comprehensive data set that will provide an accurate description
of the atmospheric state prior to and during an HPE event, which should lead to
o better understanding of the interaction of the physical mechanisms leading to
HPE
o decisive advances in HPE forecasting
o better understanding and quantification of the forecast errors associated with
the uncertainties of the model initial state
• a significant improvement of the AROME data assimilation system that will benefit
both the operational meteorological service and the academic research community;
• lessons for designing and optimizing future observing networks by identifying and
prioritizing the most valuable observations;
• a strengthening of the international cooperation in the field of mesoscale data
assimilation and more fruitful exchanges between the meteorological centres and
academic research;
• a contribution to the reinforcement of European cooperation around the climatic
issues in the Mediterranean area.
13/33
Most of these expected results were put in concrete form beyond our expectation. Significant
progress was made in the understanding of HPEs in the north-western Mediterranean. As
anticipated, forecast errors can be significantly reduced through more accurate initial
conditions in the marine environment. In particular, the crucial role of convergence lines for
the triggering of convection off shore was clearly evidenced. Although their monitoring is
not straightforward with current observing systems, the forecast could greatly benefit from
space-borne, high-frequency, and high-resolution low-level wind and moisture observations.
The positive impact of assimilating high-resolution radiosonde observations could have
more immediate impact on the observational strategy, especially when most of the
meteorological centres tend to reduce the number of their operational soundings. Finally,
among the many international collaborations developed within HyMeX, our exchanges with
New Mexico Tech were particularly fruitful and led to the permanent deployment of a
Lightning Mapping Array in Corsica.
C.7 CONCLUSIONS
Parmi les nombreux résultats du projet, nous retiendrons
- la construction de la première base de données regroupant l’ensemble des paramètres
atmosphériques pertinents pour l’étude des précipitations intenses dans la région
méditerranéenne.
- l’amélioration du système d’assimilation du modèle opérationnel de prévision du temps
de Météo-France grâce à une meilleure exploitation des observations de routine ainsi
qu’à la prise en compte d’observations non standard
- la démonstration que cette amélioration se traduit par de meilleures prévisions des
précipitations intenses
- une meilleure compréhension des processus physiques associés aux épisodes de fortes
précipitations et l’identification de ceux qui sont encore mal représentés dans les
modèles.
Enfin nous soulignerons le rôle structurant de IODA-MED qui a permis de faire émerger
nouveaux projets collaboratifs régionaux (par exemple CRUE-SIM portant sur les
inondations du bassin de la Têt), nationaux (par exemple les projets ANR MUSIC et
EXAEDRE traitant respectivement des processus physiques et électriques au sein des nuages
convectifs) et internationaux (par exemple le projet de « Innovative Training Network »
NeWPHY récemment soumis à l’Europe).
C.8 REFERENCES
14/33
D LISTE DES LIVRABLES
Quand le projet en comporte, reproduire ici le tableau des livrables fourni au début du projet. Mentionner l’ensemble
des livrables, y compris les éventuels livrables abandonnés, et ceux non prévus dans la liste initiale.
M1=October 2011
Date de
livraison
N°
Task 1
M4
M16
1A
1B
M30
M24
1C
1D
Task 2
M21
2A
M21
2B
M21
2C
M21
2D
M21
2E
M21
2F
M30
2G
M30
2H
Titre
Nature (rapport,
logiciel, prototype,
données, …)
Partenaires
(souligner le
responsable)
Kick-off meeting
Post-SOP
meeting
Work progress
Publication
Milestone
Milestone
1-2-3
1-2-3
Report
Article
1-2-3
1-2-3
Data set from
Minorca
supersite
Data set from
Corsica
supersite
Data set from
ship
of
opportunity
LEANDRE 2 lidar
data set (ATR
42)
RASTA radar &
microphysics
data
set
(FALCON)
LMA & lightning
data set
Improved
knowledge
of
mesocale
moisture
and
dynamics
features
over
the sea relevant
for HPE
Improved
knowledge
of
the interactions
between
physical/radiativ
e properties of
ice
particles
with
the
dynamics within
Data
3
Data
1
Data
3
Data
3
Data
3
Data
1
Data analysis
3
Data analysis
3
Commentaires
et/ou Principales
Publications
associées )
Ducrocq et al,
La
Météorologie,
2013
Ducrocq et al,
BAMS, 2014
Chazette et al,
QJRMS, 2016a,
b
Duffourg et al,
QJRMS, 2016
Flaounas et al,
QJRMS, 2016
15/33
Date de
livraison
N°
M30
2I
Task 3
M20
3A
M20
3B
M20
3C
M20
3D
M20
3E
M20
3F
M20
3G
M30
NEW
Task 4
M1
4A1
M6
4A2
M9/11
4A3
4A4
M21
4A5
M28
4A6
Titre
stratiform
clouds
Improved
knowledge
of
the interactions
between
ice
microphysics
and
the
electrical
activity
Nature (rapport,
données, …)
Partenaires
(souligner le
responsable)
Commentaires
et/ou Principales
Publications
associées )
Data analysis
1
Software
1-2
Software
2
Software
2
Augros et al.,
QJRMS, 2016
Software
2
Caumont et al,
BLM, 2013
Software
2
Martinet et al,
ASL, 2014
Software
1,2
Lagouvardos et
al, AR, 2013
Software
1,2
Rysman et al,
QJRMS, 2016
Software
2
Caumont at al,
QJRMS, 2016
AROME-WMED
baseline version
AROME-WMED
Real
time
version
Software
2
Software
2
SOP1 Real time
analysis
and
forecasts
Verification
of
real
time
forecasts
First Reanalysis
Data
2
Report
2
Data
2
Lidar
water
vapor operator
Wind
profiler
reflectivity
operator
Dual
Polarization
Radar operator
Radar
refractivity
operator
Operators
for
satellite
radiances
contamined by
clouds and land
surface
Operators
for
lightning
observations
Additional
operators
for
satellite-bases
verification
Radiometer
derived
moisture
operator
Defer
et
al
AMT, 2015
Ribaud et al
QJRMS, 2016
Fourrié et
GMD, 2015
al,
16/33
Date de
livraison
N°
pending
4A7
M18
4B1
M12/14
4B2
M12/14
4B3
Abandon
ed
4B4
Abandon
ed
4B5
M4
5A
M11/16
5B
M20
5C
M32
5D
Titre
Reforecasts
Forecat
verification
Ballon data in
AROME-WMED
ZTD GPS data
in
AROMEWMED
Additional radar
data in AROMEWMED
Report on the
processing
of
the
European
radar data
Table
of
the
operational RS
moisture bias
Nature (rapport,
données, …)
Publication
Partenaires
(souligner le
responsable)
Commentaires
et/ou Principales
Publications
associées )
2
Data
Software
Data
Software
&
2
&
2-3
Data
Software
&
2
Report
2
Report
2
Not necessary
Bias
greatly
reduced
with
new sondes
Project web site
Website
1-2-3
http://mesonh.
aero.obsmip.fr/mesonh/
iodamed/
List of the data
to be archived
List of archived
data
List of archived
data (update)
Report
1-2-3
Report
1
Report
1
E IMPACT DU PROJET
Ce rapport rassemble des éléments nécessaires au bilan du projet et plus globalement permettant d’apprécier l’impact
du programme à différents niveaux.
E.1 INDICATEURS D’IMPACT
Nombre de publications et de communications (à détailler en E.2)
Comptabiliser séparément les actions monopartenaires, impliquant un seul partenaire, et les actions multipartenaires
résultant d’un travail en commun.
Attention : éviter une inflation artificielle des publications, mentionner uniquement celles qui résultent directement
du projet (postérieures à son démarrage, et qui citent le soutien de l’ANR et la référence du projet).
Publications
multipartenaires
International
Revues à comité de
lecture
Ouvrages ou chapitres
d’ouvrage
Communications
(conférence)
Publications
monopartenaires
14
14
43
65
17/33
France
Actions de
diffusion
lecture
d’ouvrage
Communications
(conférence)
Articles vulgarisation
1
Conférences
vulgarisation
Autres
1
1
2
1
8
Autres valorisations scientifiques (à détailler en E.3)
Ce tableau dénombre et liste les brevets nationaux et internationaux, licences, et autres éléments de propriété
intellectuelle consécutifs au projet, du savoir faire, des retombées diverses en précisant les partenariats éventuels. Voir
en particulier celles annoncées dans l’annexe technique).
Nombre, années et commentaires
(valorisations avérées ou probables)
Brevets internationaux
obtenus
Brevet internationaux en
cours d’obtention
Brevets nationaux obtenus
Brevet nationaux en cours
d’obtention
Licences d’exploitation
(obtention / cession)
Créations d’entreprises ou
essaimage
Nouveaux projets
collaboratifs
Colloques scientifiques
MUSIC (ANR Blanc 2014, funded), CRUE-SIM (RTRA STAE,
funded), SOLID (CNES, funded), EXAEDRE (ANR Blanc 2016,
pending), NeWPHI (EU ITN, pending),
- 9th HyMeX Workshop, 21-25 September 2015, Mykonos, Greece
- Integrated Regional Climate Modelling workshop, 20-23 January
2015, Toulouse, France
- 8th 8HyMeX Workshop, 15-18 Sep. 2014, Valetta, Malta
- 7th HyMeX Workshop, 7-10 October 2013, Cassis, France
- HyMeX SOPs' debriefing workshop, 15-17 April 2013, Toulouse,
France
- 6th HyMeX workshop, 7-10 May 2012, Primosten, Croatia
Autres (préciser)
E.2 LISTE DES PUBLICATIONS ET COMMUNICATIONS
Répertorier les publications résultant des travaux effectués dans le cadre du projet. On suivra les catégories du premier
tableau de la section Erreur ! Source du renvoi introuvable. en suivant les normes éditoriales habituelles. En ce qui
concerne les conférences, on spécifiera les conférences invitées.
Liste actualisée 02/2016
Bien que directement liées à IODA-MED les références en rouge ont par inadvertance
omis de citer explicitement IODA-MED. Elles sont indiquées pour mémoire mais ne sont
pas comptabilisées dans les indicateurs d’impact.
Liste des publications multipartenaires (résultant d’un travail mené en commun)
18/33
lecture
1.
2.
3.
4.
International
5.
6.
7.
8.
9.
Ducrocq, V., I. Braud, S. Davolio, R. Ferretti, C. Flamant,
A. Jansa, N. Kalthoff, E. Richard, I. Taupier-Letage, P.-A.
Ayral, S. Belamari, A. Berne, M. Borga, B. Boudevillain, O.
Bock, J.-L. Boichard, M.-N. Bouin, O. Bousquet, C. Bouvier,
J. Chiggiato, D. Cimini, U. Corsmeier, L. Coppola P.
Cocquerez, E. Defer, J. Delanoë, P. Di Girolamo , A.
Doerenbecher, P. Drobinski, Y. Dufournet, N. Fourrié, J. J.
Gourley, L. Labatut, D. Lambert, J. Le Coz, F. S. Marzano,
G. Molinié, A. Montani, G. Nord, M. Nuret, K. Ramage, B.
Rison, O. Roussot, F. Said, A. Schwarzenboeck, P. Testor, J.
Van Baelen, B. Vincendon , M. Aran, J. Tamayo: 2013,
HyMeX-SOP1, the field campaign dedicated to heavy
precipitation and flash flooding in the northwestern
Mediterranean. Bull. Amer. Meteor. Soc., 1083-1099, 2014.
Lagouvardos, K., V. Kotroni, E. Defer, and O. Bousquet,
Study of a heavy precipitation event over southern France,
in the frame of HYMEX project: Observational analysis and
model results using assimilation of lightning, Atmos. Res.
134, 45–55, 2013.
Bousquet, O. A. Berne, J. Delanoe, Y. Dufournet, J.J.
Gourley, J. Van-Baelen, C. Augros, L. Besson, B.
Boudevillain, O. Caumont, E. Defer, J. Grazioli, D. J.
Jorgensen, P.-E. Kirstetter, J-F.Ribaud, J. Beck, G. Delrieu,
V. Ducrocq, D. Scipion, A.Schwarzenboeck and J. Zwiebel,
Multiple-frequency radar observations collected in southern
France during the field phase of the Hydrometeorological
cycle in the Mediterranean Experiment (HYMEX). Bull. Amer.
Meteor. Soc., 96, 267-282, 2015.
Defer, E., J.-P. Pinty, S. Coquillat, J.-M. Martin, S. Prieur, S.
Soula, E. Richard, W. Rison, P. Krehbiel, R. Thomas, D.
Rodeheffer, C. Vergeiner, F. Malaterre, S. Pedeboy, W.
Schulz, T. Farges, L.-J. Gallin, P. Ortéga, J.-F. Ribaud, G.
Anderson, H.-D. Betz, B. Meneux, V. Kotroni, K.
Lagouvardos, S. Roos, V. Ducrocq, O. Roussot, L. Labatut
and G. Molinié, An overview of the lightning and
atmospheric electricity observations collected in Southern
France during the HYdrological cycle in Mediterranean
EXperiment (HyMeX), SOP1, Atm. Mea. Tech., 8, 649-669,
2015.
Soula, S. E. Defer, M. Füllekrug, O. van der Velde, J.
Montanya, O. Bousquet, J. Mlynarczyk, S. Coquillat, J.-P.
Pinty, W. Rison, P.R. Krehbiel, R. Thomas and S. Pedeboy.
Time and space correlation between sprites and their parent
lightning flashes for a thunderstorm observed during the
HyMeX campaign. J. Geophys. Res. Atmos., 120, 11,552–
11,574, 2015.
Ribaud, J-F., Bousquet, O., Coquillat, S., Al-Sakka, H.,
Lambert, D., Ducrocq, V. and Fontaine, E. Evaluation and
application of hydrometeor classification algorithm outputs
inferred from multi-frequency dual-polarimetric radar
observations collected during HyMeX. Quart. J. Roy. Meteor.
Soc. DOI: 10.1002/qj.2589 (early view).
Rysman, J.-F., Claud, C., Chaboureau, J.-P., Delanoë, J. and
Funatsu, B. M. Severe convection in the Mediterranean from
microwave observations and a convection-permitting model.
Quart. J. Roy. Met. Soc. DOI:10.1002/qj.2611 (early
view)
Chazette, P., C. Flamant, X. Shang, J. Totems, J.-C. Raut,
A. Doerenbecher, V. Ducrocq, N. Fourrié, O. Bock, A.
Dorenbecher and S. Cloché, 2016: Multi-instrument and
multi-model assessment of atmospheric moisture variability
over the Western Mediterranean during HyMeX, Q. J. Roy.
Met. Soc. (early view).
Duffourg, F., O. Nuissier, V. Ducrocq, C. Flamant, P.
Chazette, J. Delano, A. Doerenbecher, N. Fourrié, P. Di
Girolamo, C. Lac, D. Legain, M. Martinet, F. SaId and O.
Bock. Offshore deep convection initiation and maintenance
during I0P16a Offshore deep convection initiation and
maintenance during HyMeX IOP 16a heavy precipitation
event. Quart. J. Roy. Met. Soc. DOI: 10.1002/qj. 2725
(early view)
19/33
10. Khodayar, S., G. Fosser, S. Berthou, S. Davolio, P.
Drobinski, V. Ducrocq, R. Ferretti, M. Nuret, E. Pichelli, E.
Richard and O. Bock A seamless weather-climate multimodel intercomparison on the representation of a high
impact weather event in the Western Mediterranean:
HyMeX IOP12. Quart. J. Roy. Met. Soc. , DOI:
10.1002/qj.2700 (early view)
11. Bousquet O., J. Delanoë and S. Bielli. Evaluation of 3D wind
observations inferred from the analysis of airborne and
ground-based radars during HyMeX SOP-1. DOI:
10.1002/qj.2710 (early view)
12. Di Girolamo, P., C. Flamant , M. Cacciani , E. Richard , V.
Ducrocq , D. Summa , D. Stelitano , N. Fourrié , F. Saïd Di
Girolamo. Observation of low-level wind reversals in the
Gulf of Lion area and their impact on the water vapour
variability. Quart. J. Roy. Met. Soc. (early view)
13. Saïd, F., B. Campistron, H. Delbarre, G., Canut, A
Doerenbecher, P. Durand, N. Fourrié, D. Lambert, and D.
Legain. Offshore winds obtained from a network of wind
profiler radars during HyMeX. Quart. J. Roy. Met. Soc.
(accepted)
14. Ribaud J.-F. O. Bousquet, and S. Coquillat. Relationships
between total lightning activity, microphysics, and
kinematics during the 24 September 2012 HyMeX bow echo
system. Quart. J. Roy. Met. Soc. (accepted).
15. Pinty, J.-P., C. Barthe, E. Defer, E. Richard, and M. Chong,
Explicit simulation of electrified clouds: from idealized to
real case studies, Atmos. Res., 123, 82-92, 2013.
16. Bock, P. Bosser, R. Pacione, M. Nuret, N. Fourrié and A.
Parracho. A high quality reprocessed ground-based GPS
dataset for atmospheric process studies, radiosonde and
model evaluation, and reanalysis of HyMeX Special
Observing Period. Quart. J. Roy. Met. Soc. DOI:
10.1002/qj.2701 (early view).
d’ouvrage
Communications
(conférence)
1.
1.
2.
3.
4.
5.
6.
7.
Ducrocq, V. and HyMeX EC-ISC Team. HyMeX-SOP1, the
field campaign dedicated to heavy precipitation and flashflooding in Northwestern Mediterranean.EGU General
Assembly 2013. Exposé invité.
Ducrocq, V., E. Richard and the HyMeX EC-ISC Team.
HyMeX SOP1, the field campaign dedidicate to heavy
precipitation and flash-floods in Northwestern
Mediterranean, International Conference on Alpine
Meteorology, Kranjska Gora, Slovenia, 3 - 7 June 2013.
Exposé invité.
Ducrocq, V. and HyMeX EC-ISC (SOP1)Team. HyMeX-SOP1,
a field campaign dedicated to heavy precipitation and flashflooding in Northwestern Mediterranean, 13th EMS Annual
Meeting & 11th European Conference on Applications of
Meteorology (ECAM) , 09 – 13 September 2013, Reading,
United Kingdom. Exposé invité.
Defer, E., S. Coquillat, J.-P. Pinty, S. Soula, E. Richard, J.M. Martin, S. Prieur, W. Rison, P. Krhebiel, R. Thomas, D.
Rodeheffer, V. Ducrocq, O. Bousquet, L. Labatut, O.
Roussot, S. Roos, T. Farges, C. Vergeiner, F. Malaterre, S.
Pedeboy, W. Schulz, P. Blanchet, G. Anderson, H.-D. Betz,
K. Lagouvardos, P. Ortega, and G. Molinié. An overview of
HyMeX SOP1 - Focus on Atmospheric Electricty, AGU fall
meeting, 3-7 December 2012.
Caumont, O., K. Y. Nawanti, F. Saïd, O. Bousquet, B.
Campistron. An observation operator to compare wind
profiler mass observations with convective-scale model
outputs. 6th Mediterranean-6th HyMeX workshop, 7-10 May
2012, Primošten, Croatia.
Defer E. and the TTO1h team. Update on the
instrumentation, data/products and analysis strategy of the
HyMeX lightning task team TTO1h. 6th HyMeX workshop, 710 May 2012, Primosten, Croatia.
Defer, E., S. Coquillat, J.-P. Pinty, S. Soula, E. Richard, J.-
20/33
8.
9.
10.
11.
12.
13.
14.
15.
16.
17.
18.
19.
M. Martin, S. Prieur, W. Rison, P. Krehbiel, R. Thomas, D.
K. Lagouvardos, P. Ortega, and G. Molinie. An overview of
HyMeX SOP1 - Focus on Atmospheric Electricty, AGU fall
meeting, 3-7 December 2012.
Lagouvardos, K., V. Kotroni, O. Bousquet, E. Defer,
A.Lampiris, G. Molinie, and J.-F. Ribaud, The IOP6 (24
September 2012) heavy precipitation event overSouthern
France: observational and model analysis, 7th HyMeX
Workshop, 7-10 October 2013, Cassis, France.
Pinty, J.-P., M. Chong, E. Defer, S. Bielli, HyLMA and
EUCLID teams, First simulations of some electrical aspects
of observed real cases of SOP1 HyMeX with MesoNH, 7th
HyMeX Workshop, 7-10 October 2013, Cassis, France.
Anderson, G., H.-D. Betz, S. Coquillat, E. Defer, T. Farges,
L.-J. Gallin, V. Kotroni, P. Krehbiel, K. Lagouvardos, P.
Ortéga, S. Pedeboy, J.-P. Pinty, W. Rison, W. Schulz, S.
Soula, R. Thomas, and C. Vergeiner, Examples of STLightning Observations During SOP1 at Flash and Storm
Scales, 7th HyMeX Workshop, 7-10 October 2013, Cassis,
France.
Coquillat, S., E. Defer, and F. Honoré, On SOP1 Lightning
Activity Relatively to NW Mediterranean Lightning
Climatology, 7th HyMeX Workshop, 7-10 October 2013,
Cassis, France.
Ribaud, J.-F., O. Bousquet, H. Al-Sakka, A.-A.
Boumahmoud, S. Coquillat, E. Defer, B. Fradon, D.
Lambert, and P. Tabary, Improvement of Meteo-France’s
polarimetric hydrometeor classification scheme for lightning
studies, 7th HyMeX Workshop, 7-10 October 2013, Cassis,
France.
Flamant, C., E. Richard, V. Ducrocq, 2013 : Water vapour
variability over the Mediterranean upstream of convective
system: a comparison between airborne LIDAR observations
and mesoscale NMP models forecasts during the HyMeX
SOP1. 7th HyMeX Workshop, 7-10 October 2013, Cassis,
France.
Flamant C., J.-P. Chaboureau, P. Chazette, P. Di Girolamo,
E. Freney, F. Burnet, J. Banks, A. Schwarzenboeck, R.
Dupuy, 2013 : The impact of desert dust on the life cycle of
convection in the Mediterranean basin: a case study from
the HyMeX SOP1, 7th HYMEX workshop, 7-10 October 2013,
Cassis, France.
Bock, O., M. Nuret, P. Bosser, C. Champollion, E. Bresson,
G. Dick, M. Ramatschi, and M. Kohler, Comparison of GNSS
and radiosonde integrated water vapour measurements
during the HYMEX SOP, 7th HYMEX workshop, Cassis,
France, 7-10 October 2013.
S. Berthou, J. Taillefer, Ph. Drobinski, S. Mailler, T. Arsouze,
C. Basdevant, O. Bock, P. Chazette, Ph. Cocquerez, P. Di
Girolamo, A. Doerenbecher, C. Flamant, L. Menut, M.
Stéfanon, 2013: Evaluation of WRF forecast and regional
climate simulations against HyMeX SOP1 measurements,
7th HYMEX workshop, 7-10 October 2013, Cassis, France.
Soula, S., E. Defer, M. Fullekrug, O. van der Velde, S.
Coquillat, J.-P. Pinty, W. Rison, P. R. Krehbiel, R. J. Thomas,
O. Bousquet, and S. Pedeboy, Time and space correlation
between sprites and lightning flash events for a storm case
during HyMeX campaign, AGU Falll Meeting, San Francisco,
USA, 2013.
Gallin, L.-J., F. Coulouvrat, T. Farges, R. Marchiano, E.
Defer, W. Rison, W. Schulz, and M. Nuret, Lightning
characterization through acoustic and electromagnetic
measurements recorded during the HyMeX SOP1 and
simulation of the acoustic nonlinear propagation in realistic
thunderstorm meteorological conditions, AGU Falll Meeting,
San Francisco, USA, 2013.
Defer, E., S. Coquillat, J.-P. Pinty, S. Soula, E. Richard, J.M. Martin, S. Prieur, W. Rison, P. Krebhiel, R. Thomas, D.
21/33
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21.
22.
23.
24.
25.
26.
27.
28.
29.
30.
K. Lagouvardos, P. Ortega, and G. Molinie , An overview of
the electrical activity recorded during PEACH, the
atmospheric electricity component of HyMeX, ECSS 2013,
7th European Conference on Severe Storms, Helsinki,
Finland, 3 - 7 June 2013. Heino Tooming Award.
Pinty J.-P., M. Chong, E. Defer, C. Barthe, E. Richard, P.
Krehbiel, W. Rison and R. Thomas, Explicit simulations of
mixed-phase electrified clouds of the HyMeX-SOP1
experiment with the mesoscale model MesoNH, ECSS 2013,
7th European Conference on Severe Storms, Helsinki,
Finland, 3 - 7 June 2013.
Farges, T., E. Blanc, A. Le Pichon, E. Defer, M. Fullekrug,
and S. Soula, Overview of acoustic measurements in SouthEast of France in 2012 during severe weather, Geophysical
Research Abstracts, Vol. 15, EGU2013-6893, EGU General
Assembly 2013.
Soula, S., E. Defer, M. Fullekrug, T. Farges, O. van der
Velde, S. Coquillat, J.-P. Pinty, J.-M. Martin, W. Rison, P.
Krehbiel, R. Thomas, O. Bousquet, C. Vergeiner, and S.
Pedeboy, Spatial and temporal correlation between sprites
and their parent lightning flashes for a storm case during
HyMeX campaign, EGU General Assembly, Vienna, Austria,
2013.
Bousquet, O., A. Berne, J. Delanoe, Y. Dufournet, J.
Gourley, J. Van Baelen, C. Augros, L. Besson, B.
Boudevillain, O. Caumont, S. Coquillat, E. Defer, V.
Ducrocq, J. Grazioli, D. J. Jorgensen, P.-E. Kirstetter, J.-F.
Ribaud, D. Scipion, H. Al-Sakka, A.-A. Boumahmoud, J.
Beck, B. Fradon, A. Schwarzenboeck et P. Tabary. Multiplefrequency radar observations collected in southern France
during HyMeX SOP1. 7th HyMeX Workshop, Cassis, France,
7-10 October 2013.
Saïd, F., B. Campistron, S. Paupe, D. Lambert, O. Bock, O.
Caumont, C. Champollion, H. Delbarre, P. D. Girolamo, O.
Garrouste, D. Legain et A. Sokolov. Continuous Humidity
Profiling using Wind-Profiler Radars in the UHF-VHF band.
7th HyMeX Workshop, Cassis, France, 7-10 October 2013.
Chaboureau, J.-P. and J. Delanoë: Verification of Meso-NH
hydrometeors forecasts against remote sensing
observations, 7th HyMeX international workshop, Cassis,
France, 7-10 October 2013.
Richard, E.., V. Ducrocq et al. The HyMeX SOP1 field
experiment. 16th Conference on Mountain Meteorology, San
Diego, Ca, USA, 18-22 Aug. 2014. Exposé invité.
Richard, E, N. Fourrié, M. Faivre, S. Bielli, C. Flamant.
Assimilation of LEANDRE II water observations: impact
study on the HyMeX SOP1 precipitation forecasts. 8th HyMeX
workshop, 15-18 Sep. 2014, Valetta, Malta.
Di Girolamo, P., C. Flamant, D. Summa, D. Stelitano, M.
Cacciani, P. Chazette, V. Ducrocq, M. Nuret, N. Fourié, E.
Richard. Raman lidar measurements in the frame of the
HyMeX SOP1. 8th HyMeX workshop, 15-18 Sep. 2014,
Valetta, Malta.
Saïd F., B. Campistron, D. Lambert , H. Delbarre, M.
Abadie, J.A. Aranda , E. Bargain, F. Besson, Y. Bezombes,
J.L. Boichard, J.L. Bourrian, O. Bousquet, G. Canut, G.
Cherel, S. Derrien, A. Doerenbecher, J.M. Donier, T.
Douffet, P. Durand, J.B. Estrampes, A. Ezcurra, A. Frappier,
J.A. Garcia-Moya , O. Garrouste, J.A. Guijarro, R. Guillot, C.
Hervier, J.L. Jouve, J. Lovichi, M. Macaigne, M. M. Maruri, B.
Piguet, E. Pique, Y Pointin, S. Prieur, E. Richard, C. RuffinSoler, A. Sokolov, D. Subra, J. Torres, M. Turp. First results
on wind conditions in the North-Western Mediterranean
basin observed by a network of wind profiler radars. 8th
HyMeX workshop, 15-18 Sep. 2014, Valetta, Malta.
Defer, E., O. Bousquet, J. Delanoë, P. Krehbiel, S. Pedeboy,
J.-P. Pinty, W. Rison, W. Schulz, A. Schwarzenboeck
Schwarzenboeck, C. Flamant Preliminary results on the
22/33
31.
32.
33.
34.
35.
36.
37.
38.
39.
40.
41.
42.
43.
44.
45.
study of the lightning activity and the cloud properties
recorded during the SOP1-IOP6 (24 September 2012). 8th
HyMeX workshop 15-18 September 2014, La Valletta, Malta
Chazette, P., C. Flamant, X. Shang, A. Doerenbecher, J.
Totems, F. Marnas. Water vapor observations upstream of
two intense rainfall events documented in the framework of
HyMeX SOP1. 8th HyMeX workshop 15-18 September 2014,
La Valletta, Malta.
Bock, O., P. Bosser, R. Pacione, Jose Antonio Sánchez
Sobrino, M. Nuret, N. Fourrié, A high quality reprocessed
GPS integrated water vapour dataset for atmospheric
process studies, model evaluation and assimilation into
HYMEX SOP reanalysis, EMS General Assembly, Prague,
Czech Republic, 6–10 October 2014.
Saussereau, G., Caumont, O. and Delanoë, J. A data
assimilation experiment of RASTA airborne cloud radar data
during HyMeX IOP16. EGU General Assembly, Vienna,
2015.
Flamant, C. et al. Sources and transport of water vapour.
9th HyMeX workshop, 21-25 September 2015, Mykonos,
Greece.
Delanoë, J. et al. Microphyisics in precipitating systems. 9th
HyMeX workshop, 21-25 September 2015, Mykonos,
Greece.
Davolio, S. Studies of IOPs (SOP1) precipitation events. 9th
Greece.
Saïd F., B. Campistron, D. Bengochea, O. Bock, P. Di
Girolamo, D. Legain. Continuous humidity profiling using
wind-profiler radar in the UHF band. 9th HyMeX workshop,
21-25 September 2015, Mykonos, Greece.
Di Girolamo P., C. Flamant, M. Cacciani, E. Richard, V.
Ducrocq, D. Summa, D. Stelitano, N. Fourrié, F. Said.
Observation of low-level wind reversals in the Gulf of Lion
area and their impact on the water vapour distribution and
variability. 9th HyMeX workshop, 21-25 September, 2015
Mykonos, Greece.
Chazette, P., C. Flamant, X. Shang, J. Totems, J.-C. Raut,
A. Doerenbecher, V. Ducrocq, N. Fourrié, O. Bock, S.
Cloché. Coherence between multi-instrument and multimodel atmospheric moisture retrievals in the framework of
the HyMeX SOP1. 9th HyMeX workshop, 21-25 September,
2015, Mykonos, Greece.
Lee, K., C. Flamant, V. Durocq, Nadia Fourrié, P. Chazette,
O. Bock. Multi-scale interactions between moist-air flow and
deep precipitation during HyMeX IOP15a heavy precipitation
event. . 9th HyMeX workshop, 21-25 September 2015,
Mykonos, Greece.
Fourrié, N. M. Nuret, P. Brousseau, A. Doerenbecher, H.
Bénichou, P. Moll, O. Bock, F. Saïd
The second AROMEWMED reanalysis of SOP1. 9th HyMeX workshop, 21-25
September 2015, Mykonos, Greece.
Zecchin, C., O. Caumont, É. Defer, J.-P. Pinty, C. Bovalo, C.
Barthe.Assimilation of Lightning Mapping Array (LMA) data
into AROME-WMED: a first attempt on HyMeX IOP6. 9th
Greece.
Ribaud, J.-F., O. Bousquet, S. Coquillat. Relationships
between total lightning activity, microphysics, and
kinematics during the 24 September 2012 HyMeX bow-echo
system. 9th HyMeX workshop, 21-25 September 2015,
Mykonos, Greece.
Rysman, J.-F., C. Claud, J.-P. Chaboureau, J. Delanoe, B.
Funatsu Severe convection in the Mediterranean from
microwave observations. 9th HyMeX workshop, 21-25
September 2015, Mykonos, Greece.
Bock, O., P. Bosser , R. Pacione , M. Nuret , N. Fourrié , A.
Parracho. A high quality reprocessed ground-based GPS
dataset for atmospheric process studies, radiosonde and
model evaluation, and reanalysis of HyMeX Special
Observing Period. 9th HyMeX workshop, 21-25 September
23/33
2015, Mykonos, Greece.
46. Richard E. et al., Heavy precipitation events in the
northwestern Mediterranean : Some examples from HyMeX.
HD(CP)2 international conference, 15-19 February 2016,
Berlin, Germany (exposé invité).
lecture
1.
d’ouvrage
Communications
(conférence)
Articles de
vulgarisation
1.
Conférences de
vulgarisation
1.
Ducrocq, V. HyMeX, un vaste programme expérimental en
Méditerranée, débat SMF Météo et Climat du 28 mars 2013,
Cité de l'Espace, Toulouse.
Autres
1.
Dossier de presse et Conférence de presse nationale le 30
août 2012 à Paris
Point presse pour les média régionaux et locaux le 10
septembre 2012 avec la visite du centre des opérations, des
avions et du site de Candillargues
2 dépêches AFP, 1 dépêche Reuters
TV: reportages France3 national, journal de 20h TF1 (WE),
Journal de 16h (LCI), Soir3 WE, France 3 Rhône reportage,
TVsud + plateau TV, Marina TV, Aleas.TV
Presse nationale : Le Monde (Science), Le Figaro, Les
Echos (Science), Le Midi Libre (Algérie)
Radios : France-inter, France-Bleue minute verte, France
bleue Provence, France-Bleue Hérault, France Bleue
Vaucluse, France-bleue Roussillon, NRJ/ChérieFM, RDC,
Radio Méditerranée internationale
Presse régionale : Le Dauphiné Libéré, Le Midi Libre,
L’Indépendant du Midi, L’Hérault du Jour, …
Internet : 7sur7.be, rtl.be, 20min.fr, 20min.ch, capital.fr,
actu-environnement.com, ansamed.info,catnat.net,
ilcapoluogo.globalist.it, ilfattoquotidiano.it, ultimahora.es,
nieuwsbank.nl, nachrichten.ch, noaanews.noaa.gov,….
France
1.
1.
2.
3.
4.
Actions de
diffusion
Ducrocq V., S. Belamari, B. Boudevillain, O. Bousquet, P.
Cocquerez, A. Doerenbecher, P. Drobinski, C. Flamant, L.
Labatut, D. Lambert, M. Nuret, E. Richard, O. Roussot, P.
Testor, P. Arbogast, P.-A. Ayral, J. Van Baelen, C.
Basdevant, J.-L. Boichard, D. Bourras, C. Bouvier, M.-N.
Bouin, O. Bock, Isabelle Braud, C. Champollion, L.Coppola,
S. Coquillat, E. Defer, J. Delanoë, G. Delrieu, J.-F. DidonLescot, P. Durand, C. Estournel, N. Fourrié, O. Garrouste,
H.Giordani, J.Le Coz, Y. Michel, O. Nuissier, G. Roberts, F.
Saïd, A. Schwarzenboeck, K. Sellegri, I. Taupier-Letage et
J.-P. Vandervaere. HyMeX, les campagnes de mesures :
focus sur les événements extrêmes en Méditerranée. La
Météorologie, 80, 37-47, 2013.
5.
6.
7.
8.
Liste des publications monopartenaires (impliquant un seul partenaire)
lecture
1.
2.
International
3.
4.
Caumont O., A. Foray, L. Besson and J. Parent du Châtelet.
An Observation Operator for Radar Refractivity Change:
Comparison of Observations and Convective-Scale
Simulations. Bound. Layer Meteor., 148, 379-397, 2013
Chazette, P., F. Marnas, and J. Totems. The mobile Water
vapor Aerosol Raman LIdar and its implication in the
framework of the HyMeX and ChArMEx programs: application
to a dust transport process, Atmos. Meas. Tech., 7, 16291647, 2014.
Chazette, P., Marnas, F., and Totems, J.: Comparison of IASI
water vapor retrieval with H2O-Raman lidar in the frame of
the Mediterranean HyMeX and ChArMEx programs, Atmos.
Chem. Phys., 14, 9583-9596, 2014.
Martinet, P., N. Fourrié, Y. Bouteloup, E. Bazile and F.
Rabier. Toward the improvement of short-range forecasts by
the analysis of cloud variables from IASI radiances. Atmos.
24/33
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6.
7.
8.
9.
10.
11.
12.
13.
14.
15.
16.
17.
18.
19.
Sci. Let. 15: 342–347, 2014
Fourrié N., E. Bresson, M. Nuret, C. Jany, P. Brousseau, A.
Doerenbecher, M. Kreitz, O. Nuissier, E. Sevault, H.
Bénichou, M. Amodei and F. Pouponneau. AROME-WMED, a
real-time mesoscale model designed for the HyMeX Special
Observation Periods. Geoscientific Model Development., 8,
1919-1941, 2015.
Pantillon, F., J.-P. Chaboureau and E. Richard. Remote
impact of North Atlantic hurricanes on the Mediterranean
during episodes of intense rainfall in autumn 2012. Quart. J.
Roy. Meteor. Soc., 141, 967–978, 2015.
Sbii, S., M. Zazaoui, N., Semane. Dynamical contribution of
mean potential vorticity pseudo-observations derived from
MetOp/GOME2 ozone data into short-range weather forecast
during high precipitation events. Int. J. Bas. Appl. Sci., 4,
206-215, 2015
Legrand R., Y. Michel, and T. Montmerle (2016): Diagnosing
non-Gaussianity of forecast and analysis errors in a
convective-scale model. Nonlin. Processes Geophys., 23, 112. doi:10.5194/npg-23-1-2016.
Bouttier F., L. Raynaud, O. Nuissier and B. Ménétrier.
Sensitvity of the AROME ensemble to initial and surface
perturbations during HyMeX. Quart. J. Roy. Meteor. Soc..,
DOI: 10.1002/qj.2622 (early view).
Chazette, P., C. Flamant, J.-C. Raut, J. Totems and X.
Shang. Tropical moisture enriched storm tracks over the
Mediterranean and their link with intense rainfall in the
Cevennes-Vivarais area during HyMeX. Quart. J. Roy.
Meteor. Soc.., DOI: 10.1002/qj.2674 (early view).
Augros, C., Caumont, O., Ducrocq, V., Gaussiat, N. and
Tabary, P.: Comparisons between S, C, and X band
polarimetric radar observations and convective-scale
simulations of HyMeX first special observing period. Quart. J.
Roy. Meteor. Soc., DOI: 10.1002/qj.2572 (early view).
Flaounas, E. K. Lagouvardos, V. Kotroni, C. Claud, J.
Delanoë, C. Flamant, E. Madonna and H. Wernli. Processes
leading to heavy precipitation associated with two
Mediterranean cyclones observed during the HyMeX SOP1.
Quart. J. Roy. Meteor. Soc., DOI: 10.1002/qj.2618 (early
view).
Pantillon, F., J.-P. Chaboureau and E. Richard Vortex–vortex
interaction between Hurricane Nadine (2012) and an Atlantic
cut-off dropping the predictability over the Mediterranean.
Quart. J. Roy. Meteor. Soc., DOI: 10.1002/qj.2635 (early
view).
Scheffknecht P., E. Richard and D. Lambert. A highly
localised high precipitation event over Corsica. Quart. J. Roy.
Meteor. Soc. (accepted).
Caumont, O., B. Vincendon, D. Cimini, U. Löhnert, L. AladosArboledas, R. Bleisch, F. Buffa, M. E. Ferrario, A. Haefele, T.
Huet, F. Madonna et G. Pace : Assimilation of humidity and
temperature observations retrieved from ground-based
microwave radiometers into a convective-scale NWP model.
Quart. J. Roy. Meteor. Soc. (in revision)
Martinet P., Fourrié N., Guidard V., Rabier, F., Montmerle T.
and Brunel P. Towards the use of microphysical variables for
the assimilation of cloud-affected infrared radiances. Quart.
J. Roy. Meteor. Soc., 2013.
Ménétrier B., Montmerle T., Michel Y. et Berre L. Linear
Filtering of Sample Covariances for Ensemble-Based Data
Assimilation. Part I: Optimality Criteria and Application to
Variance Filtering and Covariance Localization. Mon. Weather
Rev., 143, 1622—1643, 2014.
Ménétrier B., Montmerle T., Michel Y. et Berre L. Linear
Filtering of Sample Covariances for Ensemble-Based Data
Assimilation. Part II: Application to a Convective-Scale NWP
Model. Mon. Weather Rev., 143, 1644—1664, 2014.
Ménétrier B., Montmerle T., Berre L. et Michel Y. Estimation
and diagnosis of heterogeneous flow-dependent background
error covariances at convective scale using either large or
small ensembles. Q.J.R. Meteorol. Soc., 140, 2050—2061,
25/33
14, 9583–9596, 2014.
d’ouvrage
Communications
(conférence)
20.
1.
1.
2.
3.
4.
5.
6.
7.
8.
9.
10.
11.
12.
13.
14.
15.
Augros, C., P. Tabary, O. Caumont, 2012: Simulation of
polarimetric variables and comparison to observations by
polarimetric radar. Proc., 7th European Conf. on Radar in
Meteor. and Hydrol. (ERAD2012), Toulouse, France.
Caumont, O., A. Foray, L. Besson, J. Parent du Châtelet,
2012: A radar refractivity change observation operator for a
convective-scale model: Comparison of observations and
simulations. 6th Mediterranean-HyMeX workshop,
Primošten, Croatia, PS1.14.
Caumont, O., A. Foray, L. Besson, J. Parent du Châtelet,
2012: Comparison between weather radar refractivity
change observations and mesoscale numerical weather
prediction analyses. Proc., 7th European Conf. on Radar in
Meteor. and Hydrol. (ERAD2012), Toulouse, France.
Cimini, D., O. Caumont, U. Löhnert, L. Alados-Arboledas, R.
Bleisch, J. Fernández-Gálvez, T. Huet, M. Ferrario, F.
Madonna, O. Maier, F. Nasir, G. Pace, R. Posada, 2012: An
international network of ground-based microwave
radiometers for the assimilation of temperature and
humidity profiles into NWP model. 9th International
Symposium on Tropospheric Profiling (ISTP), L’Aquila, Italy,
Center of Excellence for the Forecast of Severe Events
(CETEMPS).
Martinet P., F. Rabier, L. Lavanant, N. Fourrié and A.
Gambacorta, 2013: Evaluation of new IASI channel
selections to improve the assimilation of cloud-affected
radiances by the retrieval of cloud microphysical variables.
3ème Conférence IASI, 4-8 Février 2013, Presqu’île de
Giens Hyères les Palmiers, France.
Martinet P., N. Fourrié, V. Guidard, F. Rabier, T. Montmerle
and P. Brunel, 2012: New developments for the use of
microphysical variables for the assimilation of IASI radiances
in convective scale models. 18th International Study TOVS
conference, 21-27 Mars 2012, Toulouse, France.
Martinet P., F. Faijan, L. Lavanant, N. Fourrié ,F.Rabier,
2012: IASI Channel Selection in Cloudy Conditions. 18th
International Study TOVS conference, 21-27 Mars 2012,
Toulouse, France.
Ménétrier B., T. Montmerle, Y. Michel and L. Berre, 2012:
Adaptative denoising of ensemble-based background error
variance maps at convective scale. Int. Conf. on Ensemble
Methods in Geophysical Sciences, Toulouse, 12-16 nov.
Michel, Y., R. Legrand, B. Ménétrier and T. Montmerle,
2012: A large ensemble of data assimilations for studying
forecast errors and predictability over the Mediterranean.
6th HyMeX workshop, 7-10 May 2012, Primosten, Croatia.
Montmerle T., Y. Michel, and P. Martinet, 2012a: Forecast
errors in clouds and precipitation for the assimilation of
cloudy radiances and radar data CNRM-GAME. 6th HyMeX
workshop, 7-10 May 2012, Primosten, Croatia.
Montmerle T., E. Wattrelot and C. Geijo, 2012b: Operational
assimilation of radar data at convective scale in AROME
France: current status and international cooperations. 7th
European Conference on Radar in Meteorology and
Hydrology (ERAD), 24-29 june, Toulouse, France.
Montmerle T. and P. Martinet, 2012: Forecast errors in
clouds and precipitation: diagnosis and modelling for the
assimilation of cloudy radiances and radar data in the
AROME model at convective scale. Int. Conf. on Ensemble
Methods in Geophysical Sciences, Toulouse, 12-16 nov.
Vincensini A., Fourrié, Rabier F. and Vincent Guidard, 2012:
Data assimilation of IASI radiances over land. 18th
International Study TOVS conference, 21-27 Mars 2012,
Toulouse, France.
Flamant C., J. Delanoë, 2012: Safire aircraft flight plans. 6th
HyMeX workshop 7-10 May 2012, Primosten, Croatia.
Fourrié N., M. Nuret, E. Bresson, P. Brousseau, 2012:
26/33
16.
17.
18.
19.
20.
21.
22.
23.
24.
25.
26.
27.
28.
29.
30.
AROME-WMED, a mesoscale model designed for the HyMeX
special observation periods. 6th HyMeX workshop 7-10 May
2012, Primosten, Croatia.
Ducrocq V., 2012: General operation coordination incl. main
and secondary centers. 6th HyMeX workshop 7-10 May
2012, Primosten, Croatia.
Labatut L., 2012: HyMeX SOP website: real-time
observations, real-time models and models products. 6th
HyMeX workshop 7-10 May 2012, Primosten, Croatia.
Kalthoff, N., D. Lambert and the TS4a team Overview of the
SOP1 in Corsica. 6th HyMeX workshop 7-10 May 2012,
Primosten, Croatia.
Pinty, J.-P., S. Coquillat, J.-M. Martin, S. Prieur, E. Defer, W.
Rison, P. Krheniel, and D. Rodeheffer, Observation and
modeling of the cloud electrical activity during HyMeX, 14th
Plinius conference, Palma de Mallorca, 13-16 November
2012.
Pinty, J.-P., C. Barthe, E. Defer, E. Richard, and M. Chong,
Explicit simulation of electrified clouds from idealized to real
case studies, 16th ICCP, Leipzig, Germany, 30 July-03
August, 2012.
Pinty, J.-P., C. Barthe, E. Defer, E. Richard, and M. Chong,
Explicit simulations of electrified mixed-phase clouds in
MESO-NH: Towards real-case studies for HyMeX, 6th
Mediterranean-HyMeX workshop, Primošten, Croatia.
Nuret M., N. Fourrié, E. Bresson, A.Jansa,S. Guedj, C. Payan
and V. Guidard, 2012: Evaluation of the AROME_WMED
MODEL for the autumn 2011 period. 6th HyMeX workshop 710 May 2012, Primosten, Croatia.
Pinty, J.-P., C. Barthe, E. Defer, E. Richard and M. Chong,
2012: Explicit simulations of electrified mixed-phase clouds
in MESO-NH: Towards real-case studies for HyMeX. 6th
HyMeX workshop, 7-10 May 2012, Primosten, Croatia.
Buguet, M., S. Coquillat, S. Soula, C. Barthe, M. Chong, O.
Bousquet and E. Defer, 2012: Relationships between
lightning activity, microphysics, and kinematics during a
thundercloud observed in the HyMeX SOP1 area. 6th HyMeX
workshop, 7-10 May 2012, Primosten, Croatia.
Delanoë J., A. Protat, J. Vinson, E. Fontaine, A.
Schwarzenboeck and C. Flamant, 2012: RASTA: The airbone
cloud radar, a tool for studying cloud and precipitation
during HyMeX SOP1. 6th HyMeX workshop, 7-10 May 2012,
Primosten, Croatia.
Lambert Dominique , Kalthoff Norbert , Aemisegger
Franziska , Bargain Erwan , Bezombes Yannick , Campistron
Bernard , Coquillat Sylvain , Corsmeier Ulrich , Defer Eric ,
Derrien Solène , Hankers Rudolf , Jarnot Christian ,
Kottmeier Christoph , Martin Jean-Michel , Pinty Jean-Pierre
, Prieur Serge , Richard Evelyne , Said Frederique , VanBaelen Joël , Wernli Heini , Wieser Andreas CORSICA: a
mediterranean atmospheric observatory in Corsica scientific objectives and deployment strategy for HyMeX. 6th
HyMeX workshop, 7-10 May 2012, Primosten, Croatia.
Wattrelot, E., T. Montmerle and C. Geijo, 2012: Assimilation
of radar data in the AROME-WMED model at convective
scale. 6th HyMeX workshop, 7-10 May 2012, Primosten,
Croatia.
Bock, O., P. Bosser, B. Garayt, T. Duquesnoy (2012) A
comparison of GPS atmospheric products for weather
forecasting and climate monitoring applications in the
Mediterranean region, 6th HyMeX Workshop, 7-10 May,
2012, Primosten, Croatia..
Augros, C., O. Caumont, V. Ducrocq et P. Tabary, 2013 :
Development and validation of a full polarimetric radar
simulator. 36th Conference on Radar Meteorology,
Breckenridge, Colorado, Amer. Meteor. Soc., 387.
Augros, C., P. Tabary et O. Caumont, 2013 : Development
and validation of a polarimetric radar simulator. 11th
International Precipitation Conference, Ede-Wageningen,
Pays-Bas, Hydrology, Quantitative Water Management
Group (Wageningen University) et Royal Netherlands
27/33
Meteorological Institute (KNMI).
31. Augros, C., O. Caumont, V. Ducrocq et P. Tabary, 2013 :
Development and validation of a full polarimetric radar
simulator. Proc., 7th HyMeX Workshop, Cassis, France.
32. Augros, C., O. Caumont, P. Tabary et V. Ducrocq, 2013 :
Development of a polarimetric radar simulator in Meso-NH.
7th Meso-NH User’s Meeting, Toulouse, France, CNRMGAME/LA.
33. Besson, L., O. Caumont, L. Goulet, S. Bastin, J. Parent du
Châtelet, L. Menut et F. Fabry : Refractivity measurement
by radar during the HYMEX campaign. 36th Conference on
Radar Meteorology, Breckenridge, Colorado, Amer. Meteor.
Soc., 222.
34. Besson, L., O. Caumont, L. Goulet, S. Bastin, J. Parent du
Châtelet, L. Menut et F. Fabry, 2013 : Refractivity
measurement by radar during the HyMeX campaign. Proc.,
7th HyMeX Workshop, Cassis, France.
35. Bousquet, O., C. Voirin, O. Maier, J.-M. Donier, A. Haefele,
E. Maillard, O. Caumont, O. Garrouste et P. di Girolamo,
2013 : Evaluation of brightness temperatures and vertical
profiles of temperature and humidity deduced from
microwave radiometer measurements performed in
Candillargues during HyMeX SOP1. 7th HyMeX Workshop,
Cassis, France.
36. Campistron, B., F. Saïd, H. Delbarre, P. Augustin, and D.
Lambert, 2013. Rain Profiling with a UHF Wind Profiler and
its Application to Soil Erosion Study. 7th HyMeX Workshop,
Cassis, France.
37. Nuret, N. Fourrié, E. Bresson. AROME_WMED reanalysis of
the HyMeX SOP1. 7th HyMeX Workshop, Cassis, France.
38. Sokolov A., Delbarre H., Saïd F. , Campistron B. , Lambert
D. , Kalthoff N. , Wieser A., Augustin P. , Fourmentin M.,
2013. Multi-scale study of the dynamics of low troposphere
by correlation technique using UHF radar measurements at
southern Corsica. HYMEX 7th conference, Cassis, France
39. Delanoë, J., J.-P. Vinson, C. Caudoux, M. Ceccaldi, E.
Fontaine, A. Schwarzenboeck, C. Flamant. Cloud dynamic
and microphysics derived from RASTA measurements during
HyMeX SOP1. 7th HyMeX Workshop, 7-10 October 2013,
Cassis, France.
40. Duroure, C., R. Dupuy, E. Fontaine, A. Schwarzenboeck Use
of imaging probes to quantify the balance between riming
and aggregation processes in the precipitation fields of
mesoscale convective cloud systems (MCS) sampled during
HyMeX 2012. 7th HyMeX Workshop, 7-10 October 2013,
Cassis, France.
41. Fontaine, E., R. Dupuy, C. Duroure, C. Gourbeyre, J.
Delanoë, A. Schwarzenboeck. Determination of areadiameter and mass-diameter relationships from ice particle
imagery in order to deduce IWC within mid-latitude
convective clouds observed over the Mediterranean basin.
7th HyMeX Workshop, 7-10 October 2013, Cassis, France.
42. Beck, J., O. Bousquet, M. Nuret. Verification of AROMEWMED wind field forecasts using ARAMIS multiple-doppler
syntheses. 7th HyMeX Workshop, 7-10 October 2013,
Cassis, France.
43. Bock,O., M. Nuret, P. Bosser, C. Champollion, E. Bresson,
G. Dick, M. Ramatschi, M. Kohler. Comparison of GNSS and
radiosonde integrated water vapour measurements during
the HyMeX SOP. 7th HyMeX Workshop, 7-10 October 2013,
Cassis, France.
44. H. Sodemann, M. Böttcher, C. Grams, F. Aemisegger, S.
Pfahl, A. Schäfler, A. Dörnbrack, U. Corsmeier, A. Wieser, C.
Flamant, H. Wernli, 2013: Moist air inflow and heavy
precipitation over Italy during IOP12a: a Lagrangian
analysis of data from multiple aircraft, 7th HYMEX
workshop, 7-10 October 2013, Cassis, France.
45. Cimini, D., O. Caumont, U. Löhnert, L. Alados-Arboledas, R.
Bleisch, J. Fernández-Gálvez, T. Huet, M. E. Ferrario, F.
Madonna, O. Maier, F. Nasir, G. Pace et R. Posada, 2014 : A
data assimilation experiment of temperature and humidity
28/33
46.
47.
48.
49.
50.
51.
52.
profiles from an international network of ground-based
microwave radiometers. 13th Specialist Meeting on
Microwave Radiometry and Remote Sensing of the
Environment (MicroRad 2014), Pasadena, California,
California Institute of Technology.
N. Fourrié, E. Bresson, M. Nuret, C. Jany, P. Brousseau, A.
Doerenbecher, M. Kreitz, H. Benichou, M. Amodei, F.
Pouponneau (2014) : AROME-WMED, a real-time mesoscale
model designed for the HyMeX Special Observation Periods.
The world weather open science conference, Montréal,
Canada, 16-21 August, 2014.
Fourrié, N., M. Nuret, E. Bresson, C. Jany, P. Brousseau, A.
Doerenbecher, H. Bénichou Evaluation of the 1st
AROME_WMED reanalysis of SOP1 and plans for the 2nd
AROME_WMED reanalysis. 8th HyMeX workshop 15-18
September 2014, La Valletta, Malta.
Caumont, O., D. Cimini, U. Löhnert, L. Alados-Arboledas, R.
Bleisch, M. E. Ferrario, T. Huet, F. Madonna, A. Haefele,
M3.4 - Data assimilation experiments of temperature and
humidity profiles from an international network of groundbased microwave radiometers. 8th HyMeX workshop 15-18
Ménétrier, B., Y. Michel, T. Montmerle, L. BerreF. Nasir, G.
Pace, R. Posada Development and test of an heterogeneous
background error model for convective scale AROME during
HyMeX SOP1. 8th HyMeX workshop 15-18 September 2014,
La Valletta, Malta.
Ribaud, J.-F., O. Bousquet, S. Coquillat, E. Defer, R.
Thomas, W. Rison, P. Krehbiel, J.-P. Pinty, V. Ducrocq, D.
Lambert. Relationships between total lightning activity,
microphysics, and kinematics during the 24 September 2012
HyMeX bow-echo system. 8th HyMeX workshop 15-18
Vergeiner, C., E. Defer, P. Laroche, W. Rison, P. Krehbiel, R.
Thomas, W. Schulz, G. Anderson, S. Pedeboy, F. Malaterre,
S. Soula Investigation of lightning properties during HyMeX
SOP1 storms based on distinct observation data sets - First
analysis and results. 8th HyMeX workshop 15-18 September
2014, La Valletta, Malta.
Pinty, J.-P., M. Chong, P. Krehbiel, B. Rison, E. Defer
Simulation of the electrication process of several storms
observed by the HyMeX-LMA lightning flash detector. 8th
HyMeX workshop 15-18 September 2014, La Valletta, Malta.
53.
54. O. Bock, P. Bosser, R. Pacione, J.A. Sánchez Sobrino, M.
Nuret, N. Fourrié. A high quality reprocessed dataset of GPS
tropospheric delay and integrated water vapour for process
studies and assimilation into atmospheric models during
HyMeX SOP. 8th HyMeX workshop 15-18 September 2014,
La Valletta, Malta.
55. Saussereau, G., O. Caumont, J. Delanoë. A data
assimilation experiment of RASTA airborne cloud radar data
during HyMeX IOP16. 8th HyMeX workshop 15-18
56. Delanoë, J., J.-P. Vinson, C. Caudoux, A. Guignard, E.
Fontaine, A. An update on cloud dynamic and microphysics
products derived from RASTA measurements during HYMEXSOP1. 8th HyMeX workshop 15-18 September 2014, La
Valletta, Malta.
57. Scheffknecht, P., E. Richard and D. Lambert. A localized
heavy precipitation event over Corsica triggered by lee-side
convergence. 9th HyMeX workshop, 21-25 September,
Mykonos, Greece.
58. Brousseau, P., Y. Seity, N. Fourrié. Impact of the recent
improvements of the AROME-France numerical weather
prediction system on the convection forecasting. 9th HyMeX
workshop, 21-25 September, Mykonos, Greece.
59. Michel, Y., T. Montmerle. Development of a new ensemble
data assimilation scheme for the convective scale AROME
model. 9th HyMeX workshop, 21-25 September, Mykonos,
Greece.
29/33
lecture
France
Actions de
diffusion
d’ouvrage
Communications
(conférence)
60. Coquillat, S., E. Defer, D. Lambert, J.-M. Martin, J.-P. Pinty,
V. Pont, S. Prieur. SAETTA: fine-scale observation of the
total lightning activity in the framework of the CORSiCA
atmospheric observatory. 9th HyMeX workshop, 21-25
September, Mykonos, Greece.
61. Molinié, G., J.-P. Pinty, H. Bresson, E. Defer, S. Coquillat.
Lightning morphologies in the LMA-HyMeX database. 9th
HyMeX workshop, 21-25 September, Mykonos, Greece.
62. Pinty,J.-P., C. Bovalo, P. Krehbiel, B. Rison, R. Thomas, E.
Defer, E. Richard. Simulation in a mesoscale model of
several electrified storms observed by a LMA during HyMeX
SOP1. 9th HyMeX workshop, 21-25 September, Mykonos,
Greece.
63. Saïd, F., B. Campistron, T. Payan, H. Delbarre, Y. Dufournet,
A. Sokolov. Rain profiling with a UHF wind profiler and its
application to microphysics studies. 9th HyMeX workshop,
21-25 September, Mykonos, Greece.
64. Flamant, C., P. Chazette, K-O Lee , J.-C. Raut, O. Bock,
Xiaoxia Shang, J. Totems. Large scale moisture patterns and
their link with heavy precipitation events during the HyMeX
SOP1. 9th HyMeX workshop, 21-25 September, Mykonos,
Greece.
65. Defer E. and the HyMeX ST-Lightning Team. An overview on
the current HyMeX ST-Lightning activities: from the SOP1 to
the LOP. 9th HyMeX workshop, 21-25 September, Mykonos,
Greece.
66. Defer , E., J. Grazioli , A. Bernes , W. Rison , P. Krehbiel , J.P. Pinty , S. Coquillat. Looking at the influence of lightning
occurrence on the change of microphysics orientation
inferred from HyLMA and MXPOL data during the 24
September 2012 IOP6 case. 9th HyMeX workshop, 21-25
September, Mykonos, Greece.
1. Besson, L., O. Caumont et J. Parent du Châtelet, 2013 : La
réfractivité radar:vers une cartographie de l’humidité entrès
basse couche de l’atmosphère. La Météorologie, 8(83), 81–
89, DOI : 10.4267/2042/52057, URL :
http://dx.doi.org/10.4267/2042/52057.
1.
2.
1. Caumont, O. et al., 2012: Assimilation of new remotesensing data types in Arome — The Antydote project. 4e
Colloque National sur l’Assimilation de Données, Nice,
France.
2. Bousquet, O., C. Voirin, O. Maier, J.-M. Donier, A. Haefele,
E. Maillard, O. Caumont et P. di Girolamo, 2013 : Evaluation
des températures de brillance et des profils verticaux de
température et d’humidité obtenus par radiomètre microonde pendant HyMeX. Journée Scientifique SIRTA,
Palaiseau, France, SIRTA.
Articles de
vulgarisation
1.
Conférences de
vulgarisation
Autres
1.
2.
1.
2.
Coquillat, S., 2015 : Observation tridimensionnelle des
éclairs dans le cadre de l’observatoire atmosphérique
CORSiCA. Météo et Climat Info ; Mars 2015, p5-6
E.3 LISTE DES ELEMENTS DE VALORISATION
La liste des éléments de valorisation inventorie les retombées (autres que les publications) décomptées dans le deuxième
tableau de la section Erreur ! Source du renvoi introuvable.. On détaillera notamment :
30/33
brevets nationaux et internationaux, licences, et autres éléments de propriété intellectuelle consécutifs au
projet.
- logiciels et tout autre prototype
- actions de normalisation
- lancement de produit ou service, nouveau projet, contrat,…
- le développement d’un nouveau partenariat,
- la création d’une plate-forme à la disposition d’une communauté
- création d’entreprise, essaimage, levées de fonds
- autres (ouverture internationale,..)
Elle en précise les partenariats éventuels. Dans le cas où des livrables ont été spécifiés dans l’annexe technique, on
présentera ici un bilan de leur fourniture.
-
31/33
E.4 BILAN ET SUIVI DES PERSONNELS RECRUTES EN CDD (HORS STAGIAIRES)
Ce tableau dresse le bilan du projet en termes de recrutement de personnels non permanents sur CDD ou assimilé. Renseigner une ligne par personne embauchée sur le projet quand l’embauche a été
financée partiellement ou en totalité par l’aide de l’ANR et quand la contribution au projet a été d’une durée au moins égale à 3 mois, tous contrats confondus, l’aide de l’ANR pouvant ne représenter
qu’une partie de la rémunération de la personne sur la durée de sa participation au projet.
Les stagiaires bénéficiant d’une convention de stage avec un établissement d’enseignement ne doivent pas être mentionnés.
Les données recueillies pourront faire l’objet d’une demande de mise à jour par l’ANR jusqu’à 5 ans après la fin du projet.
Identification
Nom et
Sexe Adresse
prénom
H/F email (1)
MIERE
Arnaud
H
BRESSO F
N Emilie
HALLY
Alan
FRESNA
Y Simon
FRESNA
Y Simon
BOVALO
Christoph
e
H
H
H
H
arnaud.mie
[email protected]
emilie.bres
son@gmail
.com
alan.hally@
meteo.fr
simonfresn
[email protected]
simonfresn
[email protected]
Christophe.
bovalo@ae
r.obs-mip.fr
02/2016
Avant le recrutement sur le projet
Dernier
Lieu d'études Expérience
diplôme
(France, UE, prof.
obtenu au
hors UE)
Antérieure,
moment du
y compris
recrutement
post-docs
(ans)
Analyste_Pro France
3.5
grammeur
CNAM
Doctorat
France
3
01/2016
Master
UE
06/2015
Master
06/2015
03/2016
Date des
dernières
nouvelles
Recrutement sur le projet
Partenaire ayant Poste dans Durée
embauché la
le projet (2) missions
personne
(mois) (3)
Après le projet
Date de fin Devenir
Type
Type d’emploi
de mission professionnel d’employeur (5) (6)
sur le projet (4)
Lien au Valorisation
projet
expérience
ANR (7) (8)
1
Assistant
ingénieur
7
26/10/2012 ???
EPST
Oui
Oui
2
Ingénieur
16
30/04/2013 CDD
Non
Oui
3
1
Ingénieur
2
Oui
Oui
France
3
1
Doctorant
25
30/11/2013 Post-Doc
France
31/01/2014 Post-Doc
Enseignement et Ingénieur
recherche
publique
EPST
Chercheur
EPST
Chercheur
Oui
Oui
Doctorat
France
4
1
Post-Doc
3
30/04/2014 CDD
TPE
Ingénieur
Non
Oui
Doctorat
France
3
1
Post-Doc
6,25
31/10/2014 Post-Doc
France
EPIC
Post-Doc
Non
Oui
Assistant
Ingénieur
Aide pour le remplissage
(1) Adresse email : indiquer une adresse email la plus pérenne possible
(2) Poste dans le projet : post-doc, doctorant, ingénieur ou niveau ingénieur, technicien, vacataire, autre (préciser)
(3) Durée missions : indiquer en mois la durée totale des missions (y compris celles non financées par l’ANR) effectuées sur le projet
(4) Devenir professionnel : CDI, CDD, chef d’entreprise, encore sur le projet, post-doc France, post-doc étranger, étudiant, recherche d'emploi, sans nouvelles
(5) Type d’employeur : enseignement et recherche publique, EPIC de recherche, grande entreprise, PME/TPE, création d’entreprise, autre public, autre privé, libéral, autre (préciser)
(6) Type d’emploi : ingénieur, chercheur, enseignant-chercheur, cadre, technicien, autre (préciser)
32/33
(7) Lien au projet ANR : préciser si l’employeur est ou non un partenaire du projet
(8) Valorisation expérience : préciser si le poste occupé valorise l’expérience acquise pendant le projet.
Les informations personnelles recueillies feront l’objet d’un traitement de données informatisées pour les seuls besoins de l’étude anonymisée sur le devenir professionnel des personnes recrutées sur
les projets ANR. Elles ne feront l’objet d’aucune cession et seront conservées par l'ANR pendant une durée maximale de 5 ans après la fin du projet concerné. Conformément à la loi n° 78-17 du 6
janvier 1978 modifiée, relative à l'Informatique, aux Fichiers et aux Libertés, les personnes concernées disposent d'un droit d'accès, de rectification et de suppression des données personnelles les
concernant. Les personnes concernées seront informées directement de ce droit lorsque leurs coordonnées sont renseignées. Elles peuvent exercer ce droit en s'adressant l'ANR (http://www.agencenationale-recherche.fr/Contact).
33/33

IODA-MED

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