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Journal articles on the topic 'Météorologie Spatiale'

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Published: 4 June 2021

Last updated: 8 February 2022

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1

Hamon, Jean. "Trente années de météorologie spatiale." La Météorologie 8, spécial (1995): 101. http://dx.doi.org/10.4267/2042/52033.

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Rochas, Michel, ** compléter auteur **. "Les débuts de la météorologie spatiale." La Météorologie 8, no. 70 (2010): 45. http://dx.doi.org/10.4267/2042/34576.

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DONGUY, Patrick, and Loic HARANG. "40 ans de météorologie spatiale - Décembre 2003." La Météorologie 8, no. 45 (2004): 10. http://dx.doi.org/10.4267/2042/36034.

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Lebeau, André. "Le développement de la météorologie spatiale en Europe." Hermès 34, no. 2 (2002): 183. http://dx.doi.org/10.4267/2042/14453.

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Le Borgne, Pierre, Gérard Legendre, and Anne Marsouin. "Meteosat and GOES-East Imager Visible Channel Calibration." Journal of Atmospheric and Oceanic Technology 21, no. 11 (2004): 1701–9. http://dx.doi.org/10.1175/jtechjtech-1675.1.

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Abstract As a preliminary step to solar irradiance calculations, the Centre de Météorologie Spatiale (CMS) has developed a pragmatic approach to calibrate the visible channels of Meteosat and GOES-East imagers. The responsivity of the Meteosat visible channel has been monitored with three desert targets from 1989 to 2002. The annual degradation rate has been estimated to 1.8% for Meteosat-4, 1.4% for Meteosat-5, and 1.9% for Meteosat-7. A reference calibration coefficient for Meteosat-7 has been derived from a comparison with Clouds and Earth's Radiant Energy System (CERES) data in summer 1998

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Kerr, Yann, Philippe Waldteufel, Jean-Pierre Wigneron, et al. "The Soil Moisture and Ocean Salinity (SMOS) Mission: first results and achievements." Revue Française de Photogrammétrie et de Télédétection, no. 200 (April 19, 2014): 12–19. http://dx.doi.org/10.52638/rfpt.2012.57.

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La mission SMOS (Soil moisture and Ocean Salinity) a été lancée avec succès le 2 novembre 2009. Cette mission menée par l'ESA (Agence Spatiale Europénne) est dédiée à la mesure de l'humidité superficielle des sols sur les continents (avec une précision recherchée de 0,04m3/m3) et la salinité des océans (objectif 0.1psu). Ces deux quantités géophysiques sont très importantes car elle contrôle le budget énergétique à l'interface sol-atmosphère. Leur connaissance à l'échelle globale est utile pour les recherches sur le climat et la météorologie, en particulier pour les modèles de prévision numéri

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Boyer, Nathalie, Pierre Todoroff, Louis Paulin, and Agnès Bégué. "Un modèle de prévision de rendement de la canne à sucre basé sur des images satellitaires SPOT : l'exemple de la Réunion." Revue Française de Photogrammétrie et de Télédétection, no. 197 (April 22, 2014): 76–85. http://dx.doi.org/10.52638/rfpt.2012.84.

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Cet article présente une méthode de prévision de récolte de canne à sucre à partir d'images satellites à haute résolution spatiale Spot, adaptée à des zones de production de canne à sucre composées d'une multitude de petites parcelles. Cette étude est réalisée sur l'exemple de l'île de La Réunion. Elle est basée sur l'ajustement d'une relation empiriqueentre l'indice de végétation NDVI (Normalized Difference Vegetation Index), mesuré au maximum de développement du couvert végétal, et le rendement en biomasse fraiche à la récolte. Le rendement est traduit en production à différentes échelles (c

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Olivier, Chomette, Raymond Armante, Cyril Crevoisier, et al. "CH4 IPDA Lidar mission data simulator and processor for MERLIN: prototype development at LMD/CNRS/Ecole Polytechnique." EPJ Web of Conferences 176 (2018): 02016. http://dx.doi.org/10.1051/epjconf/201817602016.

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The MEthane Remote sensing Lidar missioN (MERLIN), currently in phase C, is a joint cooperation between France and Germany on the development of a spatial Integrated Path Differential Absorption (IPDA) LIDAR (LIght Detecting And Ranging) to conduct global observations of atmospheric methane. This presentation will focus on the status of a LIDAR mission data simulator and processor developed at LMD (Laboratoire de Météorologie Dynamique), Ecole Polytechnique, France, for MERLIN to assess the performances in realistic observational situations.

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Ottlé, Catherine, Daniel Richard, Sylvie LeHégarat, et al. "Modélisation hydro-météorologique du bassin du Rhône : apport de la télédétection spatiale." La Houille Blanche, no. 1 (February 2002): 57–61. http://dx.doi.org/10.1051/lhb/2002007.

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Krinner, Gerhard, and Christophe Genthon. "The Antarctic surface mass balance in a stretched grid general circulation model." Annals of Glaciology 25 (1997): 73–78. http://dx.doi.org/10.1017/s0260305500013823.

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The Laboratoire de Météorologie Dynamique (LMD) variable-grid atmospheric general circulation model (AGCM) was used in this study for a five-year high-resolution simulation of the Antarctic climate. The horizontal resolution is about 100 km over a large part of the ice sheet. This study focuses on the simulated surface mass balance (precipitation-evaporation sublimation-melt) and on the spatial and temporal variability of snowfall in Antarctica. The simulated annual mean surface mass balance for the whole continent is close to the observed value, and the model simulates well the spatial distri

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Krinner, Gerhard, and Christophe Genthon. "The Antarctic surface mass balance in a stretched grid general circulation model." Annals of Glaciology 25 (1997): 73–78. http://dx.doi.org/10.3189/s0260305500013823.

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The Laboratoire de Météorologie Dynamique (LMD) variable-grid atmospheric general circulation model (AGCM) was used in this study for a five-year high-resolution simulation of the Antarctic climate. The horizontal resolution is about 100 km over a large part of the ice sheet. This study focuses on the simulated surface mass balance (precipitation-evaporation sublimation-melt) and on the spatial and temporal variability of snowfall in Antarctica. The simulated annual mean surface mass balance for the whole continent is close to the observed value, and the model simulates well the spatial distri

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12

Silva, Felipe Das Neves Roque da, and José Ricardo Almeida França. "Impacto da duplicação de CO2 no clima global simulado por um modelo de circulação geral da atmosfera." Anuário do Instituto de Geociências 27 (January 1, 2004): 27–52. http://dx.doi.org/10.11137/2004_0_27-52.

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The objective of this work is to evaluate climate changes caused by atmospheric CO2 concentration duplication. The LMD-Z atmosphere general circulation model (AGCM) was used (Laboratoire de Météorologie Dynamique - France). The model was integrated for a fifty years period and only the last forty years were used for analyses. This experiment have made two simulations: the first using the current CO2 concentration (control case) and the second using this concentration doubled (duplication case). Both were made with a variable spatial resolution with maximum of it centered in Rio de Janeiro. Thi

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Gao, Jing, V. Masson-Delmotte, T. Yao, L. Tian, C. Risi, and G. Hoffmann. "Precipitation Water Stable Isotopes in the South Tibetan Plateau: Observations and Modeling*." Journal of Climate 24, no. 13 (2011): 3161–78. http://dx.doi.org/10.1175/2010jcli3736.1.

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Abstract Measurements of precipitation isotopic composition have been conducted on a daily basis for 1 yr at Bomi, in the southeast Tibetan Plateau, an area affected by the interaction of the southwest monsoon, the westerlies, and Tibetan high pressure systems, as well as at Lhasa, situated west of Bomi. The measured isotope signals are analyzed both on an event basis and on a seasonal scale using available meteorological information and airmass trajectories. The processes driving daily and seasonal isotopic variability are investigated using multidecadal climate simulations forced by twentiet

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14

Soubeyroux, Jean-Michel, Fabrice Dosnon, Jacques Richon, Michel Schneider, and Pierre Lassegues. "Caractérisation à haute résolution spatiale des tempêtes historiques en métropole : Application à la tempête zeus du 6 Mars 2017." Climatologie 14 (2017): 96–106. http://dx.doi.org/10.4267/climatologie.1282.

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Une nouvelle méthode de spatialisation des rafales de vent à la résolution de 2,5 km sur la France a récemment été développée à partir des données anémométriques, des paramètres du relief et des analyses du modèle météorologique AROME pour caractériser les évènements de tempête à haute résolution spatio-temporelle. Différents indicateurs de sévérité ont été définis pour représenter les impacts des tempêtes aux différentes échelles nationale, régionale et départementale. Grâce à une reconstitution historique débutant en 1980, une nouvelle base de données de plus de 300 tempêtes a été constituée

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15

Verma, S., O. Boucher, M. S. Reddy, et al. "Tropospheric distribution of sulphate aerosol mass and number concentration during INDOEX-IFP and its transport over the Indian Ocean: a GCM study." Atmospheric Chemistry and Physics Discussions 5, no. 1 (2005): 395–436. http://dx.doi.org/10.5194/acpd-5-395-2005.

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Abstract. An interactive sulphate aerosol chemistry module has been incorporated in the Laboratoire de Météorologie Dynamique General Circulation Model (LMD-GCM) to simulate the sulphur chemistry during the Indian Ocean Experiment (INDOEX) Intensive Field Phase-1999 (INDOEX-IFP). The originality of this module is its ability to predict particle mass and number concentration for the Aitken and accumulation modes. The model qualitatively reproduces the spatial patterns of observations on sulphate aerosol during INDOEX. On the basis of size distribution retrieved from the observations made along

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16

Beck, Jeffrey, Mathieu Nuret, and Olivier Bousquet. "Model Wind Field Forecast Verification Using Multiple-Doppler Syntheses from a National Radar Network." Weather and Forecasting 29, no. 2 (2014): 331–48. http://dx.doi.org/10.1175/waf-d-13-00068.1.

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Abstract Model verification has traditionally relied upon in situ observations, which typically exist on a sparse network, making nonsurface model forecast verification difficult. Given increasing model resolution, supplemental observational datasets are needed. Multiple-Doppler wind retrievals using a national network of radars provide an opportunity to assess the accuracy of wind forecasts at multiple levels, as well as verification within a three-dimensional domain. Wind speed and direction verification results are presented for a 9-day period of forecasts from the French Application of Res

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17

L’Hévéder, Blandine, Francis Codron, and Michael Ghil. "Impact of Anomalous Northward Oceanic Heat Transport on Global Climate in a Slab Ocean Setting." Journal of Climate 28, no. 7 (2015): 2650–64. http://dx.doi.org/10.1175/jcli-d-14-00377.1.

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Abstract This paper explores the impact of anomalous northward oceanic heat transport on global climate in a slab ocean setting. To that end, the GCM LMDZ5A of the Laboratoire de Météorologie Dynamique is coupled to a slab ocean, with realistic zonal asymmetries and seasonal cycle. Two simulations with different anomalous surface heating are imposed: 1) uniform heating over the North Atlantic basin and 2) concentrated heating in the Gulf Stream region, with a compensating uniform cooling in the Southern Ocean in both cases. The magnitudes of the heating and of the implied northward interhemisp

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18

Magand, Claire, Agnès Ducharne, François Tilmant, et al. "Hybridation de réanalyses météorologiques de surface pour les zones de montagne : exemple du produit DuO sur le bassin de la Durance." La Houille Blanche, no. 3 (June 2018): 77–85. http://dx.doi.org/10.1051/lhb/2018035.

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La rareté des mesures et la complexité du terrain dans les régions montagneuses engendrent d'importantes incertitudes dans les réanalyses météorologiques de surface. L'hybridation de plusieurs réanalyses est une technique efficace pour limiter ces incertitudes. Dans le bassin versant de la Durance, deux réanalyses se basant sur des réseaux de mesures et des techniques d'extrapolation différentes coexistent, SAFRAN et SPAZM. Leur comparaison montre qu'elles sont complémentaires car les précipitations de SPAZM à une résolution spatiale plus fine que celle de SAFRAN, se basent sur un plus grand n

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19

Gryazin, V., C. Risi, J. Jouzel, et al. "To what extent could water isotopic measurements help us understand model biases in the water cycle over Western Siberia." Atmospheric Chemistry and Physics 14, no. 18 (2014): 9807–30. http://dx.doi.org/10.5194/acp-14-9807-2014.

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Abstract. We evaluate the isotopic composition of water vapor and precipitation simulated by the LMDZ (Laboratoire de Météorologie Dynamique-Zoom) GCM (General Circulation Model) over Siberia using several data sets: TES (Tropospheric Emission Spectrometer) and GOSAT (Greenhouse gases Observing SATellite) satellite observations of tropospheric water vapor, GNIP (Global Network for Isotopes in Precipitation) and SNIP (Siberian Network for Isotopes in Precipitation) precipitation networks, and daily, in situ measurements of water vapor and precipitation at the Kourovka site in Western Siberia. L

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20

Zou, Liwei, Tianjun Zhou, Laurent Li, and Jie Zhang. "East China Summer Rainfall Variability of 1958–2000: Dynamical Downscaling with a Variable-Resolution AGCM." Journal of Climate 23, no. 23 (2010): 6394–408. http://dx.doi.org/10.1175/2010jcli3689.1.

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Abstract A variable-grid atmospheric general circulation model, namely, Laboratoire de Météorologie Dynamique-zoom, version 4 (LMDz4), with a local zoom over eastern China, is driven by 40-yr European Centre for Medium-Range Weather Forecasts (ECMWF) Re-Analysis (ERA-40) data and is used as a downscaling tool of summer rainfall variability for the period 1958–2000. During the integration, the model temperature and wind were nudged to the ERA-40 data through a relaxation procedure. The performance of the LMDz4 in simulating the regional rainfall features is thoroughly assessed through a compari

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21

Jourdain, L., S. Bekki, F. Lott, and F. Lefèvre. "The coupled chemistry-climate model LMDz-REPROBUS: description and evaluation of a transient simulation of the period 1980–1999." Annales Geophysicae 26, no. 6 (2008): 1391–413. http://dx.doi.org/10.5194/angeo-26-1391-2008.

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Abstract. We present a description and evaluation of the Chemistry-Climate Model (CCM) LMDz-REPROBUS, which couples interactively the extended version of the Laboratoire de Météorologie Dynamique General Circulation Model (LMDz GCM) and the stratospheric chemistry module of the REactive Processes Ruling the Ozone BUdget in the Stratosphere (REPROBUS) model. The transient simulation evaluated here covers the period 1980–1999. The introduction of an interactive stratospheric chemistry module improves the model dynamical climatology, with a substantial reduction of the temperature biases in the l

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22

Castebrunet, H., P. Martinerie, C. Genthon, and E. Cosme. "A three-dimensional model study of methanesulphonic acid to non sea salt sulphate ratio at mid and high-southern latitudes." Atmospheric Chemistry and Physics Discussions 9, no. 4 (2009): 14995–5043. http://dx.doi.org/10.5194/acpd-9-14995-2009.

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Abstract. The Antarctic and sub-Antarctic methanesulphonic acid (MSA) to non sea salt sulphate (nssSO4) ratio is simulated with the Laboratoire de Météorologie Dynamique Atmospheric General Circulation Model including an atmospheric sulphur chemistry module. Spatial variations of the MSA/nssSO4 ratio in different regions have been suggested to be mostly dependent on temperature or sulphur source contributions. Its past variations in ice cores have been interpreted as related to the DMS precursor source location. Our model results are compared with available field measurements in the Antarctic

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23

Locatelli, R., P. Bousquet, F. Chevallier, et al. "Impact of transport model errors on the global and regional methane emissions estimated by inverse modelling." Atmospheric Chemistry and Physics 13, no. 19 (2013): 9917–37. http://dx.doi.org/10.5194/acp-13-9917-2013.

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Abstract. A modelling experiment has been conceived to assess the impact of transport model errors on methane emissions estimated in an atmospheric inversion system. Synthetic methane observations, obtained from 10 different model outputs from the international TransCom-CH4 model inter-comparison exercise, are combined with a prior scenario of methane emissions and sinks, and integrated into the three-component PYVAR-LMDZ-SACS (PYthon VARiational-Laboratoire de Météorologie Dynamique model with Zooming capability-Simplified Atmospheric Chemistry System) inversion system to produce 10 different

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24

Delrieu, G., A. Bellon, and J. D. Creutin. "Estimation de lames d'eau spatiales à l'aide de données de pluviomètres et de radar météorologique — Application au pas de temps journalier dans la région de Montréal." Journal of Hydrology 98, no. 3-4 (1988): 315–44. http://dx.doi.org/10.1016/0022-1694(88)90020-0.

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25

Castebrunet, H., P. Martinerie, C. Genthon, and E. Cosme. "A three-dimensional model study of methanesulphonic acid to non sea salt sulphate ratio at mid and high-southern latitudes." Atmospheric Chemistry and Physics 9, no. 24 (2009): 9449–69. http://dx.doi.org/10.5194/acp-9-9449-2009.

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Abstract. The Antarctic and sub-Antarctic methanesulphonic acid (MSA) to non sea salt sulphate (nssSO4) ratio is simulated with the Laboratoire de Météorologie Dynamique Atmospheric General Circulation Model including an atmospheric sulphur chemistry module. Spatial variations of the MSA/nssSO4 ratio in different regions have been suggested to be mostly dependent on temperature or sulphur source contributions. Its past variations in ice cores have been interpreted as related to the DMS precursor source location. Our model results are compared with available field measurements in the Antarctic

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26

Ostler, Andreas, Ralf Sussmann, Prabir K. Patra, et al. "Evaluation of column-averaged methane in models and TCCON with a focus on the stratosphere." Atmospheric Measurement Techniques 9, no. 9 (2016): 4843–59. http://dx.doi.org/10.5194/amt-9-4843-2016.

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Abstract. The distribution of methane (CH4) in the stratosphere can be a major driver of spatial variability in the dry-air column-averaged CH4 mixing ratio (XCH4), which is being measured increasingly for the assessment of CH4 surface emissions. Chemistry-transport models (CTMs) therefore need to simulate the tropospheric and stratospheric fractional columns of XCH4 accurately for estimating surface emissions from XCH4. Simulations from three CTMs are tested against XCH4 observations from the Total Carbon Column Network (TCCON). We analyze how the model–TCCON agreement in XCH4 depends on the

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27

Soto Molina, Victor Hugo, and Hugo Delgado Granados. "Estimación de la temperatura del aire en la alta montaña mexicana mediante un modelo de elevación del terreno: caso del volcán Nevado de Toluca (México) / Estimation of the air temperature in the Mexican high mountain environment by means of a model of elevation of the terrain, case of the Nevado de Toluca volcano (Mexico)." Ería 2, no. 2 (2020): 167–82. http://dx.doi.org/10.17811/er.2.2020.167-182.

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La carencia de estaciones climatológicas por encima de 3.500 metros sobre el nivel del mar (msnm) en México condiciona que los estudios sobre ecosistemas de alta montaña sean realizados con datos de estaciones cercanas, pero sin considerar la diferencia altitudinal de la temperatura debida al relieve y al gradiente vertical. Por tal razón, se realiza un modelo mensual y anual de la distribución espacial de la temperatura del aire en superficie para el volcán Nevado de Toluca (4.680 msnm) y zonas adyacentes, mediante el uso de un Modelo Digital de Elevaciones y el Gradiente Vertical de la Tempe

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28

Stenni, Barbara, Claudio Scarchilli, Valerie Masson-Delmotte, et al. "Three-year monitoring of stable isotopes of precipitation at Concordia Station, East Antarctica." Cryosphere 10, no. 5 (2016): 2415–28. http://dx.doi.org/10.5194/tc-10-2415-2016.

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Abstract. Past temperature reconstructions from Antarctic ice cores require a good quantification and understanding of the relationship between snow isotopic composition and 2 m air or inversion (condensation) temperature. Here, we focus on the French–Italian Concordia Station, central East Antarctic plateau, where the European Project for Ice Coring in Antarctica (EPICA) Dome C ice cores were drilled. We provide a multi-year record of daily precipitation types identified from crystal morphologies, daily precipitation amounts and isotopic composition. Our sampling period (2008–2010) encompasse

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