Identification of the sources of inertia-gravity waves in the Andes Cordillera region

Four major sources of inertia-gravity waves are known in the Earth atmosphere: upper-tropospheric jet-streams, lower-tropospheric fronts, convection and topography. The Andes Cordillera region is an area where all of these major sources are potentially present. By combining ECMWF and NCEP-NCAR...

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Main Authors: A. Spiga, H. Teitelbaum, V. Zeitlin
Format: Article
Language:English
Published: Copernicus Publications 2008-09-01
Series:Annales Geophysicae
Online Access:https://www.ann-geophys.net/26/2551/2008/angeo-26-2551-2008.pdf
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spelling doaj-e089e47bc8e64a4785efb0244ad035b62020-11-24T22:36:21ZengCopernicus PublicationsAnnales Geophysicae0992-76891432-05762008-09-01262551256810.5194/angeo-26-2551-2008Identification of the sources of inertia-gravity waves in the Andes Cordillera regionA. Spiga0H. Teitelbaum1V. Zeitlin2Laboratoire de Météorologie Dynamique, École Normale Supérieure, 24 rue Lhomond, 75231 Paris Cedex 05, FranceLaboratoire de Météorologie Dynamique, École Normale Supérieure, 24 rue Lhomond, 75231 Paris Cedex 05, FranceLaboratoire de Météorologie Dynamique, École Normale Supérieure, 24 rue Lhomond, 75231 Paris Cedex 05, FranceFour major sources of inertia-gravity waves are known in the Earth atmosphere: upper-tropospheric jet-streams, lower-tropospheric fronts, convection and topography. The Andes Cordillera region is an area where all of these major sources are potentially present. By combining ECMWF and NCEP-NCAR reanalysis, satellite and radiosoundings data and mesoscale WRF simulations in the Andes Cordillera region, we were able to identify the cases where, respectively, the jet-stream source, the convective source and the topography source are predominantly in action. We retrieve emitted wave parameters for each case, compare them, and analyse possible emission mechanisms. The WRF mesoscale model shows very good performance in reproducing the inertia-gravity waves identified in the data analysis, and assessing their likely sources.https://www.ann-geophys.net/26/2551/2008/angeo-26-2551-2008.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. Spiga
H. Teitelbaum
V. Zeitlin
spellingShingle A. Spiga
H. Teitelbaum
V. Zeitlin
Identification of the sources of inertia-gravity waves in the Andes Cordillera region
Annales Geophysicae
author_facet A. Spiga
H. Teitelbaum
V. Zeitlin
author_sort A. Spiga
title Identification of the sources of inertia-gravity waves in the Andes Cordillera region
title_short Identification of the sources of inertia-gravity waves in the Andes Cordillera region
title_full Identification of the sources of inertia-gravity waves in the Andes Cordillera region
title_fullStr Identification of the sources of inertia-gravity waves in the Andes Cordillera region
title_full_unstemmed Identification of the sources of inertia-gravity waves in the Andes Cordillera region
title_sort identification of the sources of inertia-gravity waves in the andes cordillera region
publisher Copernicus Publications
series Annales Geophysicae
issn 0992-7689
1432-0576
publishDate 2008-09-01
description Four major sources of inertia-gravity waves are known in the Earth atmosphere: upper-tropospheric jet-streams, lower-tropospheric fronts, convection and topography. The Andes Cordillera region is an area where all of these major sources are potentially present. By combining ECMWF and NCEP-NCAR reanalysis, satellite and radiosoundings data and mesoscale WRF simulations in the Andes Cordillera region, we were able to identify the cases where, respectively, the jet-stream source, the convective source and the topography source are predominantly in action. We retrieve emitted wave parameters for each case, compare them, and analyse possible emission mechanisms. The WRF mesoscale model shows very good performance in reproducing the inertia-gravity waves identified in the data analysis, and assessing their likely sources.
url https://www.ann-geophys.net/26/2551/2008/angeo-26-2551-2008.pdf
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AT hteitelbaum identificationofthesourcesofinertiagravitywavesintheandescordilleraregion
AT vzeitlin identificationofthesourcesofinertiagravitywavesintheandescordilleraregion
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