Ten years of temperature and wind observation on a 45-m tower at Dome C, East Antarctic plateau

International audience Abstract. Long-term, continuous in situ observations of the near-surface atmospheric boundary layer are critical for many weather and climate applications. Although there is a proliferation of surface stations globally, especially in and around populous areas, there are notabl...

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Main Authors: Genthon, Christophe, Veron, Dana, Vignon, Etienne, Six, Delphine, Dufresne, Jean-Louis, Madeleine, Jean-Baptiste, Sultan, Emmanuelle, Forget, François
Other Authors: Laboratoire de Météorologie Dynamique (UMR 8539) (LMD), Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris, École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL), School of Marine Science and Policy, College of Earth, Ocean, and Environment Newark (CEOE), University of Delaware Newark -University of Delaware Newark, Centre National de la Recherche Scientifique (CNRS), Institut des Géosciences de l’Environnement (IGE), Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ), Université Grenoble Alpes (UGA), Centre De Recherche et d'Enseignement sur les Systèmes Côtiers (CRESCO), Muséum national d'Histoire naturelle (MNHN)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2021
Subjects:
Online Access:https://hal.science/hal-03853764
https://hal.science/hal-03853764/document
https://hal.science/hal-03853764/file/essd-2021-204.pdf
https://doi.org/10.5194/essd-2021-204
id ftepunivpsaclay:oai:HAL:hal-03853764v1
record_format openpolar
institution Open Polar
collection École Polytechnique, Université Paris-Saclay: HAL
op_collection_id ftepunivpsaclay
language English
topic [SDE]Environmental Sciences
[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology
spellingShingle [SDE]Environmental Sciences
[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology
Genthon, Christophe
Veron, Dana
Vignon, Etienne
Six, Delphine
Dufresne, Jean-Louis
Madeleine, Jean-Baptiste
Sultan, Emmanuelle
Forget, François
Ten years of temperature and wind observation on a 45-m tower at Dome C, East Antarctic plateau
topic_facet [SDE]Environmental Sciences
[SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology
description International audience Abstract. Long-term, continuous in situ observations of the near-surface atmospheric boundary layer are critical for many weather and climate applications. Although there is a proliferation of surface stations globally, especially in and around populous areas, there are notably fewer tall meteorological towers with multiple instrumented levels. This is particularly true in remote and extreme environments such as the Eastern Antarctic plateau. In the article, we present and analyze 10 years of data from 6 levels of meteorological instrumentation mounted on a 42-m tower located at Dome C, East Antarctica near the Concordia research station, producing a unique climatology of the near-surface atmospheric environment (Genthon et al., 2021,a,b). Monthly temperature and wind data demonstrate the large seasonal differences in the near-surface boundary layer dynamics, depending on the presence or absence of solar surface forcing. Strong vertical temperature gradients (inversions) frequently develop in calm, winter conditions, while vertical convective mixing occurs in the summer leading to near-uniform temperatures along the tower. Seasonal variation in wind speed is much less notable at this location than the temperature variation as the winds are less influenced by the solar cycle; there are no katabatic winds as Dome C is quite flat. Harmonic analysis confirms that most of the energy in the power spectrum is at diurnal, annual and semi-annual time scales. Analysis of observational uncertainty and comparison to reanalysis data from ERA-5 indicate that wind speed is particularly difficult to measure at this location. Data are distributed on PANGAEA data repository, see data availability section.
author2 Laboratoire de Météorologie Dynamique (UMR 8539) (LMD)
Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris
École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)
School of Marine Science and Policy
College of Earth, Ocean, and Environment Newark (CEOE)
University of Delaware Newark -University of Delaware Newark
Centre National de la Recherche Scientifique (CNRS)
Institut des Géosciences de l’Environnement (IGE)
Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )
Université Grenoble Alpes (UGA)
Centre De Recherche et d'Enseignement sur les Systèmes Côtiers (CRESCO)
Muséum national d'Histoire naturelle (MNHN)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)
format Article in Journal/Newspaper
author Genthon, Christophe
Veron, Dana
Vignon, Etienne
Six, Delphine
Dufresne, Jean-Louis
Madeleine, Jean-Baptiste
Sultan, Emmanuelle
Forget, François
author_facet Genthon, Christophe
Veron, Dana
Vignon, Etienne
Six, Delphine
Dufresne, Jean-Louis
Madeleine, Jean-Baptiste
Sultan, Emmanuelle
Forget, François
author_sort Genthon, Christophe
title Ten years of temperature and wind observation on a 45-m tower at Dome C, East Antarctic plateau
title_short Ten years of temperature and wind observation on a 45-m tower at Dome C, East Antarctic plateau
title_full Ten years of temperature and wind observation on a 45-m tower at Dome C, East Antarctic plateau
title_fullStr Ten years of temperature and wind observation on a 45-m tower at Dome C, East Antarctic plateau
title_full_unstemmed Ten years of temperature and wind observation on a 45-m tower at Dome C, East Antarctic plateau
title_sort ten years of temperature and wind observation on a 45-m tower at dome c, east antarctic plateau
publisher HAL CCSD
publishDate 2021
url https://hal.science/hal-03853764
https://hal.science/hal-03853764/document
https://hal.science/hal-03853764/file/essd-2021-204.pdf
https://doi.org/10.5194/essd-2021-204
geographic Antarctic
East Antarctica
geographic_facet Antarctic
East Antarctica
genre Antarc*
Antarctic
Antarctica
East Antarctica
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
op_source ISSN: 1866-3508
Earth System Science Data
https://hal.science/hal-03853764
Earth System Science Data, 2021, ⟨10.5194/essd-2021-204⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/essd-2021-204
hal-03853764
https://hal.science/hal-03853764
https://hal.science/hal-03853764/document
https://hal.science/hal-03853764/file/essd-2021-204.pdf
doi:10.5194/essd-2021-204
op_rights http://creativecommons.org/licenses/by/
info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.5194/essd-2021-204
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spelling ftepunivpsaclay:oai:HAL:hal-03853764v1 2024-06-09T07:40:42+00:00 Ten years of temperature and wind observation on a 45-m tower at Dome C, East Antarctic plateau Genthon, Christophe Veron, Dana Vignon, Etienne Six, Delphine Dufresne, Jean-Louis Madeleine, Jean-Baptiste Sultan, Emmanuelle Forget, François Laboratoire de Météorologie Dynamique (UMR 8539) (LMD) Institut national des sciences de l'Univers (INSU - CNRS)-École polytechnique (X)-École des Ponts ParisTech (ENPC)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Département des Géosciences - ENS Paris École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-École normale supérieure - Paris (ENS-PSL) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL) School of Marine Science and Policy College of Earth, Ocean, and Environment Newark (CEOE) University of Delaware Newark -University of Delaware Newark Centre National de la Recherche Scientifique (CNRS) Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ) Université Grenoble Alpes (UGA) Centre De Recherche et d'Enseignement sur les Systèmes Côtiers (CRESCO) Muséum national d'Histoire naturelle (MNHN)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER) 2021 https://hal.science/hal-03853764 https://hal.science/hal-03853764/document https://hal.science/hal-03853764/file/essd-2021-204.pdf https://doi.org/10.5194/essd-2021-204 en eng HAL CCSD Copernicus Publications info:eu-repo/semantics/altIdentifier/doi/10.5194/essd-2021-204 hal-03853764 https://hal.science/hal-03853764 https://hal.science/hal-03853764/document https://hal.science/hal-03853764/file/essd-2021-204.pdf doi:10.5194/essd-2021-204 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 1866-3508 Earth System Science Data https://hal.science/hal-03853764 Earth System Science Data, 2021, ⟨10.5194/essd-2021-204⟩ [SDE]Environmental Sciences [SDU.STU.ME]Sciences of the Universe [physics]/Earth Sciences/Meteorology info:eu-repo/semantics/article Journal articles 2021 ftepunivpsaclay https://doi.org/10.5194/essd-2021-204 2024-05-16T11:54:18Z International audience Abstract. Long-term, continuous in situ observations of the near-surface atmospheric boundary layer are critical for many weather and climate applications. Although there is a proliferation of surface stations globally, especially in and around populous areas, there are notably fewer tall meteorological towers with multiple instrumented levels. This is particularly true in remote and extreme environments such as the Eastern Antarctic plateau. In the article, we present and analyze 10 years of data from 6 levels of meteorological instrumentation mounted on a 42-m tower located at Dome C, East Antarctica near the Concordia research station, producing a unique climatology of the near-surface atmospheric environment (Genthon et al., 2021,a,b). Monthly temperature and wind data demonstrate the large seasonal differences in the near-surface boundary layer dynamics, depending on the presence or absence of solar surface forcing. Strong vertical temperature gradients (inversions) frequently develop in calm, winter conditions, while vertical convective mixing occurs in the summer leading to near-uniform temperatures along the tower. Seasonal variation in wind speed is much less notable at this location than the temperature variation as the winds are less influenced by the solar cycle; there are no katabatic winds as Dome C is quite flat. Harmonic analysis confirms that most of the energy in the power spectrum is at diurnal, annual and semi-annual time scales. Analysis of observational uncertainty and comparison to reanalysis data from ERA-5 indicate that wind speed is particularly difficult to measure at this location. Data are distributed on PANGAEA data repository, see data availability section. Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica École Polytechnique, Université Paris-Saclay: HAL Antarctic East Antarctica