Trends in Atmospheric Humidity and Temperature above Dome C, Antarctica Evaluated from Observations and Reanalyses

International audience The time evolution of humidity and temperature above Dome C (Antarctica) has been investigated by considering data from (1) meteorological radiosondes (2005-2017), (2) the microwave radiometer HAMSTRAD (2012-2017), (3) four modern meteorological reanalyses (1980-2017) and (4)...

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Published in:Atmosphere
Main Authors: Ricaud, Philippe, Grigioni, Paolo, Roehrig, Romain, Durand, Pierre, Veron, Dana
Other Authors: Centre national de recherches météorologiques (CNRM), Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS), Laboratoire d'aérologie (LAERO), Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Observatoire Midi-Pyrénées (OMP), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS), University of Delaware Newark
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2020
Subjects:
Online Access:https://hal.science/hal-03043267
https://hal.science/hal-03043267/document
https://hal.science/hal-03043267/file/atmosphere-11-00836-v3.pdf
https://doi.org/10.3390/atmos11080836
id ftutoulouse3hal:oai:HAL:hal-03043267v1
record_format openpolar
institution Open Polar
collection Université Toulouse III - Paul Sabatier: HAL-UPS
op_collection_id ftutoulouse3hal
language English
topic radiosondes
microwave radiometer
meteorological reanalyses
precipitable water
temperature
SAM index
trends
[SDE]Environmental Sciences
spellingShingle radiosondes
microwave radiometer
meteorological reanalyses
precipitable water
temperature
SAM index
trends
[SDE]Environmental Sciences
Ricaud, Philippe
Grigioni, Paolo
Roehrig, Romain
Durand, Pierre
Veron, Dana
Trends in Atmospheric Humidity and Temperature above Dome C, Antarctica Evaluated from Observations and Reanalyses
topic_facet radiosondes
microwave radiometer
meteorological reanalyses
precipitable water
temperature
SAM index
trends
[SDE]Environmental Sciences
description International audience The time evolution of humidity and temperature above Dome C (Antarctica) has been investigated by considering data from (1) meteorological radiosondes (2005-2017), (2) the microwave radiometer HAMSTRAD (2012-2017), (3) four modern meteorological reanalyses (1980-2017) and (4) the southern annular mode (SAM) index (1980-2017). From these observations (2005-2017), a significant moistening trend (0.08 ± 0.06 kg m −2 dec −1) is associated with a significant warming trend (1.08 ± 0.55 K dec −1) in summer. Conversely, a significant drying trend of −0.04 ± 0.03 kg m −2 dec −1 (−0.05 ± 0.03 kg m −2 dec −1) is associated with a significant cooling trend of −2.4 ± 1.2 K dec −1 (−5.1 ± 2.0 K dec −1) in autumn (winter), with no significant trends in the spring. We demonstrate that 1) the trends identified in the radiosondes (2005-2017) are also present in the reanalyses and 2) the multidecadal variability of integrated water vapor and near-surface temperature (1980-2017) is strongly influenced by variability in the SAM index for all seasons but spring. Our study suggests that the decadal trends observed in humidity and near-surface temperature at Dome C (2005-2017) reflect the multidecadal variability of the atmosphere, and are not indicative of long-term trends that may be related to global climate change.
author2 Centre national de recherches météorologiques (CNRM)
Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP)
Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)
Laboratoire d'aérologie (LAERO)
Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Observatoire Midi-Pyrénées (OMP)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)
University of Delaware Newark
format Article in Journal/Newspaper
author Ricaud, Philippe
Grigioni, Paolo
Roehrig, Romain
Durand, Pierre
Veron, Dana
author_facet Ricaud, Philippe
Grigioni, Paolo
Roehrig, Romain
Durand, Pierre
Veron, Dana
author_sort Ricaud, Philippe
title Trends in Atmospheric Humidity and Temperature above Dome C, Antarctica Evaluated from Observations and Reanalyses
title_short Trends in Atmospheric Humidity and Temperature above Dome C, Antarctica Evaluated from Observations and Reanalyses
title_full Trends in Atmospheric Humidity and Temperature above Dome C, Antarctica Evaluated from Observations and Reanalyses
title_fullStr Trends in Atmospheric Humidity and Temperature above Dome C, Antarctica Evaluated from Observations and Reanalyses
title_full_unstemmed Trends in Atmospheric Humidity and Temperature above Dome C, Antarctica Evaluated from Observations and Reanalyses
title_sort trends in atmospheric humidity and temperature above dome c, antarctica evaluated from observations and reanalyses
publisher HAL CCSD
publishDate 2020
url https://hal.science/hal-03043267
https://hal.science/hal-03043267/document
https://hal.science/hal-03043267/file/atmosphere-11-00836-v3.pdf
https://doi.org/10.3390/atmos11080836
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source ISSN: 2073-4433
EISSN: 2073-4433
Atmosphere
https://hal.science/hal-03043267
Atmosphere, 2020, 11 (8), pp.836. ⟨10.3390/atmos11080836⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.3390/atmos11080836
hal-03043267
https://hal.science/hal-03043267
https://hal.science/hal-03043267/document
https://hal.science/hal-03043267/file/atmosphere-11-00836-v3.pdf
doi:10.3390/atmos11080836
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.3390/atmos11080836
container_title Atmosphere
container_volume 11
container_issue 8
container_start_page 836
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spelling ftutoulouse3hal:oai:HAL:hal-03043267v1 2024-09-15T17:45:02+00:00 Trends in Atmospheric Humidity and Temperature above Dome C, Antarctica Evaluated from Observations and Reanalyses Ricaud, Philippe Grigioni, Paolo Roehrig, Romain Durand, Pierre Veron, Dana Centre national de recherches météorologiques (CNRM) Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) Laboratoire d'aérologie (LAERO) Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Observatoire Midi-Pyrénées (OMP) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) University of Delaware Newark 2020-08 https://hal.science/hal-03043267 https://hal.science/hal-03043267/document https://hal.science/hal-03043267/file/atmosphere-11-00836-v3.pdf https://doi.org/10.3390/atmos11080836 en eng HAL CCSD MDPI info:eu-repo/semantics/altIdentifier/doi/10.3390/atmos11080836 hal-03043267 https://hal.science/hal-03043267 https://hal.science/hal-03043267/document https://hal.science/hal-03043267/file/atmosphere-11-00836-v3.pdf doi:10.3390/atmos11080836 info:eu-repo/semantics/OpenAccess ISSN: 2073-4433 EISSN: 2073-4433 Atmosphere https://hal.science/hal-03043267 Atmosphere, 2020, 11 (8), pp.836. ⟨10.3390/atmos11080836⟩ radiosondes microwave radiometer meteorological reanalyses precipitable water temperature SAM index trends [SDE]Environmental Sciences info:eu-repo/semantics/article Journal articles 2020 ftutoulouse3hal https://doi.org/10.3390/atmos11080836 2024-06-25T00:13:50Z International audience The time evolution of humidity and temperature above Dome C (Antarctica) has been investigated by considering data from (1) meteorological radiosondes (2005-2017), (2) the microwave radiometer HAMSTRAD (2012-2017), (3) four modern meteorological reanalyses (1980-2017) and (4) the southern annular mode (SAM) index (1980-2017). From these observations (2005-2017), a significant moistening trend (0.08 ± 0.06 kg m −2 dec −1) is associated with a significant warming trend (1.08 ± 0.55 K dec −1) in summer. Conversely, a significant drying trend of −0.04 ± 0.03 kg m −2 dec −1 (−0.05 ± 0.03 kg m −2 dec −1) is associated with a significant cooling trend of −2.4 ± 1.2 K dec −1 (−5.1 ± 2.0 K dec −1) in autumn (winter), with no significant trends in the spring. We demonstrate that 1) the trends identified in the radiosondes (2005-2017) are also present in the reanalyses and 2) the multidecadal variability of integrated water vapor and near-surface temperature (1980-2017) is strongly influenced by variability in the SAM index for all seasons but spring. Our study suggests that the decadal trends observed in humidity and near-surface temperature at Dome C (2005-2017) reflect the multidecadal variability of the atmosphere, and are not indicative of long-term trends that may be related to global climate change. Article in Journal/Newspaper Antarc* Antarctica Université Toulouse III - Paul Sabatier: HAL-UPS Atmosphere 11 8 836