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)...
Published in: | Atmosphere |
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Main Authors: | , , , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2020
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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 |
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ftutoulouse3hal:oai:HAL:hal-03043267v1 |
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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 |
_version_ |
1810492735313936384 |
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 |