Evaluation of cloudiness over Monte San Valentín, Northern Patagonia Icefield, from 2000 to 2008 using MODIS satellite images: implications for paleoclimate investigations from ice cores

International audience An unexpectedly low annual net accumulation (20 cm w.e. a-1) has been inferred from analyses of a firn core extracted from Glaciar Monte San Valentín, Northern Patagonia Icefield (46835' S, 73819' W; 3747 m a.s.l.). We test a hypothesis linking the low accumulation t...

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Published in:Journal of Glaciology
Main Authors: Vimeux, Françoise, Maignan, Fabienne, Reutenauer, Corentin, Pouyaud, Bernard
Other Authors: Hydrosciences Montpellier (HSM), Institut national des sciences de l'Univers (INSU - CNRS)-Institut de Recherche pour le Développement (IRD)-Université Montpellier 2 - Sciences et Techniques (UM2)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS), Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Glaces et Continents, Climats et Isotopes Stables (GLACCIOS), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Modélisation des Surfaces et Interfaces Continentales (MOSAIC)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2011
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-03106355
https://hal.archives-ouvertes.fr/hal-03106355/document
https://hal.archives-ouvertes.fr/hal-03106355/file/fichier8.pdf
https://doi.org/10.3189/002214311796405915
id ftccsdartic:oai:HAL:hal-03106355v1
record_format openpolar
institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
Vimeux, Françoise
Maignan, Fabienne
Reutenauer, Corentin
Pouyaud, Bernard
Evaluation of cloudiness over Monte San Valentín, Northern Patagonia Icefield, from 2000 to 2008 using MODIS satellite images: implications for paleoclimate investigations from ice cores
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
description International audience An unexpectedly low annual net accumulation (20 cm w.e. a-1) has been inferred from analyses of a firn core extracted from Glaciar Monte San Valentín, Northern Patagonia Icefield (46835' S, 73819' W; 3747 m a.s.l.). We test a hypothesis linking the low accumulation to a frequent lack of cloud cover over the mountain range at this altitude. The cloudiness over Monte San Valentín and surrounding regions is examined using $3000 daily MODIS satellite images from 2000 to 2008. The visual evaluation of the synoptic situation leads to the definition of a daily cloudiness index (EI) for the San Valentín summit and for the regions to the southwest (SW) and northeast (NE). We check its robustness by applying different tests and comparisons. Three levels are assigned for the EI: 'clear' (EI = 0), 'cloudy' (EI = 1) and 'mixed' (EI = 0.5). The results show that the SV cloud cover is similar to the regional cloudiness for more than half the year (54%) and that the case in which the San Valentín summit is clear while both SW and NE regions are cloudy is exceptional (2%). As clouds are necessary to provide precipitation, we show that the low annual net accumulation cannot be explained by an uncommon low cloudiness. This result implies that net accumulation inferred from ice cores in this Andean region must be cautiously interpreted. We also point out that the Andes at this latitude acts as an orographic barrier but without a total blocking of air masses.
author2 Hydrosciences Montpellier (HSM)
Institut national des sciences de l'Univers (INSU - CNRS)-Institut de Recherche pour le Développement (IRD)-Université Montpellier 2 - Sciences et Techniques (UM2)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS)
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
Glaces et Continents, Climats et Isotopes Stables (GLACCIOS)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
Modélisation des Surfaces et Interfaces Continentales (MOSAIC)
format Article in Journal/Newspaper
author Vimeux, Françoise
Maignan, Fabienne
Reutenauer, Corentin
Pouyaud, Bernard
author_facet Vimeux, Françoise
Maignan, Fabienne
Reutenauer, Corentin
Pouyaud, Bernard
author_sort Vimeux, Françoise
title Evaluation of cloudiness over Monte San Valentín, Northern Patagonia Icefield, from 2000 to 2008 using MODIS satellite images: implications for paleoclimate investigations from ice cores
title_short Evaluation of cloudiness over Monte San Valentín, Northern Patagonia Icefield, from 2000 to 2008 using MODIS satellite images: implications for paleoclimate investigations from ice cores
title_full Evaluation of cloudiness over Monte San Valentín, Northern Patagonia Icefield, from 2000 to 2008 using MODIS satellite images: implications for paleoclimate investigations from ice cores
title_fullStr Evaluation of cloudiness over Monte San Valentín, Northern Patagonia Icefield, from 2000 to 2008 using MODIS satellite images: implications for paleoclimate investigations from ice cores
title_full_unstemmed Evaluation of cloudiness over Monte San Valentín, Northern Patagonia Icefield, from 2000 to 2008 using MODIS satellite images: implications for paleoclimate investigations from ice cores
title_sort evaluation of cloudiness over monte san valentín, northern patagonia icefield, from 2000 to 2008 using modis satellite images: implications for paleoclimate investigations from ice cores
publisher HAL CCSD
publishDate 2011
url https://hal.archives-ouvertes.fr/hal-03106355
https://hal.archives-ouvertes.fr/hal-03106355/document
https://hal.archives-ouvertes.fr/hal-03106355/file/fichier8.pdf
https://doi.org/10.3189/002214311796405915
long_lat ENVELOPE(-54.650,-54.650,-61.100,-61.100)
geographic Patagonia
Valentín
geographic_facet Patagonia
Valentín
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_source ISSN: 0022-1430
Journal of Glaciology
https://hal.archives-ouvertes.fr/hal-03106355
Journal of Glaciology, International Glaciological Society, 2011, 57 (202), pp.221-230. ⟨10.3189/002214311796405915⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.3189/002214311796405915
hal-03106355
https://hal.archives-ouvertes.fr/hal-03106355
https://hal.archives-ouvertes.fr/hal-03106355/document
https://hal.archives-ouvertes.fr/hal-03106355/file/fichier8.pdf
doi:10.3189/002214311796405915
IRD: PAR00007898
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.3189/002214311796405915
container_title Journal of Glaciology
container_volume 57
container_issue 202
container_start_page 221
op_container_end_page 230
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spelling ftccsdartic:oai:HAL:hal-03106355v1 2023-05-15T16:57:27+02:00 Evaluation of cloudiness over Monte San Valentín, Northern Patagonia Icefield, from 2000 to 2008 using MODIS satellite images: implications for paleoclimate investigations from ice cores Vimeux, Françoise Maignan, Fabienne Reutenauer, Corentin Pouyaud, Bernard Hydrosciences Montpellier (HSM) Institut national des sciences de l'Univers (INSU - CNRS)-Institut de Recherche pour le Développement (IRD)-Université Montpellier 2 - Sciences et Techniques (UM2)-Université de Montpellier (UM)-Centre National de la Recherche Scientifique (CNRS) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Glaces et Continents, Climats et Isotopes Stables (GLACCIOS) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Modélisation des Surfaces et Interfaces Continentales (MOSAIC) 2011 https://hal.archives-ouvertes.fr/hal-03106355 https://hal.archives-ouvertes.fr/hal-03106355/document https://hal.archives-ouvertes.fr/hal-03106355/file/fichier8.pdf https://doi.org/10.3189/002214311796405915 en eng HAL CCSD International Glaciological Society info:eu-repo/semantics/altIdentifier/doi/10.3189/002214311796405915 hal-03106355 https://hal.archives-ouvertes.fr/hal-03106355 https://hal.archives-ouvertes.fr/hal-03106355/document https://hal.archives-ouvertes.fr/hal-03106355/file/fichier8.pdf doi:10.3189/002214311796405915 IRD: PAR00007898 info:eu-repo/semantics/OpenAccess ISSN: 0022-1430 Journal of Glaciology https://hal.archives-ouvertes.fr/hal-03106355 Journal of Glaciology, International Glaciological Society, 2011, 57 (202), pp.221-230. ⟨10.3189/002214311796405915⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 2011 ftccsdartic https://doi.org/10.3189/002214311796405915 2021-12-19T00:34:53Z International audience An unexpectedly low annual net accumulation (20 cm w.e. a-1) has been inferred from analyses of a firn core extracted from Glaciar Monte San Valentín, Northern Patagonia Icefield (46835' S, 73819' W; 3747 m a.s.l.). We test a hypothesis linking the low accumulation to a frequent lack of cloud cover over the mountain range at this altitude. The cloudiness over Monte San Valentín and surrounding regions is examined using $3000 daily MODIS satellite images from 2000 to 2008. The visual evaluation of the synoptic situation leads to the definition of a daily cloudiness index (EI) for the San Valentín summit and for the regions to the southwest (SW) and northeast (NE). We check its robustness by applying different tests and comparisons. Three levels are assigned for the EI: 'clear' (EI = 0), 'cloudy' (EI = 1) and 'mixed' (EI = 0.5). The results show that the SV cloud cover is similar to the regional cloudiness for more than half the year (54%) and that the case in which the San Valentín summit is clear while both SW and NE regions are cloudy is exceptional (2%). As clouds are necessary to provide precipitation, we show that the low annual net accumulation cannot be explained by an uncommon low cloudiness. This result implies that net accumulation inferred from ice cores in this Andean region must be cautiously interpreted. We also point out that the Andes at this latitude acts as an orographic barrier but without a total blocking of air masses. Article in Journal/Newspaper Journal of Glaciology Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Patagonia Valentín ENVELOPE(-54.650,-54.650,-61.100,-61.100) Journal of Glaciology 57 202 221 230