Evolution of glaciers in the Ecuadorian Andes since the 1950s and its contribution to the study of the climate change in the inner tropics

Climate of the tropical regions plays an important role in the balance of the global climate system. Consequently, it appears essential to understand its functioning and variability to apprehend at best the effects of climate change. In tropical regions where climate projections show an important wa...

Full description

Bibliographic Details
Main Author: Basantes-Serrano, Rubén
Other Authors: Laboratoire d'étude des transferts en hydrologie et environnement (LTHE), Observatoire des Sciences de l'Univers de Grenoble (OSUG), Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Institut National Polytechnique de Grenoble (INPG)-Centre National de la Recherche Scientifique (CNRS), Université Grenoble Alpes, Bernard Francou, Antoine Rabatel
Format: Doctoral or Postdoctoral Thesis
Language:French
Published: HAL CCSD 2015
Subjects:
Online Access:https://theses.hal.science/tel-01219778
https://theses.hal.science/tel-01219778/document
https://theses.hal.science/tel-01219778/file/BASANTES_2015_archivage.pdf
id ftunigrenoble:oai:HAL:tel-01219778v1
record_format openpolar
institution Open Polar
collection Université Grenoble Alpes: HAL
op_collection_id ftunigrenoble
language French
topic Glaciology
Aerial Photogrammetry
Remote Sensing
Climate
Hidrology
Ecuador
Glaciares tropicales
Balance de masa
Variabilidad climática
Fotogrametría
Glaciologie
Photogrammétrie aérienne
Télédétection
Climat
Hydrologie
Equateur
[SDE.MCG]Environmental Sciences/Global Changes
spellingShingle Glaciology
Aerial Photogrammetry
Remote Sensing
Climate
Hidrology
Ecuador
Glaciares tropicales
Balance de masa
Variabilidad climática
Fotogrametría
Glaciologie
Photogrammétrie aérienne
Télédétection
Climat
Hydrologie
Equateur
[SDE.MCG]Environmental Sciences/Global Changes
Basantes-Serrano, Rubén
Evolution of glaciers in the Ecuadorian Andes since the 1950s and its contribution to the study of the climate change in the inner tropics
topic_facet Glaciology
Aerial Photogrammetry
Remote Sensing
Climate
Hidrology
Ecuador
Glaciares tropicales
Balance de masa
Variabilidad climática
Fotogrametría
Glaciologie
Photogrammétrie aérienne
Télédétection
Climat
Hydrologie
Equateur
[SDE.MCG]Environmental Sciences/Global Changes
description Climate of the tropical regions plays an important role in the balance of the global climate system. Consequently, it appears essential to understand its functioning and variability to apprehend at best the effects of climate change. In tropical regions where climate projections show an important warming at high elevations, glaciers are the first victims of the increase in temperature. But they also appear as accurate indicators of climatic variations. Until now, glaciological observations carried out in the inner tropics on Glacier Antisana 15 have been used in multiple studies that helped understand physical processes controlling glacial melt in this region. However, the latter studies have not taken into account the spatial and temporal representativeness of these processes at the scale of the whole ice cap. Based on geodetic observations, the present study shows the spatial and temporal evaluation of nine glaciers during four periods spread over the last fifty years (1956-2014). Situated in the volcanic cone of Antisana, these glaciers were chosen according to their orientation and morphological characteristics. In a first phase, we evaluated existing glaciological observations made on Glacier Antisana 15α between 1995 and 2012. Our results suggest an overestimation of at least 5 m w.e. of the cumulated mass balance of this glacier. This excess in the ablation rate was caused by an underestimation of the annual accumulation measurement, linked to the difficulty of identifying the layer separating two hydrological years. In a second phase, we analysed the geometrical fluctuations of glaciers: generally there is a negative trend with a loss rate of -0.5 w.e. per year, leading to a retreat of 38% of the ice cap surface area. However, this trend is not constant. We highlighted a contrasting behaviour from one period to the other: some characteristics draw attention, such as the fact that the mass balance was very negative between 1956 and 1964 (-1.3 m w.e. per year) when in a more recent period (1998 to 2009) ...
author2 Laboratoire d'étude des transferts en hydrologie et environnement (LTHE)
Observatoire des Sciences de l'Univers de Grenoble (OSUG)
Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Institut National Polytechnique de Grenoble (INPG)-Centre National de la Recherche Scientifique (CNRS)
Université Grenoble Alpes
Bernard Francou
Antoine Rabatel
format Doctoral or Postdoctoral Thesis
author Basantes-Serrano, Rubén
author_facet Basantes-Serrano, Rubén
author_sort Basantes-Serrano, Rubén
title Evolution of glaciers in the Ecuadorian Andes since the 1950s and its contribution to the study of the climate change in the inner tropics
title_short Evolution of glaciers in the Ecuadorian Andes since the 1950s and its contribution to the study of the climate change in the inner tropics
title_full Evolution of glaciers in the Ecuadorian Andes since the 1950s and its contribution to the study of the climate change in the inner tropics
title_fullStr Evolution of glaciers in the Ecuadorian Andes since the 1950s and its contribution to the study of the climate change in the inner tropics
title_full_unstemmed Evolution of glaciers in the Ecuadorian Andes since the 1950s and its contribution to the study of the climate change in the inner tropics
title_sort evolution of glaciers in the ecuadorian andes since the 1950s and its contribution to the study of the climate change in the inner tropics
publisher HAL CCSD
publishDate 2015
url https://theses.hal.science/tel-01219778
https://theses.hal.science/tel-01219778/document
https://theses.hal.science/tel-01219778/file/BASANTES_2015_archivage.pdf
genre Ice cap
genre_facet Ice cap
op_source https://theses.hal.science/tel-01219778
Milieux et Changements globaux. Université Grenoble Alpes, 2015. Français. ⟨NNT : 2015GREAU009⟩
op_relation NNT: 2015GREAU009
tel-01219778
https://theses.hal.science/tel-01219778
https://theses.hal.science/tel-01219778/document
https://theses.hal.science/tel-01219778/file/BASANTES_2015_archivage.pdf
op_rights info:eu-repo/semantics/OpenAccess
_version_ 1802645457855315968
spelling ftunigrenoble:oai:HAL:tel-01219778v1 2024-06-23T07:53:41+00:00 Evolution of glaciers in the Ecuadorian Andes since the 1950s and its contribution to the study of the climate change in the inner tropics Contribution à l’étude de l’évolution des glaciers et du changement climatique dans les Andes équatoriennes depuis les années 1950 Basantes-Serrano, Rubén Laboratoire d'étude des transferts en hydrologie et environnement (LTHE) Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Institut National Polytechnique de Grenoble (INPG)-Centre National de la Recherche Scientifique (CNRS) Université Grenoble Alpes Bernard Francou Antoine Rabatel 2015-07-08 https://theses.hal.science/tel-01219778 https://theses.hal.science/tel-01219778/document https://theses.hal.science/tel-01219778/file/BASANTES_2015_archivage.pdf fr fre HAL CCSD NNT: 2015GREAU009 tel-01219778 https://theses.hal.science/tel-01219778 https://theses.hal.science/tel-01219778/document https://theses.hal.science/tel-01219778/file/BASANTES_2015_archivage.pdf info:eu-repo/semantics/OpenAccess https://theses.hal.science/tel-01219778 Milieux et Changements globaux. Université Grenoble Alpes, 2015. Français. ⟨NNT : 2015GREAU009⟩ Glaciology Aerial Photogrammetry Remote Sensing Climate Hidrology Ecuador Glaciares tropicales Balance de masa Variabilidad climática Fotogrametría Glaciologie Photogrammétrie aérienne Télédétection Climat Hydrologie Equateur [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/doctoralThesis Theses 2015 ftunigrenoble 2024-06-04T00:15:32Z Climate of the tropical regions plays an important role in the balance of the global climate system. Consequently, it appears essential to understand its functioning and variability to apprehend at best the effects of climate change. In tropical regions where climate projections show an important warming at high elevations, glaciers are the first victims of the increase in temperature. But they also appear as accurate indicators of climatic variations. Until now, glaciological observations carried out in the inner tropics on Glacier Antisana 15 have been used in multiple studies that helped understand physical processes controlling glacial melt in this region. However, the latter studies have not taken into account the spatial and temporal representativeness of these processes at the scale of the whole ice cap. Based on geodetic observations, the present study shows the spatial and temporal evaluation of nine glaciers during four periods spread over the last fifty years (1956-2014). Situated in the volcanic cone of Antisana, these glaciers were chosen according to their orientation and morphological characteristics. In a first phase, we evaluated existing glaciological observations made on Glacier Antisana 15α between 1995 and 2012. Our results suggest an overestimation of at least 5 m w.e. of the cumulated mass balance of this glacier. This excess in the ablation rate was caused by an underestimation of the annual accumulation measurement, linked to the difficulty of identifying the layer separating two hydrological years. In a second phase, we analysed the geometrical fluctuations of glaciers: generally there is a negative trend with a loss rate of -0.5 w.e. per year, leading to a retreat of 38% of the ice cap surface area. However, this trend is not constant. We highlighted a contrasting behaviour from one period to the other: some characteristics draw attention, such as the fact that the mass balance was very negative between 1956 and 1964 (-1.3 m w.e. per year) when in a more recent period (1998 to 2009) ... Doctoral or Postdoctoral Thesis Ice cap Université Grenoble Alpes: HAL