Post Little Ice Age changes in the Morsárjökull and Skaftafellsjökull proglacial landscape (Southeast of Iceland)
International audience The Global Warming which started since the end of the Little Ice Age (mid-19th Century in Iceland), leads to the retreat of glacier fronts. Thus, the terminus of the Morsárjökull and Skaftafellsjökull glaciers, outlets of the Vatnajökull ice cap, have receded about 1 to 1.5 km...
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2007
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ftunivlimoges:oai:HAL:hal-00466850v1 2024-02-11T09:59:07+01:00 Post Little Ice Age changes in the Morsárjökull and Skaftafellsjökull proglacial landscape (Southeast of Iceland) Roussel, Erwan Chenet, Marie Decaulne, Armelle Maison des Sciences de l'Homme de Clermont-Ferrand (MSH Clermont) Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Centre National de la Recherche Scientifique (CNRS) Laboratoire de Géographie Physique et Environnementale (GEOLAB) Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut Sciences de l'Homme et de la Société (IR SHS UNILIM) Université de Limoges (UNILIM)-Université de Limoges (UNILIM)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Université Clermont Auvergne (UCA) Laboratoire de géographie physique : Environnements Quaternaires et Actuels (LGP) Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS) Skaftafell, Iceland 2007-05-02 https://hal.science/hal-00466850 en eng HAL CCSD hal-00466850 https://hal.science/hal-00466850 . 37 th Annual Arctic Workshop https://hal.science/hal-00466850 . 37 th Annual Arctic Workshop, May 2007, Skaftafell, Iceland Post Little Ice Age Sandur Glacier Retreat Slopes [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology info:eu-repo/semantics/conferenceObject Conference poster 2007 ftunivlimoges 2024-01-23T23:37:11Z International audience The Global Warming which started since the end of the Little Ice Age (mid-19th Century in Iceland), leads to the retreat of glacier fronts. Thus, the terminus of the Morsárjökull and Skaftafellsjökull glaciers, outlets of the Vatnajökull ice cap, have receded about 1 to 1.5 km since the LIA. This retreat induces new dynamics in the glacier foreland, especially related to glacial meltwater and recent deglaciated slopes development. Lichenometric measures on moraine ridges and paleosandurs provide the opportunity to reconstruct the evolution of the Morsárjökull and the Skaftafellsjökull the proglacial areas. Conference Object Arctic glacier Ice cap Iceland Vatnajökull Université de Limoges: HAL Morsárjökull ENVELOPE(-16.904,-16.904,64.095,64.095) Skaftafell ENVELOPE(-16.940,-16.940,63.999,63.999) Skaftafellsjökull ENVELOPE(-16.881,-16.881,64.063,64.063) Vatnajökull ENVELOPE(-16.823,-16.823,64.420,64.420) |
institution |
Open Polar |
collection |
Université de Limoges: HAL |
op_collection_id |
ftunivlimoges |
language |
English |
topic |
Post Little Ice Age Sandur Glacier Retreat Slopes [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology |
spellingShingle |
Post Little Ice Age Sandur Glacier Retreat Slopes [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology Roussel, Erwan Chenet, Marie Decaulne, Armelle Post Little Ice Age changes in the Morsárjökull and Skaftafellsjökull proglacial landscape (Southeast of Iceland) |
topic_facet |
Post Little Ice Age Sandur Glacier Retreat Slopes [SDU.STU.GM]Sciences of the Universe [physics]/Earth Sciences/Geomorphology |
description |
International audience The Global Warming which started since the end of the Little Ice Age (mid-19th Century in Iceland), leads to the retreat of glacier fronts. Thus, the terminus of the Morsárjökull and Skaftafellsjökull glaciers, outlets of the Vatnajökull ice cap, have receded about 1 to 1.5 km since the LIA. This retreat induces new dynamics in the glacier foreland, especially related to glacial meltwater and recent deglaciated slopes development. Lichenometric measures on moraine ridges and paleosandurs provide the opportunity to reconstruct the evolution of the Morsárjökull and the Skaftafellsjökull the proglacial areas. |
author2 |
Maison des Sciences de l'Homme de Clermont-Ferrand (MSH Clermont) Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Centre National de la Recherche Scientifique (CNRS) Laboratoire de Géographie Physique et Environnementale (GEOLAB) Université Blaise Pascal - Clermont-Ferrand 2 (UBP)-Institut Sciences de l'Homme et de la Société (IR SHS UNILIM) Université de Limoges (UNILIM)-Université de Limoges (UNILIM)-Université Clermont Auvergne 2017-2020 (UCA 2017-2020 )-Centre National de la Recherche Scientifique (CNRS)-Université Clermont Auvergne (UCA) Laboratoire de géographie physique : Environnements Quaternaires et Actuels (LGP) Université Paris 1 Panthéon-Sorbonne (UP1)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS) |
format |
Conference Object |
author |
Roussel, Erwan Chenet, Marie Decaulne, Armelle |
author_facet |
Roussel, Erwan Chenet, Marie Decaulne, Armelle |
author_sort |
Roussel, Erwan |
title |
Post Little Ice Age changes in the Morsárjökull and Skaftafellsjökull proglacial landscape (Southeast of Iceland) |
title_short |
Post Little Ice Age changes in the Morsárjökull and Skaftafellsjökull proglacial landscape (Southeast of Iceland) |
title_full |
Post Little Ice Age changes in the Morsárjökull and Skaftafellsjökull proglacial landscape (Southeast of Iceland) |
title_fullStr |
Post Little Ice Age changes in the Morsárjökull and Skaftafellsjökull proglacial landscape (Southeast of Iceland) |
title_full_unstemmed |
Post Little Ice Age changes in the Morsárjökull and Skaftafellsjökull proglacial landscape (Southeast of Iceland) |
title_sort |
post little ice age changes in the morsárjökull and skaftafellsjökull proglacial landscape (southeast of iceland) |
publisher |
HAL CCSD |
publishDate |
2007 |
url |
https://hal.science/hal-00466850 |
op_coverage |
Skaftafell, Iceland |
long_lat |
ENVELOPE(-16.904,-16.904,64.095,64.095) ENVELOPE(-16.940,-16.940,63.999,63.999) ENVELOPE(-16.881,-16.881,64.063,64.063) ENVELOPE(-16.823,-16.823,64.420,64.420) |
geographic |
Morsárjökull Skaftafell Skaftafellsjökull Vatnajökull |
geographic_facet |
Morsárjökull Skaftafell Skaftafellsjökull Vatnajökull |
genre |
Arctic glacier Ice cap Iceland Vatnajökull |
genre_facet |
Arctic glacier Ice cap Iceland Vatnajökull |
op_source |
. 37 th Annual Arctic Workshop https://hal.science/hal-00466850 . 37 th Annual Arctic Workshop, May 2007, Skaftafell, Iceland |
op_relation |
hal-00466850 https://hal.science/hal-00466850 |
_version_ |
1790595104729202688 |