Temperature estimation at the beginning of the last millennium in western Greenland: preliminary results from the application of a degree‑day glaciological model on the Lyngmarksbræen glacier
International audience The last millennium is deined as a 'stable' climatic period with anomalies such as the Little Ice Age (LIA: ~1450 AD to 1850 AD), a period marked by low temperatures and associated with a glacier advance. Also the Medieval Climate Anomaly (MCA: ~950 AD to 1250 AD), c...
Published in: | Géomorphologie : relief, processus, environnement |
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Main Authors: | , , , , , , , |
Other Authors: | , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2018
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Subjects: | |
Online Access: | https://hal.archives-ouvertes.fr/hal-02349964 https://hal.archives-ouvertes.fr/hal-02349964/document https://hal.archives-ouvertes.fr/hal-02349964/file/BIETTE_et_al_2018.pdf https://doi.org/10.4000/geomorphologie.11977 |