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@proceedings{1395014,
author = {Láska, Kamil and Engel, Zbyněk and Nývlt, Daniel and Stachoň, Zdeněk and Lippl, Stefan and Braun, Matthias},
booktitle = {The EGU General Assembly 2017},
keywords = {Antarctica; James Ross Island;glacier;snow; ablation; accumulation; surface mass balance;},
language = {eng},
title = {Response of glacier mass on recent temperature cooling in northeastern Antarctic Peninsula},
url = {https://www.egu2017.eu/},
year = {2017}
}
TY - CONF
ID - 1395014
AU - Láska, Kamil - Engel, Zbyněk - Nývlt, Daniel - Stachoň, Zdeněk - Lippl, Stefan - Braun, Matthias
PY - 2017
TI - Response of glacier mass on recent temperature cooling in northeastern Antarctic Peninsula
KW - Antarctica
KW - James Ross Island;glacier;snow
KW - ablation
KW - accumulation
KW - surface mass balance;
UR - https://www.egu2017.eu/
L2 - https://www.egu2017.eu/
N2 - We have studied annual changes of mass balance and equilibrium line altitude of Whisky Glacier, a cold-bases land-terminating valley glacier (~2.4 km2), in the northern part of James Ross Island. The surface mass balance changes were estimated based on ablation stake measurements, carried out in late summer over the five years period (2009/10–2013/14). In addition, glacier surface velocity and area changes were determined for this period from aerial and satellite imageries based digital elevation models. Automatic weather stations in the northern part of James Ross Island reflect the recent cold period and indicate a prominent cooling by 1.2 °C over the period 2006–2015. A response of glaciers on colder conditions can be observed throughout the area where negative mass changes turned to predominantly positive values after 2009.
ER -
LÁSKA, Kamil, Zbyněk ENGEL, Daniel NÝVLT, Zdeněk STACHOŇ, Stefan LIPPL a Matthias BRAUN. Response of glacier mass on recent temperature cooling in northeastern Antarctic Peninsula. In \textit{The EGU General Assembly 2017}. 2017. ISSN~1029-7006.
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