2023
Persistent mass loss of Triangular Glacier, James Ross Island, north-eastern Antarctic Peninsula
ENGEL, Zbyněk; Kamil LÁSKA; Jan KAVAN a Jana SMOLÍKOVÁZákladní údaje
Originální název
Persistent mass loss of Triangular Glacier, James Ross Island, north-eastern Antarctic Peninsula
Autoři
ENGEL, Zbyněk; Kamil LÁSKA; Jan KAVAN a Jana SMOLÍKOVÁ
Vydání
Journal of Glaciology, Cambridge University Press, 2023, 0022-1430
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10508 Physical geography
Stát vydavatele
Velká Británie a Severní Irsko
Utajení
není předmětem státního či obchodního tajemství
Odkazy
Impakt faktor
Impact factor: 2.800
Označené pro přenos do RIV
Ano
Kód RIV
RIV/00216224:14310/23:00129985
Organizační jednotka
Přírodovědecká fakulta
UT WoS
EID Scopus
Klíčová slova anglicky
Antarctic glaciology; climate change; glacier mass balance; glacier meteorology; glacier volume
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 21. 3. 2024 11:25, Mgr. Marie Novosadová Šípková, DiS.
Anotace
V originále
The retreat rates of Triangular Glacier since 1979 and its mass changes during the period 2014/15-2019/20 indicate the sensitive response of small ice masses on the eastern side of the Antarctic Peninsula to air temperature evolution. This cirque glacier in the northern part of James Ross Island receded rapidly during the period of regional warming in the late 20th century, losing 30.8% of its surface area between 1979 and 2006 (-1.7% a(-1)). The retreat rate then dropped to -0.3% a(-1) following the regional cooling trend, but started to accelerate again (-0.8 to -2.3% a(-1)) with increasing air temperature since the summer 2014/15. Since the glaciological year 2015/16, Triangular Glacier has experienced enhanced snow melt, wind scour and permanent mass loss with annual mass balance ranging from -0.08 +/- 0.35 to -0.56 +/- 0.25 m w.e. The largest mass loss was observed in the glaciological year 2019/20, which included the warmest summer of the observation period. The cumulative mass balance of -1.66 +/- 0.83 m w.e. over the years 2014/15-2019/20 is consistent with the termination of the positive mass-balance period that occurred in the north-eastern Antarctic Peninsula from 2009/10 to 2014/15.
Návaznosti
| GA20-20240S, projekt VaV |
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| LM2015078, projekt VaV |
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| VAN 2021, interní kód MU |
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