2021
Seasonal dynamics of snow ablation on selected glaciers in central Spitsbergen derived from Sentinel-2 satellite images
KAVAN, Jan a Vincent HAAGMANSZákladní údaje
Originální název
Seasonal dynamics of snow ablation on selected glaciers in central Spitsbergen derived from Sentinel-2 satellite images
Autoři
KAVAN, Jan (203 Česká republika, garant, domácí) a Vincent HAAGMANS
Vydání
Journal of Glaciology, Cambridge University Press, 2021, 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: 4.278
Kód RIV
RIV/00216224:14310/21:00119356
Organizační jednotka
Přírodovědecká fakulta
UT WoS
000695957300018
Klíčová slova anglicky
Glacier ablation phenomena; glacier mass balance; snow; wind-blown snow
Štítky
Příznaky
Mezinárodní význam, Recenzováno
Změněno: 7. 12. 2021 11:19, Mgr. Marie Šípková, DiS.
Anotace
V originále
The dynamics of seasonal snow ablation on six glaciers in central Spitsbergen (Dicksonland) were assessed by examining a set of Sentinel-2 satellite images covering the summer ablation season for the period 2016-19. All glaciers lost 80% or more of their surface snow cover during the studied ablation seasons. This bolsters the recently observed trend of local glacier thinning, even at higher altitudes. Snow ablation dynamics are highly dependent on the glaciers altitudes, their position relative to the prevailing wind direction and the exposure to insolation. The accumulation areas of the studied glaciers were delimited based on the overlap of the minimum extent of snow-covered areas in the four consecutive studied summer seasons. The high temporal and spatial resolutions of available images enabled a detailed description of the seasonal snow ablation dynamics. Moreover, an estimate of the average number of days with below threshold glacier snow cover was made. This study contributes to our understanding of recent processes and might further support the modelling of glacier melt and subsequent runoff.
Návaznosti
GA20-20240S, projekt VaV |
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MUNI/G/1540/2019, interní kód MU |
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