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Titel Brief Communication: On the magnitude and frequency of Khurdopin glacier surge events
VerfasserIn D. J. Quincey, A. Luckman
Medientyp Artikel
Sprache Englisch
ISSN 1994-0416
Digitales Dokument URL
Erschienen In: The Cryosphere ; 8, no. 2 ; Nr. 8, no. 2 (2014-04-03), S.571-574
Datensatznummer 250116086
Publikation (Nr.) Volltext-Dokument vorhandencopernicus.org/tc-8-571-2014.pdf
 
Zusammenfassung
The return periods of Karakoram glacier surges are poorly quantified. Here, we present evidence of an historic surge of the Khurdopin Glacier that began in the mid-1970s and peaked in 1979. Measured surface displacements reached >5 km a−1, two orders of magnitude faster than during quiescence. The Khurdopin Glacier next surged in the late 1990s, equating to a return period of 20 years. Surge evolution in the two events shows remarkable similarity suggesting a common trigger. Surge activity in the Karakoram needs to be better understood if accurate mass balance assessments of Hindu-Kush–Karakoram–Himalaya glaciers are to be made.
 
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