Comment on “Friction at the bed does not control fast glacier flow”
Author(s) -
Brent Minchew,
Colin Meyer,
Samuel S. Pegler,
Bradley P. Lipovsky,
A. W. Rempel,
G. Hilmar Gudmundsson,
Neal R. Iverson
Publication year - 2019
Publication title -
science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 12.556
H-Index - 1186
eISSN - 1095-9203
pISSN - 0036-8075
DOI - 10.1126/science.aau6055
Subject(s) - drag , glacier , geology , flow (mathematics) , mechanics , stress (linguistics) , physics , geomorphology , linguistics , philosophy
Stearns and van der Veen (Reports, 20 July 2018, p. 273) conclude that fast glacier sliding is independent of basal drag (friction), even where drag balances most of the driving stress. This conclusion raises fundamental physical issues, the most striking of which is that sliding velocity would be independent of stresses imparted through the ice column, including gravitational driving stress.
Accelerating Research
Robert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom
Address
John Eccles HouseRobert Robinson Avenue,
Oxford Science Park, Oxford
OX4 4GP, United Kingdom