Articles | Volume 10, issue 3
The Cryosphere, 10, 1331–1337, 2016
https://doi.org/10.5194/tc-10-1331-2016
The Cryosphere, 10, 1331–1337, 2016
https://doi.org/10.5194/tc-10-1331-2016

Comment/reply 29 Jun 2016

Comment/reply | 29 Jun 2016

Basal buoyancy and fast-moving glaciers: in defense of analytic force balance

C. J. van der Veen C. J. van der Veen
  • Department of Geography and Atmospheric Science, University of Kansas, 203 Lindley Hall, 1475 Jayhawk Blvd, Lawrence, KS 66045, USA

Abstract. The geometric approach to force balance advocated by T. Hughes in a series of publications has challenged the analytic approach by implying that the latter does not adequately account for basal buoyancy on ice streams, thereby neglecting the contribution to the gravitational driving force associated with this basal buoyancy. Application of the geometric approach to Byrd Glacier, Antarctica, yields physically unrealistic results, and it is argued that this is because of a key limiting assumption in the geometric approach. A more traditional analytic treatment of force balance shows that basal buoyancy does not affect the balance of forces on ice streams, except locally perhaps, through bridging effects.

Short summary
This paper evaluates the geometric force balance, with application to Byrd Glacier, Antarctica. It is concluded that this approach does not yield physically reasonable results.