Documentation for PISM, the Parallel Ice Sheet Model

Differences

This shows you the differences between two versions of the page.

Link to this comparison view

applications:201504 [2015/04/02 17:57] (current)
Ed Bueler created by copy of future_applications page
Line 1: Line 1:
 +====== April 2015 ======
 +<div left 49% centeralign>​
 +[[http://​www.the-cryosphere.net/​9/​631/​2015/​tc-9-631-2015.html|{{:​applications:​feldmannlevermann2015.png?​380 |}}]]
  
 +<​html>​
 +&nbsp;
 +</​html>​
 +
 +Click the image to go to //The Cryosphere//​ page.
 +</​div>​
 +
 +<div right 44%>
 +| **Interaction of marine ice-sheet instabilities in two drainage basins: simple scaling of geometry and transition time** ||
 +| **investigators**:​ | [[https://​www.pik-potsdam.de/​members/​frieler|J. Feldmann]] and A. Levermann|
 +| **journal**:​ | [[http://​www.the-cryosphere.net/​|The Cryosphere]] |
 +
 +The marine ice-sheet instability generally comes from the ocean side of the ice sheet. ​ Using a flow-line geometry in PISM, this paper investigates whether instability can be triggered from the direction of the ice divide. ​ The authors find that the instability in one basin can induce a destabilization in the other. ​ The underlying mechanism is dynamic thinning and consequent motion of the ice divide. ​ They conclude that for the three-dimensional case, the possibility of drainage basin interaction on timescales on the order of 1 kyr or larger cannot be excluded and needs further investigation.
 +
 +</​div>​
 +<WRAP clear></​WRAP>​
applications/201504.txt ยท Last modified: 2015/04/02 17:57 by Ed Bueler
© 2016 by PISM | webmaster