TC - Latest Articleshttp://www.the-cryosphere.net/2008-07-17T15:39:50+02:00Copernicus Electronic Production Support Officehttp://www.the-cryosphere.net/2/77/2008/Analytical solutions for the surface response to small amplitude perturbations in boundary data in the shallow-ice-stream approximationAnalytical solutions for the surface response to small amplitude perturbations in boundary data in the shallow-ice-stream approximation, G. H. Gudmundsson, The Cryosphere, 2, 77-93, 2008Copernicus Electronic Production Support Office2008-07-16T00:00:00+02:002008-07-16T00:00:00+02:00http://www.the-cryosphere.net/2/67/2008/The ISMIP-HOM benchmark experiments performed using the Finite-Element code ElmerThe ISMIP-HOM benchmark experiments performed using the Finite-Element code Elmer, O. Gagliardini and T. Zwinger, The Cryosphere, 2, 67-76, 2008Copernicus Electronic Production Support Office2008-06-13T00:00:00+02:002008-06-13T00:00:00+02:00http://www.the-cryosphere.net/2/53/2008/Is snow sublimation important in the alpine water balance?Is snow sublimation important in the alpine water balance?, U. Strasser, M. Bernhardt, M. Weber, G. E. Liston, and W. Mauser, The Cryosphere, 2, 53-66, 2008Copernicus Electronic Production Support Office2008-05-23T00:00:00+02:002008-05-23T00:00:00+02:00