TCD - Latest Articleshttp://www.the-cryosphere-discuss.net/2010-03-12T08:29:00+01:00Copernicus Electronic Production Support Officehttp://www.the-cryosphere-discuss.net/4/233/2010/The effect of more realistic forcings and boundary conditions on the modelled geometry and sensitivity of the Greenland ice-sheetThe effect of more realistic forcings and boundary conditions on the modelled geometry and sensitivity of the Greenland ice-sheet, E. J. Stone, D. J. Lunt, I. C. Rutt, and E. Hanna, The Cryosphere Discussions, 4, 233-285, 2010Copernicus Electronic Production Support Office2010-03-12T00:00:00+01:002010-03-12T00:00:00+01:00http://www.the-cryosphere-discuss.net/4/207/2010/Degree-day modelling of the surface mass balance of Urumqi Glacier No. 1, Tian Shan, ChinaDegree-day modelling of the surface mass balance of Urumqi Glacier No. 1, Tian Shan, China, E. Huintjes, H. Li, T. Sauter, Z. Li, and C. Schneider, The Cryosphere Discussions, 4, 207-232, 2010Copernicus Electronic Production Support Office2010-03-03T00:00:00+01:002010-03-03T00:00:00+01:00http://www.the-cryosphere-discuss.net/4/183/2010/An algorithm to detect sea ice leads using AMSR-E passive microwave imageryAn algorithm to detect sea ice leads using AMSR-E passive microwave imagery, J. Röhrs and L. Kaleschke, The Cryosphere Discussions, 4, 183-206, 2010Copernicus Electronic Production Support Office2010-02-22T00:00:00+01:002010-02-22T00:00:00+01:00http://www.the-cryosphere-discuss.net/4/163/2010/An explanation for the dark region in the western melt zone of the Greenland ice sheetAn explanation for the dark region in the western melt zone of the Greenland ice sheet, I. G. M. Wientjes and J. Oerlemans, The Cryosphere Discussions, 4, 163-181, 2010Copernicus Electronic Production Support Office2010-02-11T00:00:00+01:002010-02-11T00:00:00+01:00http://www.the-cryosphere-discuss.net/4/153/2010/Brief communication: ikaite (CaCO<sub>3</sub>*6H<sub>2</sub>O) discovered in Arctic sea iceBrief communication: ikaite (CaCO<sub>3</sub>*6H<sub>2</sub>O) discovered in Arctic sea ice, G. S. Dieckmann, G. Nehrke, C. Uhlig, J. Göttlicher, S. Gerland, M. A. Granskog, and D. N. Thomas, The Cryosphere Discussions, 4, 153-161, 2010Copernicus Electronic Production Support Office2010-02-09T00:00:00+01:002010-02-09T00:00:00+01:00http://www.the-cryosphere-discuss.net/4/121/2010/Modelling snowdrift sublimation on an Antarctic ice shelfModelling snowdrift sublimation on an Antarctic ice shelf, J. T. M. Lenaerts, M. R. van den Broeke, S. J. Déry, G. König-Langlo, J. Ettema, and P. Kuipers Munneke, The Cryosphere Discussions, 4, 121-152, 2010Copernicus Electronic Production Support Office2010-02-09T00:00:00+01:002010-02-09T00:00:00+01:00http://www.the-cryosphere-discuss.net/4/77/2010/Applicability of time-lapse refraction seismic tomography for the detection of ground ice degradationApplicability of time-lapse refraction seismic tomography for the detection of ground ice degradation, C. Hilbich, The Cryosphere Discussions, 4, 77-119, 2010Copernicus Electronic Production Support Office2010-01-27T00:00:00+01:002010-01-27T00:00:00+01:00http://www.the-cryosphere-discuss.net/4/31/2010/Monitoring ice shelf velocities from repeat MODIS and Landsat data – a method study on the Larsen C ice shelf, Antarctic Peninsula, and 10 other ice shelves around AntarcticaMonitoring ice shelf velocities from repeat MODIS and Landsat data – a method study on the Larsen C ice shelf, Antarctic Peninsula, and 10 other ice shelves around Antarctica, T. Haug, A. Kääb, and P. Skvarca, The Cryosphere Discussions, 4, 31-75, 2010Copernicus Electronic Production Support Office2010-01-14T00:00:00+01:002010-01-14T00:00:00+01:00http://www.the-cryosphere-discuss.net/4/1/2010/Spatial and temporal variability of snow depth and SWE in a small mountain catchmentSpatial and temporal variability of snow depth and SWE in a small mountain catchment, T. Grünewald, M. Schirmer, R. Mott, and M. Lehning, The Cryosphere Discussions, 4, 1-30, 2010Copernicus Electronic Production Support Office2010-01-13T00:00:00+01:002010-01-13T00:00:00+01:00