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Titel	The Cryosphere ; 6, no. 1
Erscheinungsjahr	2012
Medientyp	Stücktitel
ISSN	1994-0416
Erschienen	In: The Cryosphere (TC) ; Nr. 6, no. 1 (2012)
Datensatznummer	93781


Teil von
The Cryosphere (TC)


Teil(e)
Hydrologic controls on coastal suspended sediment plumes around the Greenland Ice Sheet \| V. W. Chu Reformulating the full-Stokes ice sheet model for a more efficient computational solution \| J. K. Dukowicz The impact of a seasonally ice free Arctic Ocean on the temperature, precipitation and surface mass balance of Svalbard \| J. J. Day Comparison of MODIS-derived land surface temperatures with ground surface and air temperature measurements in continuous permafrost terrain \| S. Hachem A minimal model for reconstructing interannual mass balance variability of glaciers in the European Alps \| B. Marzeion Geochemical characterization of supraglacial debris via in situ and optical remote sensing methods: a case study in Khumbu Himalaya, Nepal \| K. A. Casey A three-dimensional full Stokes model of the grounding line dynamics: effect of a pinning point beneath the ice shelf \| L. Favier Basal crevasses in Larsen C Ice Shelf and implications for their global abundance \| A. Luckman A statistical approach to modelling permafrost distribution in the European Alps or similar mountain ranges \| L. Boeckli Corrigendum to "The impact of a seasonally ice free Arctic Ocean on the temperature, precipitation and surface mass balance of Svalbard" published in The Cryosphere, 6, 35–50, 2012 \| J. J. Day Influence of sea ice lead-width distribution on turbulent heat transfer between the ocean and the atmosphere \| S. Marcq Cornice dynamics and meteorological control at Gruvefjellet, Central Svalbard \| S. Vogel Laboratory study of frazil ice accumulation under wave conditions \| S. Rosa How reversible is sea ice loss? \| J. K. Ridley Large surface meltwater discharge from the Kangerlussuaq sector of the Greenland ice sheet during the record-warm year 2010 explained by detailed energy balance observations \| D. As Changes in the marine-terminating glaciers of central east Greenland, 2000–2010 \| K. M. Walsh Derivation and analysis of a high-resolution estimate of global permafrost zonation \| S. Gruber