%0 Journal Article %J Climate Dynamics %D 2013 %T Regional and global projections of twenty-first century glacier mass changes in response to climate scenarios from global climate models %A Valentina Radić %A Andrew Bliss %A Beedlow, A.Cody %A Regine Hock %A Miles, Evan %A J. Graham Cogley %K Global climate models %K Projections of sea level rise %K Regional and global glacier mass changes %B Climate Dynamics %P 1-22 %G eng %U http://dx.doi.org/10.1007/s00382-013-1719-7 %R 10.1007/s00382-013-1719-7 %0 Journal Article %J Nature Geoscience %D 2011 %T Regionally differentiated contribution of mountain glaciers and ice caps to future sea-level rise %A Valentina Radić %A Regine Hock %B Nature Geoscience %V 4 %P 91–94 %G eng %R 10.1038/NGEO1052 %0 Journal Article %J Journal of Geophysical Research %D 2010 %T Regional and global volumes of glaciers derived from statistical upscaling of glacier inventory data %A Valentina Radić %A Regine Hock %B Journal of Geophysical Research %V 115 %P F01010 %G eng %R 10.1029/2009JF001373 %0 Journal Article %J Geophysical Research Letters %D 2009 %T Mountain glaciers and ice caps around Antarctica make a large sea-level rise contribution %A Regine Hock %A de Woul, M. %A Valentina Radić %A Dyurgerov, M. %B Geophysical Research Letters %V 36 %P L07501 %G eng %0 Journal Article %J Journal of Glaciology %D 2008 %T Analysis of scaling methods in deriving future volume evolutions of valley glaciers %A Valentina Radić %A Regine Hock %A Oerlemans, J. %B Journal of Glaciology %V 54 %P 601–612 %G eng %0 Journal Article %J Annals of glaciology %D 2007 %T Climate sensitivity of Storglaciaren, Sweden: an intercomparison of mass-balance models using ERA-40 re-analysis and regional climate model data %A Regine Hock %A Valentina Radić %A de Woul, M. %B Annals of glaciology %V 46 %P 342–348 %G eng %0 Journal Article %J Annals of Glaciology %D 2007 %T Volumearea scaling vs flowline modelling in glacier volume projections %A Valentina Radić %A Regine Hock %A Oerlemans, J. %B Annals of Glaciology %V 46 %P 234–240 %G eng