机译:格陵兰岛低渗透冰板的快速扩张
Univ Colorado Cooperat Inst Res Environm Sci Boulder CO 80309 USA;
Univ Fribourg Dept Geosci Fribourg Switzerland|Univ Zurich Dept Geog Zurich Switzerland;
Geol Survey Denmark & Greenland Copenhagen Denmark;
Bavarian Acad Sci & Humanities Munich Germany;
Univ Washington Dept Earth & Space Sci Seattle WA 98195 USA;
WSL Inst Snow & Avalanche Res SLF Davos Switzerland|Ludwig Maximilians Univ Munchen Dept Earth & Environm Sci Munich Germany|Alfred Wegener Inst Helmholtz Ctr Polar & Marine Bremerhaven Germany|Tech Univ Denmark Dept Civil Engn Lyngby Denmark;
Geol Survey Denmark & Greenland Copenhagen Denmark|Danish Meteorol Inst Copenhagen Denmark;
Univ Liege Dept Geog Liege Belgium;
Univ Utrecht Inst Marine & Atmospher Res Utrecht Netherlands;
Univ Colorado Dept Civil Engn Boulder CO 80309 USA;
Univ Colorado Natl Snow & Ice Data Ctr Boulder CO USA;
机译:过去格陵兰冰盖在东北格陵兰大陆架上扩张和流动的海洋地球物理证据
机译:快速消融区扩张扩大了格陵兰北部的质量损失
机译:冰岛和东格陵兰岛迅速下游(〜16-12 Cal Ka BP)在丹麦海峡两岸海冰,冰漂流和海洋气候
机译:使用无血清培养基和可透过气体的快速扩增细胞培养装置(G-Rex)优化人类T细胞扩增
机译:在气候变暖的情况下格陵兰岛低渗透冰板的快速膨胀
机译:格陵兰岛冰上记录的铅污染表明欧洲的排放源于上古时期的瘟疫战争和帝国扩张
机译:使用卫星L频带微波辐射测定法在格陵兰冰盖中映射多年生FIRN含水层,冰板和栖息的FIRN含水层的经验算法