supported by National Basic Research Program of China(2016YFA0602701);National Natural Science Foundation of China(41941006,41530748);National Key Research and Development Program of China(2018YFC1406104).
It is remarkable that the high-end sea level rise threat over the next few hundred years comes almost entirely from only a handful of ice streams and large glaciers.These occupy a few percent of ice sheets’coastline....
supported by the National Key R&D Program of China (Grant No. 2018YFC1406101);the Fundamental Research Funds for the Central Universities
The Jakobshavn Glacier(JG)in Greenland is one of the most active glaciers in the world.It was close to balance before 1997 but this was followed by a sudden transition to rapid thinning.The reason for the change remai...
supported by the Trond Mohn Donation to the Mohn-Sverdrup Center at the Nansen Center,the Research Council of Norway’s UK/Netherlands/Norway RAPID program;the project AWAKE under the Polish-Norwegian Research Fund(2009–2011)
Petermann Glacier is a marine-terminating outlet glacier that had a 70 km-long floating ice tongue prior to a ~ 270 km2 calving event that was observed from satellite sensors in August 2010,shortening the ice tongue ...
This study was jointly supported by the National Natural Science Foundation of China (Grant No. 49871022); the Chinese Academy of Sciences (Grant No. KZ951-A1-402-03)llTianshan Gla-ciological Station and the Chinese Postdoctoral Research Foundation.
Formate (HCOO-), acetate (CH3COO-), oxalate (C2O42-) and pyruvate ((CO)C2O42-) are detected in a 14.08-m-long ice core recovered in Glacier 1 at the Urumqi riverhead, Tianshan, China, which is a mid-latitude alpine gl...