globalchange

Search Results

Help

Item hits: (Results 1-8 of 8)

Items/Page:    Sort:
Quantitative estimates of Holocene glacier meltwater variations on the Western Tibetan Plateau [期刊论文]
Earth and Planetary Science Letters, 2021-01-01, 559
Li C.-G.;  Wang M.;  Liu W.;  Lee S.-Y.;  Chen F.;  Hou J.
View/Download:33/0
 
The 2020 Larsen C Ice Shelf surface melt is a 40-year record high [期刊论文]
Cryosphere, 2020-01-01, 14 (10
Bevan S.;  Luckman A.;  Hendon H.;  Wang G.
View/Download:2/0
 
Interannual variability of summer surface mass balance and surface melting in the Amundsen sector, West Antarctica [期刊论文]
Cryosphere, 2020-01-01, 14 (1
Donat-Magnin M.;  Jourdain N.C.;  Gallée H.;  Amory C.;  Kittel C.;  Fettweis X.;  Wille J.D.;  Favier V.;  Drira A.;  Agosta C.
View/Download:11/0
 
The influence of föhn winds on annual and seasonal surface melt on the Larsen C Ice Shelf, Antarctica [期刊论文]
Cryosphere, 2020-01-01, 14 (11
Turton J.V.;  Kirchgaessner A.;  Ross A.N.;  King J.C.;  Munneke P.K.
View/Download:2/0
 
Reconciling High Glacier Surface Melting in Summer with Air Temperature in the Semi-Arid Zone of Western Himalaya [期刊论文]
WATER, 2019-01-01, 11 (8
Pratap, Bhanu;  Sharma, Parmanand;  Patel, Lavkush;  Singh, Ajit T.;  Gaddam, Vinay Kumar;  Oulkar, Sunil;  Thamban, Meloth
View/Download:12/0
 
Effects of multilayer snow scheme on the simulation of snow: Offline Noah and coupled with NCEP CFSv2 [期刊论文]
Journal of Advances in Modeling Earth Systems, 2017-01-01, 9 (1
Saha S;  K;  , Sujith K;  , Pokhrel S;  , Chaudhari H;  S;  , Hazra A
View/Download:38/0
 
Glacier-surge mechanisms promoted by a hydro-thermodynamic feedback to summer melt [期刊论文]
Cryosphere, 2015-01-01, 9 (1
Dunse T;  , Schellenberger T;  , Hagen J;  O;  , Kääb A;  , Schuler T;  V;  , Reijmer C;  H
View/Download:39/0
 
Sea ice mass balance observations from the North Pole Environmental Observatory [期刊论文]
Geophysical Research Letters, 2014-01-01, 41 (6
Perovich D.;  Richter-Menge J.;  Polashenski C.;  Elder B.;  Arbetter T.;  Brennick O.
View/Download:30/0
 

1