Results 201 to 210 of about 95,350 (324)
Abstract Accurately predicting Greenland's ice mass loss is crucial for understanding future sea level rise. Approximately 50% of the mass loss results from iceberg calving at the ice‐ocean interface. Ice mélange, a jammed, buoyant granular material that extends for 10 km or more in Greenland's largest fjords, can inhibit iceberg calving and discharge ...
Kavinda Nissanka+7 more
wiley +1 more source
Satellite radar altimetry over ice. Volume 1: Processing and corrections of Seasat data over Greenland [PDF]
The data-processing methods and ice data products derived from Seasat radar altimeter measurements over the Greenland ice sheet and surrounding sea ice are documented.
Bindschadler, Robert A.+4 more
core +1 more source
Complex motion of Greenland Ice Sheet outlet glaciers with basal temperate ice. [PDF]
Law R+5 more
europepmc +1 more source
Steady-state characteristics of the Greenland ice sheet under different climates [PDF]
Anne Letréguilly+2 more
openalex +1 more source
Abstract The floating ice tongue of the 79N Glacier in Northeast Greenland has been thinning over the past two decades, with warning signs of a potential onset of disintegration. While previous studies primarily attribute the thinning of the ice shelf to oceanic heat flux, limited attention has been given to the significant role of ice shelf plume ...
Mahdi Mohammadi‐Aragh+9 more
wiley +1 more source
Memory of the Greenland Ice Sheet
A series of palaeoclimatic computations is performed in order to study the memory of the Greenland ice sheet, namely the information on the choice of the initial state, which is kept in the interior of the ice-sheet model after many thousands of integration years.
Rogozhina, I.+4 more
openaire +2 more sources
Interactions of Fungi and Algae from the Greenland Ice Sheet. [PDF]
Perini L+9 more
europepmc +1 more source
Ice flow around large obstacles as indicated by basal ice exposed at the margin of the Greenland ice sheet [PDF]
Peter Knight+2 more
openalex +1 more source
Abstract A glacial forebulge is a bending‐related upheaval of the lithosphere outside a glaciated area that co‐occurs to the depression of the lithosphere below an ice sheet. The forebulge of the last glaciation attracted attention over more than one century, but quantitative descriptions on the geometry of the forebulge are rare.
Christian Brandes+4 more
wiley +1 more source
Decreasing surface albedo signifies a growing importance of clouds for Greenland Ice Sheet meltwater production. [PDF]
Ryan JC+6 more
europepmc +1 more source