Add to ORKGThree-dimensional perspective of Greenland (south of 72 ° N). Bands change color every 500 meters of elevation. The elevations are derived from Seasat radar altimeter data. (Figure conceived and generated by Steve Fiegles, STX Corporation.
Radar altimetry provides valuable measurements to characterize the state and the evolution of the ic...
The prime objective of NASA's Arctic Ice Mapping project is to provide accurate ice sheet elevation ...
During the past few decades the Greenland and Antarctic ice sheets have lost ice at accelerating rat...
Fourteen SEASAT and ten GEOS-3 satellite radar altimeter groundtracks across a 1 deg x 2.5 deg study...
In August of 1991 and June of 1992, conventional leveling was done to measure surface topography alo...
Previous studies investigating the velocity and elevation change records of the Greenland Ice Sheet ...
Surface elevation maps of the southern half of the Greenland subcontinent are produced from radar al...
The Arctic Ice Mapping group (Project AIM) at the NASA Goddard Space Flight Center Wallops Flight Fa...
In this paper, a new high-resolution elevation model of Greenland, including the ice sheet as well a...
On this MSc thesis we use two radar altimetry mission data in order to study the evolution oof the G...
For more than two decades, radar altimetry missions have provided continuous elevation estimates of ...
We present ice thickness and bed topography maps with a high spatial resolution (250-500 m) of a lan...
We present ice thickness and bed topography maps with a high spatial resolution (250–500 m) of a lan...
The surface mass balance of the Greenland ice sheet critically depends on the intensity of ice melt/...
The Greenland ice sheet is sensitive to climate change. Global heating is expected to result in ice ...
Radar altimetry provides valuable measurements to characterize the state and the evolution of the ic...
The prime objective of NASA's Arctic Ice Mapping project is to provide accurate ice sheet elevation ...
During the past few decades the Greenland and Antarctic ice sheets have lost ice at accelerating rat...
Fourteen SEASAT and ten GEOS-3 satellite radar altimeter groundtracks across a 1 deg x 2.5 deg study...
In August of 1991 and June of 1992, conventional leveling was done to measure surface topography alo...
Previous studies investigating the velocity and elevation change records of the Greenland Ice Sheet ...
Surface elevation maps of the southern half of the Greenland subcontinent are produced from radar al...
The Arctic Ice Mapping group (Project AIM) at the NASA Goddard Space Flight Center Wallops Flight Fa...
In this paper, a new high-resolution elevation model of Greenland, including the ice sheet as well a...
On this MSc thesis we use two radar altimetry mission data in order to study the evolution oof the G...
For more than two decades, radar altimetry missions have provided continuous elevation estimates of ...
We present ice thickness and bed topography maps with a high spatial resolution (250-500 m) of a lan...
We present ice thickness and bed topography maps with a high spatial resolution (250–500 m) of a lan...
The surface mass balance of the Greenland ice sheet critically depends on the intensity of ice melt/...
The Greenland ice sheet is sensitive to climate change. Global heating is expected to result in ice ...
Radar altimetry provides valuable measurements to characterize the state and the evolution of the ic...
The prime objective of NASA's Arctic Ice Mapping project is to provide accurate ice sheet elevation ...
During the past few decades the Greenland and Antarctic ice sheets have lost ice at accelerating rat...