GLACIERS AND ICE SHEETS
IN A CHANGING CLIMATE

 

Spaceborne synthetic-aperture radar interferometry (InSAR) is a powerful remote sensing tool for measuring glacial motion with
millimeter-scale precision, over extensive areas, at an unprecedented level of spatial details. This technique has been used to map
the detailed topography and vector velocity of the Greenland and Antarctic Ice Sheets,  the tidally-induced vertical motion of
large areas of floating ice, and study rift propagation precursor to large calving events on Antarctic ice shelves. The results are an
important source of information for determining the current state of mass balance of outlet glaciers and ice sheets,  for estimating
their contribution to sea level rise, for capturing dynamic changes such as grounding-line retreat and flow acceleration, for predicting
future calving events, and eventually better constraint predictions of the evolution of those ice masses in a changing climate.
 



 


What is InSAR ?

Synthetic Aperture Radars (SAR) produce all weather, day and night, high resolution images of the Earth's surface providing useful information about the physical characteristics of the ground and of the vegetation canopy, such as surface roughness, soil moisture, tree height and bio-mass estimates (Imaging Radar Page at JPL). By combining two or more SAR images of the same area, it is also possible to generate elevation maps and surface change maps with unprecedented precision and resolution. This technique is called InSAR. With the advent of spaceborne radars, InSAR has been applied to the study of a number of natural processes including earthquakes, volcanoes, glacier flow, landslides, and ground subsidence.


Glaciology Research in Antarctica, Patagonia and Greenland.


Field Work (in preparation) ...


References


Data (in preparation) ...


Useful Links


For more information

Eric Rignot : eric@adelie.jpl.nasa.gov