Rignot et al have updated results, including those from
the GRACE gravity measurement satellite, to the end of 2010 and show that the downward trend in ice mass is continuing (stronger in Greenland than in Antarctica).
Not exact matches
But
measurements from the
Gravity Recovery and Climate Experiment (
GRACE) satellites, which weigh ice by measuring its gravitational tug from space, suggest that West Antarctica as a whole is losing ice — together with the Antarctic Peninsula, about 150 cubic kilometers per year as of 2005.
Additional precision in this study was provided by NASA's
Gravity Recovery and Climate Experiment, or GRACE satellites, which can make detailed measurements of gravity and, as one result, estimate the mass of glaciers they are flyin
Gravity Recovery and Climate Experiment, or
GRACE satellites, which can make detailed
measurements of
gravity and, as one result, estimate the mass of glaciers they are flyin
gravity and, as one result, estimate the mass of glaciers they are flying over.
Using satellite
measurements from the NASA / German Aerospace Center
Gravity Recovery and Climate Experiment (
GRACE), the researchers measured ice loss in all of Earth's land ice between 2003 and 2010, with particular emphasis on glaciers and ice caps outside of Greenland and Antarctica.
The issues relating to sea level rise and the global water budget can only be addressed when the record of satellite
gravity measurement from
GRACE achieves adequate duration.
... Quantification of these sources is possible using precise satellite altimetry and
gravity measurements as initiated by the IceSat (36) and
GRACE satellites (37), which warrant follow - on missions.
Collecting data from NASA's satellite
Gravity and Recovery Climate Experiment, known as
GRACE, and GPS
measurements of the bedrock on the edges of the ice sheet, the Denmark Technical Institute's National Space Institute in Copenhagen was able to show that crustal uplift due to ice loss has gone up by 1.5 inches between October 2005 and August 2009 along the northwest coast, a change that study co-author John Wahr calls «very dramatic».
Gravity anomaly map from NASA's
GRACE (
Gravity Recovery And Climate Experiment)
measurements.
Based on
GRACE satellite
gravity estimates (illustrated in the graph below on the left) and hydrographic
measurements (graph on right), Greenland's lost ice has correlated best with the pulses of warm Atlantic water that entered into the Irminger Current that flows to the west around Greenland, delivering relatively warm water to the base of Greenland's marine terminating glaciers.
Using satellite
measurements from the NASA / German Aerospace Center
Gravity Recovery and Climate Experiment (
GRACE), the researchers measured ice loss in all of Earth's land ice between 2003 and 2010, with particular emphasis on glaciers and ice caps outside of Greenland and Antarctica.
The
Gravity Recovery and Climate Experiment (GRACE) satellite, a joint project between NASA and the German Aerospace Centre, provided measurements of gravity anomalies, which the team related to groundwater
Gravity Recovery and Climate Experiment (
GRACE) satellite, a joint project between NASA and the German Aerospace Centre, provided
measurements of
gravity anomalies, which the team related to groundwater
gravity anomalies, which the team related to groundwater height.
The maps above combine data from the twin satellites of the
Gravity Recovery and Climate Experiment (
GRACE) with other satellite and ground - based
measurements to model the relative amount of water stored near the surface and underground as of September 17, 2012.
The
Gravity Recovery and Climate Experiment (
GRACE) mission provides estimates of the cryospheric contributions to the acceleration of sea - level rise, including Greenland, Antarctica, and small ice caps and mountain glaciers (22), although these
measurements only start in 2002.
Since 2003, the detailed
gravity measurements from Gravity Recovery and Climate Experiment (GRACE) of the change in glacial land ice and water show an increase in mass of the
gravity measurements from
Gravity Recovery and Climate Experiment (GRACE) of the change in glacial land ice and water show an increase in mass of the
Gravity Recovery and Climate Experiment (
GRACE) of the change in glacial land ice and water show an increase in mass of the ocean.
A decision framework is developed for quantifying the economic value of information (VOI) from the
Gravity Recovery and Climate Experiment (
GRACE) satellite mission for drought monitoring, with a focus on the potential contributions of groundwater storage and soil moisture
measurements from the
GRACE data assimilation (
GRACE - DA) system.