The second reconstruction uses
satellite gravity measurements to calculate the change in mass of land ice and land water.
2) loss of land based ice: both land based observations (Glacier National Park for instance) and
satellite gravity measurements make it clear that land based ice is decreasing.
Cazenave 2009 uses
satellite gravity measurements to create two independent estimates of ocean heat - both find warming.
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.
Not exact matches
«Tomography is the most powerful method to get this information, but in the future it will be combined with very sensitive
gravity measurements from
satellites and maybe electromagnetic sounding, where people do conductivity
measurements of the interior,» she said.
Precise
measurements of the lunar
gravity and rotation enable us to know how our natural
satellite is deformed by tidal forces.
Geophysicists will be able to answer these questions in the future using
gravity field
measurements from ESA's GOCE
gravity satellite.
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.
The glaciologist was combing through
satellite and GPS data to see what small, local effects could be clouding
satellite measurements of larger changes in Earth's
gravity from ice loss.
A more recent study based on
satellite measurements of
gravity over the entire continent suggests that while the ice sheets in the interior of Antarctica are growing thicker, even more ice is being lost from the peripheries.
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).
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.
There were reports that the sheet was not thinning from
satellite altimetry, but then the
gravity measurements showed that there was mass loss.
Therefore I strongly doubt that the «rising» of the land has any appreciable bearing upon our estimates of ice loss in Antarctica, whether they are based upon
gravity measurements via
satellites or laser altimetry.
... 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.
Abstract: Using
measurements of time - variable
gravity from the Gravity Recovery and Climate Experiment satellites, we determined mass variations of the Antarctic ice sheet during 2002 &mdash
gravity from the
Gravity Recovery and Climate Experiment satellites, we determined mass variations of the Antarctic ice sheet during 2002 &mdash
Gravity Recovery and Climate Experiment
satellites, we determined mass variations of the Antarctic ice sheet during 2002 — 2005.
The researchers compared GOSAT short - wave infrared Fourier transform spectrometer data collected between 2009 and 2013 with water level data from
Gravity Recovery and Climate Experiment observations to approximate drought and used
satellite measurements of solar - induced chlorophyll fluorescence as a proxy for vegetation levels.
Figure 1 shows
gravity satellite measurements of Greenland ice mass from April 2002 to February 2009 (Velicogna 2009).
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».
Yet the rate of ice loss from these two polar realms, as identified by
satellite measurements of the change in
gravity of the ice masses, has more than doubled over the last decade.
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.
Both of the Nature Climate Change studies used a combination of direct
measurements of temperature at various depths, a
measurement of the altitude of the top of the ocean (sea level) from highly accurate
satellite instruments, and measures of the mass of the water in the ocean, from the GRAIL
gravity research project.
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.
With that in mind, a team from the University of Edinburgh, UK, and SRON Netherlands Institute for Space Research, has used
gravity measurements from
satellites and temperature data to find out more.
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.
While modern
satellite - based techniques such as laser altimetery and
gravity anomaly
measurements provide important information on very recent changes, to get at the longer term we must rely on less direct methods.
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.