The ICESat mission provided multi-year elevation data needed to
determine ice sheet mass balance as well as cloud property information.
Not exact matches
When CryoSat was first conceived more than a decade ago, its main objective was to
determine whether Earth's large
ice sheets were losing
mass at all.
A pair of satellites (GRACE) were launched several years ago to
determine mass balance in the Antarctic and Greenland
ice sheets.
The rebound can be used to weigh the
ice sheet and
determine how much
mass it has lost and is currently losing, said Doug Wiens, PhD, professor of earth and planetary sciences in Arts & Sciences at Washington University in St. Louis.
A pair of satellites (GRACE) were launched several years ago to
determine mass balance in the Antarctic and Greenland
ice sheets.
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 — 2005.
The satellites measure changes in gravity to
determine mass variations of the entire Antarctic
ice sheet.
The software developed will combine individual assessments of
ice sheet mass balance to
determine a reconciled estimate of
ice sheet mass balance, taking into account the spatial and temporal domain of the input data and their uncertainties, and generate summary graphical and tabulated output.
A wealth of historical imagery exists for Greenland, and scientists could use this data to develop even more detailed histories of the
ice sheet, and to determine whether the Greenland Ice Sheet was at equilibrium — not losing or gaining mass — in recent tim
ice sheet, and to determine whether the Greenland Ice Sheet was at equilibrium — not losing or gaining mass — in recent t
sheet, and to
determine whether the Greenland
Ice Sheet was at equilibrium — not losing or gaining mass — in recent tim
Ice Sheet was at equilibrium — not losing or gaining mass — in recent t
Sheet was at equilibrium — not losing or gaining
mass — in recent times.
Not surprisingly, scientists are working hard to
determine if and when the
ice sheet will transition (or if it has already transitioned) from a stable state to a net
mass loss state.