The IceBridge flights, which began on August 27 and will continue until September 16, are mostly repeats of lines that the team flew in early May, so that scientists can observe changes in
ice elevation between the spring and late summer.
Not exact matches
Exact numbers are a work in progress The scientists used a combination of surface
elevation data from satellites and planes
between 1978 and 2012 and a GPS network that weighs the
ice sheet like a scale, according to Ohio State.
The main feedbacks
between climate and the
ice sheet arise from changes in
ice elevation, atmospheric and ocean circulation, and sea -
ice distribution.
We present our best estimate of the thickness and volume of the Arctic Ocean
ice cover from 10 Ice, Cloud, and land Elevation Satellite (ICESat) campaigns that span a 5 - year period between 2003 and 20
ice cover from 10
Ice, Cloud, and land Elevation Satellite (ICESat) campaigns that span a 5 - year period between 2003 and 20
Ice, Cloud, and land
Elevation Satellite (ICESat) campaigns that span a 5 - year period
between 2003 and 2008.
«Neogene extension and basin deepening in the West Antarctic rift inferred from comparisons with the East African rift and other analogs WE LeMasurier — Geology, 2008 intl-geology.geoscienceworld.org Abstract The West Antarctic rift system differs from other volcanically active rift systems in two unusual respects: (1) the rift floor lies 1000 — 2000 m lower in
elevation than others, and (2) four interior
ice - filled troughs extend
between 1500 m and 2555 m below sea level.
Between 2003 and 2005, the Greenland
Ice Sheet lost 101 ± 16 gigatons per year, with a gain of 54 gigatons per year above 2,000, meters and a loss of 155 gigatons per year at lower
elevations.
This NASA visualization shows changes in the surface
elevation of the southeast region of the
ice sheet
between 2003 and 2012.
Based on
ice - sheet model simulations consistent with
elevation changes derived from a new Greenland
ice core, the Greenland
ice sheet very likely contributed
between 1.4 m and 4.3 m sea level equivalent, implying with medium confidence a contribution from the Antarctic
ice sheet to the global mean sea level during the last interglacial period.