Sentences with phrase «relate ice sheet changes»
Not exact matches
Although CryoSat - 2 is designed to measure changes in the ice sheet elevation, these can be translated into horizontal motion at the grounding line using knowledge of the glacier and sea floor geometry and the Archimedes principle of buoyancy — which relates the thickness of floating ice to the height of its surface.
https://www.sciencedaily.com/
«New method relates Greenland ice sheet changes to sea - level rise.»
«They were questions about how ice sheets relate to sea level, changes in the ocean, changes in the atmosphere and also changes in weather and long - term climate patterns,» says Dr Kennicutt.
The latter is almost linearly related to changes in ice sheet volume; the former, however, is influenced by a range of factors, including atmosphere / ocean dynamics and changes in Earth's gravitational field, rotation, and crustal and the mantle deformation associated with the redistribution of mass between land ice and the ocean.
Most geologic sea level changes are related to tectonic processes (rates of ocean spreading, continental subduction etc.) or the waxing and waning of ice sheets (particularly over the last 2.5 million years).
This result would be strongly dependent on the exact dynamic response of the Greenland ice sheet to surface meltwater, which is modeled poorly in todays global models.Yes human influence on the climate is real and we might even now be able to document changes in the behavior of weather phenomena related to disasters (e.g., Emanuel 2005), but we certainly haven't yet seen it in the impact record (i.e., economic losses) of extreme events.
On decadal and longer time scales, global mean sea level change results from two major processes, mostly related to recent climate change, that alter the volume of water in the global ocean: i) thermal expansion (Section 5.5.3), and ii) the exchange of water between oceans and other reservoirs (glaciers and ice caps, ice sheets, other land water reservoirs - including through anthropogenic change in land hydrology, and the atmosphere; Section 5.5.5).
Although CryoSat - 2 is designed to measure changes in the ice sheet elevation, these can be translated into horizontal motion at the grounding line using knowledge of the glacier and sea floor geometry and the Archimedes principle of buoyancy — which relates the thickness of floating ice to the height of its surface.
The ice ages appear to relate to a change in that ice sheet driven by variations in the earth's orbit.
The Quaternary glacial history of the Arctic Ocean is characterized by the repeated build - up and decay of circum - Arctic ice sheets on the continental shelves, the development and disintegration of ice shelves, and related changes in ocean - circulation patterns and sea ice cover50, 51,52,53,54,55.
Sea level rise (due to thermal expansion only — the ice sheet component of the model isn't yet fully implemented) is directly related to temperature, but changes extremely slowly.
Breaking ice sheets, evaporating lakes and other phenomena relating to Earth's changing climate have influenced the patterns of these rugs by Brooklyn artist Fernando Mastrangelo.
RELATED: Home Impacts of Global Warming Government: The View from Washington, DC The Modern Temperature Trend Rapid Climate Change Supplements: Wintry Doom Ice Sheets & Rising Seas
The observed effects of cryosphere reduction include modification of river regimes due to enhanced glacial melt, snowmelt advance and enhanced winter base flow; formation of thermokarst terrain and disappearance of surface lakes in thawing permafrost; decrease in potential travel days of vehicles over frozen roads in the Arctic; enhanced potential for glacier hazards and slope instability due to mechanical weakening driven by ice and permafrost melting; regional ocean freshening; sea - level rise due to glacier and ice sheet shrinkage; biotic colonisation and faunal changes in deglaciated terrain; changes in freshwater and marine ecosystems affected by lake - ice and sea - ice reduction; changes in livelihoods; reduced tourism activities related to skiing, ice climbing and scenic activities in cryospheric areas affected by degradation; and increased ease of ship transportation in the Arctic.
Furthermore, because the regression is being defined over ice age cycles where the biggest changes are related to the (now disappeared) North American and Fenno - Scandanavian ice sheets, the regression might well be much less for situations where only Greenland and West Antarctica are «in play».