And as they fall apart, the flow of
land ice toward the sea accelerates, speeding up sea - level rise.
Not exact matches
What matters for sea - level rise is the addition of
ice from
land into the ocean, however it's the
ice shelves that hold off the flow of grounded
ice toward the ocean.
Whether dealing with historically intact or novel ecosystems — the 47 percent of Earth's
ice - free
land that has been altered by humans — scientists need to look at the paleobiology of the region, that is, what the ecosystem looked like before humans altered it, and seek to rebuild it to some degree
toward that natural balance, Barnosky said.
Over the last decade, satellites have revealed the glacier is the site of the most dramatic
ice loss in its West Antarctica neighborhood, a fringe of coastline just west of the Antarctic Peninsula — the narrow finger of
land that points
toward South America.
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«Although this paper will likely become a classic compilation of our view in 2017, the 79
ice cores analyzed are spatially restricted,» he told Earther, noting that West Antarctic cores are biased
toward the highest ground, and that East Antarctic record is biased because of a cluster of cores in Dronning Maud
Land, a vast chunk of
ice annexed by Norway in 1939.
Other factors would include: — albedo shifts (both from
ice > water, and from increased biological activity, and from edge melt revealing more
land, and from more old dust coming to the surface...); — direct effect of CO2 on
ice (the former weakens the latter); — increasing, and increasingly warm, rain fall on
ice; — «stuck» weather systems bringing more and more warm tropical air ever further
toward the poles; — melting of sea
ice shelf increasing mobility of glaciers; — sea water getting under parts of the
ice sheets where the base is below sea level; — melt water lubricating the
ice sheet base; — changes in ocean currents -LRB-?)
They used 15 years of satellite radar data from the European Earth Remote Sensing - 1 and -2, Canada's Radarsat - 1 and Japan's Advanced
Land Observing satellites to reveal the pattern of
ice sheet motion
toward the sea.
(To get an updated reading of whether trends in Antarctica
toward lower
land ice are continuing).
However, the loss of such a massive
ice berg from Larsen C, the present human - forced warming of the Antarctic
land and ocean environment, and the presently observed thinning of the
ice shelf all point
toward a rising risk of destabilization or disintegration.