Then, in the beginning days of February, the Arctic sea ice extent and area both broke records again, as
the entire global sea ice area entered the second - lowest range ever to have been recorded.
Not exact matches
But when you compare it to the 7.3 metres (24 feet) that
global sea levels are predicted to rise if the
entire Greenland
Ice Sheet were to melt away all at once... well, it puts things into perspective.
Greenland is more than twice as large as Texas and if the
entire ice sheet melted, scientists estimate
global sea levels would rise roughly 24 feet.
What they found was that local destabilization of the Amundsen
Sea region of West Antarctica ultimately causes the entire ice sheet to fall into the ocean over several centuries to several thousands of years, gradually adding 3 meters to global sea levels, they report online today in the Proceedings of the National Academy of Scienc
Sea region of West Antarctica ultimately causes the
entire ice sheet to fall into the ocean over several centuries to several thousands of years, gradually adding 3 meters to
global sea levels, they report online today in the Proceedings of the National Academy of Scienc
sea levels, they report online today in the Proceedings of the National Academy of Sciences.
A relatively small amount of melting over a few decades, the authors say, will inexorably lead to the destabilization of the
entire ice sheet and the rise of
global sea levels by as much as 3 meters.
If
global warming leads to an increase in monster storms, MacAyeal adds, then the
entire Antarctic
ice skirt could be in jeopardy: Larger
sea swells could pulverize its huge icebergs and floating
ice shelves.
The Greenland
ice sheet (GIS) has been melting so slowly and so negligibly in recent decades that the
entire ice sheet's total contribution to
global sea level rise was a mere 0.39 of a centimeter (0.17 to 0.61 cm) between 1993 and 2010 (Leeson et al, 2017).
Pine Island Glacier could collapse — stagnate and retreat far up into the bay, resulting in rapid
sea level rise — within the next few centuries, raising
global sea levels by 1.5 m11, 12, out of a total of 3.3 m from the
entire West Antarctic
Ice Sheet13.
Thus the
entire 3 — 4 meters of
global sea level contained in that
ice sheet may be vulnerable to rapid disintegration, although arguments for stability of even this marine
ice sheet have been made [94].
Having said that, it is a really small effect — if the
entire Arctic summer
sea ice pack melted (average thickness 2 metres, density ~ 920 kg / m3, area 3 × 10 ^ 6 km ^ 2 (0.8 % total ocean area) = > a 4.5 cm rise instantly which implies a
global sea level rise of 0.36 mm.
If the
entire West Antarctic
Ice Sheet were to disintegrate, estimates suggest it could raise
global sea levels by 3.3 to 6 meters.
Were Greenland's
entire ice sheet to melt,
global sea level could rise by a startling 7 meters (23 feet), inundating most of the world's coastal cities.
The Greenland
ice sheet (GIS) has been melting so slowly and so negligibly in recent decades that the
entire ice sheet's total contribution to
global sea level rise was a mere 0.39 of a centimeter (0.17 to 0.61 cm) between 1993 and 2010 (Leeson et al, 2017).
That little word of caution will of course be totally ignored by the media who will jump on the «catastrophic acceleration» of
global sea levels «on the heels» the imminent «collapse» the
entire Antarctic
ice shelf, due in 200 years.
«
Global Sea ice trend by year only (barely) crosses 95 % significance when the first two months of satellite data is included for the
entire record.»
To expand the coverage of
global gridded reanalyses, the 20th Century Reanalysis Project is an effort led by PSD and the CIRES at the University of Colorado to produce a reanalysis dataset spanning the
entire twentieth century, assimilating only surface observations of synoptic pressure, monthly
sea surface temperature and
sea ice distribution.
Arctic
sea ice loss can be an example of a tipping point, but it's primarily a tipping point for nothing else than itself (i.e., Arctic
sea ice loss, and associated ecological systems, etc)-- but without much impact on the energy budget of the
entire planet or on
global climate sensitivity.
The
entire Wilkes Basin would change from
ice sheet to
ice shelf, bringing along that 3 - 4 metres of
global sea level rise.
This has already begun to make a measureable difference to
global sea levels, and were the
entire island to shed its burden of
ice — a process that would take a considerable time − then
sea levels would rise by seven metres or more.