Antarctica's great ice sheet is losing ground as it is eroded by
warm ocean water circulating beneath its floating edge, a new study has found.
The main root of this threat is the potential collapse of West Antarctica's marine - based ice sheets — massive expanses of glacial ice that rest not on land but the ocean floor — in particular, those where
warm ocean waters circulate nearby [Intergovernmental Panel on Climate Change (IPCC), 2013].
Not exact matches
The incoming
water, part of the global conveyor belt of currents
circulating throughout the
oceans, is relatively
warm and salty compared with the rest of the Southern
Ocean.
If you decouple that ice from where it's grounded — something that currents of
warming water, already
circulating around the Antarctic coast, could do — then
water could flow beneath the inland ice and lubricate its slide into the
ocean.
A new study led by the University of Texas Institute for Geophysics has found that wind over the
ocean off the coast of East Antarctica causes
warm, deep
waters to upwell,
circulate under Totten Ice Shelf, and melt the fringes of the East Antarctic ice sheet from below.
Along one string of sites, or «stations,» that stretches from Antarctica to the southern Indian
Ocean, researchers have tracked the conditions of AABW — a layer of profoundly cold water less than 0 °C (it stays liquid because of its salt content, or salinity) that moves through the abyssal ocean, mixing with warmer waters as it circulates around the globe in the Southern Ocean and northward into all three of the major ocean ba
Ocean, researchers have tracked the conditions of AABW — a layer of profoundly cold
water less than 0 °C (it stays liquid because of its salt content, or salinity) that moves through the abyssal
ocean, mixing with warmer waters as it circulates around the globe in the Southern Ocean and northward into all three of the major ocean ba
ocean, mixing with
warmer waters as it
circulates around the globe in the Southern
Ocean and northward into all three of the major ocean ba
Ocean and northward into all three of the major
ocean ba
ocean basins.
Arrays monitor
circulating currents in the Atlantic
Ocean, in which
warm shallow
waters move north (red), while cold deep
waters move south (blue).
Because such deep seawater
circulates from the coast of Antarctica, this deep -
water warming implies that the Southern
Ocean drove the last major climate change.
Since deeper
waters will be
warmer, there is a possible link to the global
ocean circulating currents that results in
warmer water in polar regions.
That'd be a hint that
warm water could indeed get in under the icecap once the edges melt off, unblocking the deep channels and allowing
water to
circulate in and out from the southern
ocean — wouldn't it?
One of the consequences could be a disruption of major
ocean currents, particularly those flowing north and south,
circulating warm water from the equator to polar regions and cold
water from the poles back to the equator.
Over the past fifty million years, earth cooled because land moved,
ocean currents changed, more and more
warm water was
circulated in higher Latitudes and Polar
Oceans to melt more and more sea ice to support more and more snowfall to promote more and more ice on land.
This is the first extensive survey of one of these fjords that shows us how these
warm waters circulate and how vigorous the circulation is... changes in the large - scale
ocean circulation of the North Atlantic are propagating to the glaciers very quickly — not in a matter of years, but a matter of months.
Essentially, the study proposes that climate feedbacks could work completely and totally against us, as
warm water becomes trapped on top of a layer of colder Antarctic
waters due to a near total shutdown in the global
ocean conveyor belt, which
circulates ocean heat from the coast of Antarctica to Newfoundland.