This acts as what engineers call «negative feedback» and would explain the paradox of more extensive
southern ocean ice in a warming world.
Not exact matches
«Antarctica: Return of the Weddell polynya supports Kiel climate model: After 40 years, a large
ice - free area appears again in the
Southern Ocean in mid-winter.»
Driven by stronger winds resulting from climate change,
ocean waters in the Southern Ocean are mixing more powerfully, so that relatively warm deep water rises to the surface and eats away at the underside of the
ocean waters in the
Southern Ocean are mixing more powerfully, so that relatively warm deep water rises to the surface and eats away at the underside of the
Ocean are mixing more powerfully, so that relatively warm deep water rises to the surface and eats away at the underside of the
ice.
From 500 feet up everything appeared in miniature except the giant
ice shelves — seemingly endless expanses of
ice, as thick as the length of several football fields, that float in the
Southern Ocean, fringing the
ice sheets that virtually cover the Antarctic landmass.
As the climate changes,
Southern Ocean upwelling may increase, which could accelerate ice shelf melting, release more carbon into the atmosphere and limit the ocean's ability to absorb heat and carbon dioxide from the atmosp
Ocean upwelling may increase, which could accelerate
ice shelf melting, release more carbon into the atmosphere and limit the
ocean's ability to absorb heat and carbon dioxide from the atmosp
ocean's ability to absorb heat and carbon dioxide from the atmosphere.
These coastal glaciers hold back inland glaciers, so their collapse would set off a chain reaction ending with the West Antarctic
Ice Sheet pouring into the
Southern Ocean.
It's known that when
ice sheets start to melt, cooling the air in that region, the winds over the
Southern Ocean strengthen, Toggweiler says.
For example, a lack of iron limits the growth of microscopic plants in the
Southern Ocean around Antarctica and elsewhere, a fact that prompted marine biologist John Martin to famously muse: «Give me half a tanker of iron, and I'll give you the next
ice age.»
It's not a new phenomenon; this «thumb» of Antarctica, which juts out into the stormy
Southern Ocean, has lost more than 28,000 square kilometers of floating
ice — almost as large as Massachusetts — over the past half - century.
What happens when the world moves into a warm, interglacial period isn't certain, but in 2009, a paper published in Science by researchers found that upwelling in the
Southern Ocean increased as the last
ice age waned, correlated to a rapid rise in atmospheric carbon dioxide.
Great mountains of
ice are melting in Antarctica, vast plains of frozen water continue to collapse into the
Southern Ocean.
«
Southern Ocean: Reconstructing environmental conditions over the past 30,000 years: Sea -
ice zone has a major influence on the ecosystem.»
Their study, published today in Nature Geoscience, shows that the
Southern Ocean melted 1,463 km2 of Antarctica's underwater
ice between 2010 and 2016 — an area the size of Greater London.
During two different research expeditions, in the mid - to late springs of 2010 and 2012, the AUV — which resembles a 2 - meter - long bunk bed with twin hulls stacked on top of one another — traveled back and forth through several different
Southern Ocean waters in a lawn mower — like pattern at depths of 20 to 30 meters under the
ice to collect a 3D survey of the topography of the sea
ice's underbelly.
During the
ice ages, storage of the greenhouse gas CO2 in the
Southern Ocean contributed significantly to global cooling.
In addition, now that sea
ice blankets the
Southern Ocean off the western Antarctic Peninsula far less than before, more water is evaporating and forming precipitation, largely in the form of snow.
Changes to Antarctic winds have already been linked to
southern Australia's drying climate but now it appears they may also have a profound impact on warming
ocean temperatures under the
ice shelves along the coastline of West and East Antarctic.
Work done in the
southern hemisphere's summer, December through January 2012 - 13, included drilling holes in the
ice to place a variety of instruments and using radar to map the underside of the
ice shelf and the bottom of the
ocean.
As this GEOTRACES sampling device meets the
ocean, it closes in on nearby pancake
ice in the
southern Canada Basin.
A hunger for iron rules the microscopic sea life of the
Southern Ocean surrounding
ice - covered Antarctica.
He says previous predictive models of Greenland's
ice loss did not adequately take into account the faster movement of its
southern glaciers, which is accelerating the amount of
ice entering the
ocean: «Greenland is probably going to contribute more to sea level rise, and faster than predicted by these models.»
It basically puts the
Southern Ocean up front as the most significant control on the evolution of the polar
ice sheet.»
Analysing new data from marine sediment cores taken from the deep South Atlantic, between the
southern tip of South America and the
southern tip of Africa, the researchers discovered that during the last
ice age, deep
ocean currents in the South Atlantic varied essentially in unison with Greenland
ice - core temperatures.
«Antarctic sea
ice may be a source of mercury in
southern ocean fish and birds.»
Melting sea
ice, Schmidt says, may also supply an essential nutrient that is particularly sparse in the
Southern Ocean: iron.
Electron micrograph of an Antarctic sea
ice diatom, Amphiprora, with attached bacterial cells, illustrating the association between diatoms and bacteria in the
Southern Ocean ecosystem
With higher levels of carbon dioxide and higher average temperatures, the
oceans» surface waters warm and sea
ice disappears, and the marine world will see increased stratification, intense nutrient trapping in the deep
Southern Ocean (also known as the Antarctic
Ocean) and nutrition starvation in the other
oceans.
Gentlepeople, well done on nipping any controversy in the bud — as usual; though I'm left wondering if the warming trend isn't related to a subject that i'd like to see Real Climate Address more often; The possible shut - down of The North Atlantic Conveyor — as extreme warming of the
Southern Oceans, along with the plunging of Europe into a new
Ice Age would be the result of this, as I'm sure you all know.
The
Southern Hemisphere's unrelenting winds and frigid air froze
ocean water into 7.6 million square miles (19.7 million square kilometers) of Antarctic sea
ice this winter, according to the National Snow and Ice Data Center (NSID
ice this winter, according to the National Snow and
Ice Data Center (NSID
Ice Data Center (NSIDC).
Unlike the Arctic, there is no long - term submarine record of
ice thickness — but with the warming
Southern Ocean, it seems likely that that has been going on as well.
That's a process playing out throughout the
Southern Ocean, but scientists don't have a good grasp on it or how sudden changes like the loss of a huge hunk of
ice will alter carbon uptake.
Massive icebergs calving off of Antarctic
ice sheets and floating through the
Southern Ocean deposit iron, which fertilizes the seawater and nurtures massive phytoplankton blooms.
• Global messages from Antarctica, Dana Bergstrom • Deciphering past climate and
ice sheet dynamics from sedimentary records, Carlota Escutia (Antarctic Science Lecture) •
Southern Ocean Acidification, Richard Bellerby (Weyprecht Lecture) • Martha T Muse Lecture (Winner for 2014 to be announced)
«The big
ice sheets from the last Ice Age had melted, sea levels had risen to modern levels, and key ocean - atmosphere processes, such as the El Niño / Southern Oscillation, were establish
ice sheets from the last
Ice Age had melted, sea levels had risen to modern levels, and key ocean - atmosphere processes, such as the El Niño / Southern Oscillation, were establish
Ice Age had melted, sea levels had risen to modern levels, and key
ocean - atmosphere processes, such as the El Niño /
Southern Oscillation, were established.
Stephanie M. Downes, Riccardo Farneti, Petteri Uotila, Stephen M. Griffies, Simon J. Marsland, et al. (2015) An assessment of
Southern Ocean water masses and sea
ice during 1988 - 2007 in a suite of interannual CORE - II simulations, 94, 67 - 94,
Ocean Modelling, doi: 10.1016 / j.ocemod.2015.07.022,
Possible mechanisms include (vii) changes in
ocean temperature (and salinity), (viii) suppression of air - sea gas exchange by sea ice, and (ix) increased stratification in the Southern O
ocean temperature (and salinity), (viii) suppression of air - sea gas exchange by sea
ice, and (ix) increased stratification in the
Southern OceanOcean.
Now that this new iceberg is free of the
ice shelf, it will drift north into the
Southern Ocean.
Quick recovery is consistent with the
Southern Ocean - centric picture of the global overturning circulation (Fig. 4; Talley, 2013), as the Southern Ocean meridional overturning circulation (SMOC), driven by AABW formation, responds to change in the vertical stability of the ocean column near Antarctica (Sect. 3.7) and the ocean mixed layer and sea ice have limited thermal ine
Ocean - centric picture of the global overturning circulation (Fig. 4; Talley, 2013), as the
Southern Ocean meridional overturning circulation (SMOC), driven by AABW formation, responds to change in the vertical stability of the ocean column near Antarctica (Sect. 3.7) and the ocean mixed layer and sea ice have limited thermal ine
Ocean meridional overturning circulation (SMOC), driven by AABW formation, responds to change in the vertical stability of the
ocean column near Antarctica (Sect. 3.7) and the ocean mixed layer and sea ice have limited thermal ine
ocean column near Antarctica (Sect. 3.7) and the
ocean mixed layer and sea ice have limited thermal ine
ocean mixed layer and sea
ice have limited thermal inertia.
Impact of
ice melt on storms Freshwater injection onto the North Atlantic and
Southern Oceans causes increase of sea level pressure at middle latitudes and decrease at polar latitudes.
However, if the remaining
ice shelf collapses or starts losing mass more rapidly, it could effectively unplug the glaciers next to the shelf, sending land - based
ice into
Southern Ocean, and contributing to sea level rise.
Hall, A., and M. Visbeck, 2002: Synchronous variability in the
Southern Hemisphere atmosphere, sea
ice and
ocean resulting from the annular mode.
ICESat - 2 will add to our understanding of Arctic sea
ice by measuring sea
ice thickness from space, providing scientists more complete information about the volume of sea
ice in the Arctic and
Southern oceans.
Fossils provide insight into origin of unique Antarctic ecosystem (19/04/2013) Origin of circum - Antarctic
Southern Ocean's ecosystems can be traced back to the emergence of the Antarctic
ice sheets....
When they're not diving 2,000 feet under the
Southern Ocean, Weddell seals spend their time lounging on Antarctica's
ice.
The
ice melting from
ocean heat flux decreases faster than the ice growth does in the weakly stratified Southern Ocean, leading to an increase in the net ice production and hence an increase in ice mass.&r
ocean heat flux decreases faster than the
ice growth does in the weakly stratified
Southern Ocean, leading to an increase in the net ice production and hence an increase in ice mass.&r
Ocean, leading to an increase in the net
ice production and hence an increase in
ice mass.»
The vital role of the
Southern Oceans on CO2 and temperature, as well as subsurface
ocean temperature and
ice sheet destabilization leading to rapid non-linear sea level rise is also discussed.»
I wanted to bring alive everything I loved about my hometown area in
Southern California since I was a kid: the sunsets, the palm trees, the mist on June mornings, the greenbelts, the way the bright - green
ice plant meets the sand, the
ocean - facing restaurants and how it always smells a little like suntan oil and open grills when you're walking down the sidewalk in a beach town.
In his travels, Beltrá has photographed the Brazilian Amazon, the Patagonian
ice fields, the vast tundra of the Arctic, as well as the
Southern Ocean.
Paul D... As a part - time alarmist I would answer that with a little bit of extrapolation added to some warnings of climate scientists I guess the worst case scenario at least includes the total collapse of the WAIS, creating tsunamis at least all over the Pacific rim, the subsequent sea level rise of c. 7m will destroy most of the remaining harbours, communication centers near coasts, next up would be the melting of the collapsed
ice in the
southern ocean altering the climate of the entire
southern hemisphere, making it near - impossible to guess what areas are good for similar agriculture as before, leading to massive movements of people.
More than likely, the isotopic signal (the distribution of 13C - depleted carbon that invaded the atmosphere) indicates that carbon should have been «mined» from the
Southern ocean as a result of the displacement of southern winds, sea ice, and perturbations to the ocean's biological pump (e.g., Anderson et al.
Southern ocean as a result of the displacement of
southern winds, sea ice, and perturbations to the ocean's biological pump (e.g., Anderson et al.
southern winds, sea
ice, and perturbations to the
ocean's biological pump (e.g., Anderson et al., 2009).