They are going to study cosmic rays, assess polar microplastics and nano plastics and, on the 90th birthday of its loss, look for the remains of Umberto Nobile's lost dirigible, the Airship Italia, «taking advantage of
the melting ice in the region for the first time in centuries.»
Not exact matches
Study researchers Hélène Seroussi and Erik Ivins of NASA's Jet Propulsion Laboratory built a model of all the known
melting and freezing under the
ice in the
region.
Forming
in the system's colder outer
regions, where volatile compounds such as water and carbon dioxide freeze out, makes it possible that the planets incorporated those
ices and carried them along to a warmer place where they could
melt, evaporate, and become oceans and atmospheres.
Climate modelers do not include effects on land - based
ice in these
regions because they can not reduce them to equations, such as x amount of extra heat equals y amount of
melting.
Higher precipitation levels
in the
region and
melting ice would decouple the surface from the deeper water layers.
Should
ice in Arctic
regions, such as Greenland,
melt again, the globe may face a similar situation, sending Europe into a colder age despite warming taking place elsewhere.
In comparison, it took the Jakobshavn Isbræ
ice stream — a southwest Greenland
region with a fast - moving glacier that has been a focal point of scientific examination of
ice sheet
melt — 150 years to retreat 35 kilometers, said Khan.
Satellite data show that, between 1979 and 2013, the summer
ice - free season expanded by an average of 5 to 10 weeks
in 12 Arctic
regions, with sea
ice forming later
in the fall and
melting earlier
in the spring.
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.
The ascending hydrothermal fluids probably trigger local
melting in the
ice layer of the polar
region.
Scientists had previously considered the
region's ground
ice to be
in equilibrium, meaning its seasonal
melting and refreezing did not, over time, diminish the valley's overall mass of ground
ice.
With Arctic
ice melting at an accelerating rate, nations are looking to travel through a
region that has been barren since James Cook mapped the Bering Strait
in 1778.
A possible cause for the accelerated Arctic warming is the
melting of the
region's sea
ice, which reduces the icy, bright area that can reflect sunlight back out into space, resulting
in more solar radiation being absorbed by the dark Arctic waters.
Because ocean currents play a major role
in transporting the planet's heat and carbon, the ECCO simulations are being used to understand the ocean's influence on global climate and the
melting of
ice in polar
regions.
While the glaciers
in this
region seemed stable, it turns out warming ocean currents have been
melting the underside of the
ice.
«A lot of what we are seeing right now
in the coastal
regions is that warming ocean waters are
melting Antarctica's glaciers and
ice shelves, but this process may just be the beginning,» Shevenell said.
Continued warming
in these
regions will result
in even more
ice melt with the likelihood of catastrophic environmental consequences,» Yao noted.
Some scientists have argued that Earth's crust
in northern portions of North America is still slowly springing upward
in response to the
melting of the
ice sheet that smothered the
region during the last
ice age.
This remarkable correlation is supported by observations by other scientific teams who had already observed traces of glacier
melting and retreat, as well as evidence of subsurface
ice,
in the former polar
regions.
Relevant to this issue, there is currently a debate among paleoclimatologists with respect to the following condundrum: A dramatic recession of the more - than - 11,000 year old
ice cap of Mt. Kilimanjaro
in tropical East Africa is taking place despite any clear evidence that temperatures have exceeded the
melting threshold (one explanation is that the changes are largely associated with a drying atmosphere
in the
region; the most recent evidence, however, seems to indicate that
melting may indeed now be underway).
Climate change is pushing temperatures up most rapidly
in the polar
regions and left the extent of Arctic sea
ice at 1.79 million square miles at the end of the summer
melt season.
Focus of Study The long - term variation of the Earth's gravity field due to post-glacial rebound and present - day
ice melting in the polar
regions.
Collapsing
ice shelves and
melting sea
ice leaves more open water
in the Earth's polar
regions (photo a
in earlier figure).
In the long term, changes in sea level were of minor importance to rainfall patterns in north western Sumatra With the end of the last Ice Age came rising temperatures and melting polar ice sheets, which were accompanied by an increase in rainfall around Indonesia and many other regions of the world
In the long term, changes
in sea level were of minor importance to rainfall patterns in north western Sumatra With the end of the last Ice Age came rising temperatures and melting polar ice sheets, which were accompanied by an increase in rainfall around Indonesia and many other regions of the world
in sea level were of minor importance to rainfall patterns
in north western Sumatra With the end of the last Ice Age came rising temperatures and melting polar ice sheets, which were accompanied by an increase in rainfall around Indonesia and many other regions of the world
in north western Sumatra With the end of the last
Ice Age came rising temperatures and melting polar ice sheets, which were accompanied by an increase in rainfall around Indonesia and many other regions of the worl
Ice Age came rising temperatures and
melting polar
ice sheets, which were accompanied by an increase in rainfall around Indonesia and many other regions of the worl
ice sheets, which were accompanied by an increase
in rainfall around Indonesia and many other regions of the world
in rainfall around Indonesia and many other
regions of the world..
Because they depend on sea
ice to hunt seals, the polar bear is considered threatened as global warming
melts and thins
ice in this
region.
For dogs who live
in regions with
ice and snow
in the winter, road salt and sidewalk
ice -
melt products can irritate the footpads.
When the Arctic sea
ice goes the increase
in water vapour
in the Arctic
region will accelerate the Greenland
melt.
Some really interesting recent weather events
in the High Arctic have shown me the reality of a warmer polar
region, snow flakes do not
melt in an ocean -1.5 C cold, and
ice does not form when its -6 C outside.
This does not mean that the current
ice melt pattern is an example of anything less then excessive heat content
in the
region.
It is possible the Arctic
ice melt could also be related to ocean currents carrying highly saline water caused by the recent increased SSTs
in the temperate oceans between 1985 and 2005 to the
region.
Most glaciologists have assumed that temperature trends
in that
region are not big enough to matter
in the way that they have mattered on the Antarctic Peninsula, where surface
melting has led to
ice shelf collapse.
This would seem to suggest that if the volume of
ice melt is as great as suspected, that there had to be a greater salinity
in the
region that was mixing with the
melt water to reduce the expanse and depth of the brackish
region.
In many regions, changing precipitation or melting snow and ice are altering hydrological systems, affecting water resources in terms of quantity and quality (medium confidence
In many
regions, changing precipitation or
melting snow and
ice are altering hydrological systems, affecting water resources
in terms of quantity and quality (medium confidence
in terms of quantity and quality (medium confidence).
Relevant to this issue, there is currently a debate among paleoclimatologists with respect to the following condundrum: A dramatic recession of the more - than - 11,000 year old
ice cap of Mt. Kilimanjaro
in tropical East Africa is taking place despite any clear evidence that temperatures have exceeded the
melting threshold (one explanation is that the changes are largely associated with a drying atmosphere
in the
region; the most recent evidence, however, seems to indicate that
melting may indeed now be underway).
Between the spring of 2004 (above) and last spring (below), an expanding
region of
melting snow and
ice in Greenland has unburied a research camp.
This thicker multiyear
ice takes longer to
melt back (both because of greater thickness and higher albedo than first - year
ice) and so
in conjunction with the weather it is responsible for more extensive
ice in the late summer
in this
region.
Alarmed at the pace of change to our Earth caused by human - induced climate change, including accelerating
melting and loss of
ice from Greenland, the Himalayas and Antarctica, acidification of the world's oceans due to rising CO2 concentrations, increasingly intense tropical cyclones, more damaging and intense drought and floods, including glacial lakes outburst loods,
in many
regions and higher levels of sea - level rise than estimated just a few years ago, risks changing the face of the planet and threatening coastal cities, low lying areas, mountainous
regions and vulnerable countries the world over,
So, the positive feedback between
melt and velocities implies that more
melt leads to higher velocities, which bring
in more
ice from cold
regions to warm
regions which increases the
melt and hence the velocity etc, with as a final result a rapid loss of
ice and hence an enhanced increased sea level.
Generally,
in this
region you may have several
melt re-freeze cycles, with a blanket of new fallen snow with a reflectivity
in the UV range of near 90 % versus something
in the area of 50 % of
ice within the first foot.
Of course, temperatures
in the Churchill
region have risen, and the
ice extent
in Hudson Bay is
melting earlier and forming later (by about a month
in each case) than 30 years ago.
The fate of sea
ice in the Arctic Ocean is determined by a complicated mix of factors, including the pressure changes, with the biggest loss of old thick
ice resulting more from a great «flush» of floes than
melting, Dr. Rigor and many other scientists tracking the
region say.
Howell points out that concentration of MYI
in the
region is well below the historical average and that it is likely the seasonal first - year
ice will clear during the
melt season.
Ice melting in mountainous
regions not only affects river flows, it also affects sea level rise.
Scientists at the National Snow and
Ice Data Center, in Boulder, Colorado measured the sea ice at the end of the 2012 summer period of melting and the measurements do not bode well for the extraordinary wildlife, ecology and cultures of the regi
Ice Data Center,
in Boulder, Colorado measured the sea
ice at the end of the 2012 summer period of melting and the measurements do not bode well for the extraordinary wildlife, ecology and cultures of the regi
ice at the end of the 2012 summer period of
melting and the measurements do not bode well for the extraordinary wildlife, ecology and cultures of the
region.
When
ice melts it reveals darker Arctic Ocean water, which
in turn absorbs more heat from the sun, further heating the
region.
IUCN and academic partners are conducting research
in the Arctic and Baltic
regions to establish to what extent plastic particles accelerate
ice melt in the Arctic Circle.
For example, conditions at the poles affect how much heat is retained by the earth because of the reflective properties of
ice and snow, the world's ocean circulation depends on sinking
in polar
regions, and
melting of the Antarctic and Greenland
ice sheets could have drastic effects on sea level.
By
melting sea
ice, warming
in the Arctic
regions allows more sunlight to be absorbed by the ocean which leads to yet more warming.
«Our investigations show that uplift of the sea floor
in this
region, caused by the
melting of the
ice masses since the end of the last
ice age, is probably the reason for the dissolution of methane hydrate.»
And science is emerging suggesting a link between the
melting of Arctic sea
ice on one hand and faster warming
in the
region and changes to the northern hemisphere jet stream on the other, explaining why some weather systems appear to get «stuck
in place» — to often - devastating effect.