Measurements taken of Antarctic
sheet ice show that the concentration of naturally occurring carbon dioxide in the atmosphere was already 278 ppm in the 1750s before industrialization started in earnest.
Not exact matches
«These people all commissioned demographic studies that
showed they need a year - round
sheet of
ice.»
But gravity - measuring satellites have
shown that the continent's
ice sheets have been losing mass since at least 2002.
But new analyses like this, which
show previously undiscovered deep canyons, suggest that a good chunk of East Antarctica's bed lies below sea level, rendering the
ice sheet less stable than previously thought.
Parts of the massive
ice sheet once considered stable have been
shown to be melting in new research
However, fresh samples like those we collected on the Greenland
Ice Sheet can
show a clear wildfire signature.»
While the exact sources of black carbon are often difficult to pinpoint in remote areas, the researchers used molecular analysis of the black carbon along with analysis of wind patterns to
show that Greenland's
ice sheet had recently seen clear effects of wildfires burning thousands of miles away in the Canadian Arctic.
Even then, many experts disputed this, and satellite measurements have since
shown the two
sheets are already losing enough
ice to raise sea level by 1.3 millimetres a year and climbing.
As an example, Howat pointed to the portion of the mosaic
showing Jakobshavn Glacier, the fastest - flowing glacier in the Greenland
Ice Sheet.
This could have significant implications for Antarctica's
ice shelves and
ice sheets, with previous research
showing that even small increases in ocean temperatures can substantially increase melt rates around the Peninsula.
In effect, this UAV survey across the ablation zone of the
ice sheet perfectly bridges the gap between people on the ground studying what's under their feet in just one part of the
ice sheet, and the satellite data that
shows what's going on across the entire
ice sheet.
Later records
show those conditions shifted in 2013 - 2014 to favor less melting, but the damage was already done — the
ice sheet had become more sensitive.
Thousands of marks on the Antarctic seafloor, caused by icebergs which broke free from glaciers more than ten thousand years ago,
show how part of the Antarctic
Ice Sheet retreated rapidly at the end of the last ice age as it balanced precariously on sloping ground and became unstab
Ice Sheet retreated rapidly at the end of the last
ice age as it balanced precariously on sloping ground and became unstab
ice age as it balanced precariously on sloping ground and became unstable.
Their results
show that East Greenland has been actively scoured by glacial
ice for much of the last 7.5 million years — and indicate that the
ice sheet on this eastern flank of the island has not completely melted for long, if at all, in the past several million years.
Their field - based data also suggest that during major climate cool - downs in the past several million years, the
ice sheet expanded into previously
ice - free areas, «
showing that the
ice sheet in East Greenland responds to and tracks global climate change,» Bierman says.
Satellite studies of Earth's gravitational field
show that North America is still rebounding from the weight of the massive Laurentide
Ice Sheet, which retreated thousands of years ago
Previous work by coauthor Beth Shapiro, professor of ecology and evolutionary biology at UC Santa Cruz, had
shown that the bison populations north and south of the
ice sheets were genetically distinct by the time the corridor opened.
This photo from December 2010
shows a one - meter long section of the West Antarctic
Ice Sheet Divide core, with a dark layer of volcanic ash visible.
Another thing that
ice core
showed, as others have before, is that the great swing in temperature between glacial and interglacial periods was invariably accompanied by great swings in the amount of greenhouse gases in the atmosphere: When the greenhouse goes up, the
ice sheets go down.
«This
shows the need to continue to look at different components of the climate system, including the
ice sheets and oceans, in an integrated sense,» concluded Paul Myers, study co-author and Professor of Oceanography at the University of Alberta.
In the Coast Guard's spring tests, small - scale models navigated an
ice sheet as long as one - and - a-half Olympic - sized swimming pools at the National Research Council's
ice - tank test facility in Newfoundland to measure various designs» resistance, power and maneuverability (
shown below).
A March study
shows that one large swath of the
ice sheet sits on beds as deep as 8,000 feet below sea level and is connected to warming ocean currents.
Measurements of local gravitational anomalies by the GRACE satellites
show that the Greenland
ice sheet, particularly in its southern reaches, is rapidly losing mass.
Other recent findings of Bell's — that refreezing meltwater can warp the bottom of the
ice sheet — combine with the new study to
show «there's a richer range of processes that can happen at the bottom of the
ice sheet than we thought,» Bell said.
GRACE
showed that the melting polar
ice sheets are contributing more to sea level rise than the demise of mountain glaciers.
Sasha Carter, a postdoctoral researcher at the Scripps Institution of Oceanography who studies the Antarctic
ice sheet, said the new research «
shows that subglacial water transport and the refreezing of that meltwater is reshaping the interior of East Antarctica at a scale previously not believed to be possible.»
Radar images
show that water under the base of the
ice sheet refreezes into
ice, creating a new bottom layer that accounts for up to half the total thickness of the
ice sheet in some locations.
«Our model experiments
show that from 15000 to 13000 years ago, the Eurasian
ice sheet lost 750 cubic kilometres of
ice a year.
Earlier studies of lakeshore deposits had
shown that the lake was at its highest every 2000 years, matching advances of
ice sheets.
New research
shows that small fluctuations in the sizes of
ice sheets during the last
ice age were enough to trigger abrupt climate change.
Based on the southern core we thought this was a localized low heat - flux region — but our model
shows that a much larger part of the southern
ice sheet has low heat flux.
«Studies have
shown that both the Greenland and Antarctic
ice sheets contributed significantly to this sea level rise above modern levels,» said Anders Carlson, an Oregon State University glacial geologist and paleoclimatologist, and co-author on the study.
Since then, measurements from other satellites have
shown that the
ice sheets on both Antarctica and Greenland are shrinking.
A snow pit
shows off the season - by - season stratigraphy at the West Antarctic
Ice Sheet Divide.
Some say humans could have crossed through an opening between the
ice sheets, but these new findings
show that passage was likely closed until 13,400 years ago.
A new study by scientists at NASA's Jet Propulsion Laboratory (JPL) in Pasadena, California, and the University of California, Irvine,
shows that while
ice sheets and glaciers continue to melt, changes in weather and climate over the past decade have caused Earth's continents to soak up and store an extra 3.2 trillion tons of water in soils, lakes and underground aquifers, temporarily slowing the rate of sea level rise by about 20 percent.
«The main result supports and extends earlier work,
showing that human forcing contributes to changing winds that contribute to subsurface ocean warming, affecting some grounding zones of the
ice sheet,» Alley said.
But the data Rapley presented
show that glaciers within the much larger west Antarctic
Ice sheet are also starting to disappear.
But the large volumes of data on Arctic sea and land
ice that IceBridge has collected during its nine years of operations there have also enabled scientific discoveries ranging from the first map showing what parts of the bottom of the massive Greenland Ice Sheet are thawed to improvements in snowfall accumulation models for all of Greenla
ice that IceBridge has collected during its nine years of operations there have also enabled scientific discoveries ranging from the first map
showing what parts of the bottom of the massive Greenland
Ice Sheet are thawed to improvements in snowfall accumulation models for all of Greenla
Ice Sheet are thawed to improvements in snowfall accumulation models for all of Greenland.
The detailed mapping and sampling of the partially eroded Kima» Kho tuya in northern British Columbia, Canada
shows that the ancient regional
ice sheet through which the volcano erupted was twice as thick as previously estimated.
«Our work
shows that the data collected is very well - suited for
ice sheet science, and we can combine it with other satellite and airborne data sets to establish a more detailed record of these glaciers.»
The research
shows that volcanic eruptions beneath a glacial
ice sheet would have created substantial amounts of liquid water on Mars's surface around 210 million years ago.
«In this study, we are
showing that
ice sheets, mountain glaciers and
ice caps are neck - and - neck.»
Recent projections
show that for even the lowest emissions scenarios, thermal expansion of ocean waters21 and the melting of small mountain glaciers22 will result in 11 inches of sea level rise by 2100, even without any contribution from the
ice sheets in Greenland and Antarctica.
In the lab, ancient bacteria from
ice samples 420,000 years old, retrieved from more than 2 miles (3 km) inside the
ice sheet, have quickly
shown signs of life.
The fact that
ice sheets will respond to warming is not in doubt (note the 4 - 6 m sea level rise during the last interglacial), but the speed at which that might happen is highly uncertain, though the other story this week
shows it is ongoing.
Ice cores drawn from Antarctica and Greenland have shown that carbon dioxide (CO2) levels in the atmosphere began to rise at roughly the same time as the vast ice sheets began to me
Ice cores drawn from Antarctica and Greenland have
shown that carbon dioxide (CO2) levels in the atmosphere began to rise at roughly the same time as the vast
ice sheets began to me
ice sheets began to melt.
Despite being trumpeted in certain circles as meaning that there's really nothing to worry about regarding the Greenland
ice sheet, the authors made a point of noting (although not in this press release) that an additional source of mass loss needs to be identified in order to reconcile their results with the GRACE data (which do not
show a reduction in mass loss for the same period).
The relevant papers are [Velicogna and Wahr 2006 Measurements of time - variable gravity
show mass loss in Antarctica Science 311, 1754 - 1756 and Rignot and Thomas «Mass balance of polar
ice sheets» Science 297, 1502 - 1506]
Recent research
shows that there is high microbial activity on glacial surfaces (Anesio et al., 2009), some associated with pigmented algae, which absorb significantly more light than local inorganic dust particles on the Greenland
Ice Sheet (GrIS)(Lutz et al., 2014).