The Guardian reported that
the sea ice melt impacts Inuits» infrastructure and wildlife, including polar bears:
Sea ice melt impacts local and global temperatures in a feedback loop.
Not exact matches
A new University of Washington study, with funding and satellite data from NASA and other agencies, finds a trend toward earlier
sea ice melt in the spring and later
ice growth in the fall across all 19 polar bear populations, which can negatively
impact the feeding and breeding capabilities of the bears.
So, what tourism is
impacting and actually what climate change is
impacting is a relatively very small piece of that peninsula; but you know the
impact on the peninsula if all that
ice melts could be huge; when they talk about
sea levels rising, you know, by inches and feet, you know if that
ice along the peninsula
melts they will add to the volume of the
sea very quickly.
Pettersen is hopeful that, with more data analysis over longer periods of time, researchers will find more answers yet to account for the
melting ice sheet and the subsequent
sea level rise that has already had an
impact on regions across the planet.
Cantwell said that the science underway at DOE will be critical to understanding the
impacts of the rising greenhouse - gas levels in the atmosphere — from Arctic
sea -
ice melt to ocean acidification — and maintaining US leadership in clean - energy technologies.
The
impacts of climate change include global warming, rising
sea levels,
melting glaciers and
sea ice as well as more severe weather events.
The
melting of the polar
ice cap would have a drastic effect:
Sea level would rise by several meters around the world,
impacting hundreds of millions of people who live close to coasts.
At a global scale, the increased
melting of the
ice sheet contributes to rising
sea level and may
impact global ocean circulation patterns through the so - called «thermohaline circulation'that sustains among others, the Gulf Stream, which keeps Europe warm.
It is likely that several other factors, combined with the
impact of
melting Arctic
sea ice, explain the recent run of wet summers.
«Warming greater than 2 degrees Celsius above 19th - century levels is projected to be disruptive, reducing global agricultural productivity, causing widespread loss of biodiversity and — if sustained over centuries —
melting much of the Greenland
ice sheet with ensuing rise in
sea levels of several meters,» the AGU declares in its first statement in four years on «Human
Impacts on Climate.»
Starting next week, NASA's Operation IceBridge, an airborne survey of polar
ice, will be carrying science flights over
sea ice in the Arctic, to help validate satellite readings and provide insight into the
impact of the summer
melt season on land and
sea ice.
This year's record low
sea ice maximum extent might not necessarily lead to a new record low summertime minimum extent, since weather has a great
impact on the
melt season's outcome, Meier said.
Paradoxically, both phenomena are likely linked: When
sea -
ice North of Scandinavia and Russia
melts, the uncovered ocean releases more warmth into the atmosphere and this can
impact the atmosphere up to about 30 kilometers height in the stratosphere disturbing the polar vortex.
In a study out of the University of Arizona, researchers found that
melting ice sheets had a greater
impact on
sea level rise than the thermal expansion of the oceans during the previous interglacial period 125,000 years ago.
For example,
ice loss in far - off West Antarctica will have more profound
impacts in Scandinavia than it will in nearby Australia, while right now
melting Alaskan glaciers contribute more to
sea - level rise in the Baltic than the Greenland
ice sheet.
Freshwater injection already has a large
impact when
ice melt is a fraction of 1 m of
sea level.
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.
Writing in Nature Climate Change, two scientists from the Potsdam Institute for Climate
Impact Research (PIK) say the
melting of quite a small volume of
ice on the East Antarctic shore could ultimately trigger a discharge of
ice into the ocean which would result in unstoppable
sea - level rise for thousands of years ahead.
The project aims to improve understanding of snow
melt on
ice shelves, floating extensions of the massive inland
ice sheet which stabilize
ice loss, and how
melt will
impact on
ice shelf stability and
sea level.
Items covered How the climate is changing with time laps charts showing the changes in
Sea ice melting Ice sheet melting Carbon dioxide in the atmosphere Global temperature change Students will also explore a future technology on how to reduce the human impact on the environme
ice melting Ice sheet melting Carbon dioxide in the atmosphere Global temperature change Students will also explore a future technology on how to reduce the human impact on the environme
Ice sheet
melting Carbon dioxide in the atmosphere Global temperature change Students will also explore a future technology on how to reduce the human
impact on the environment.
One of the biggest potential
impacts on human affairs from sustained warming is coastal inundation as warming
seas swell and fill with water flowing from
melting ice sheets.
Given that
impacts don't scale linearly — that's true both because of the statistics of normal distributions, which imply that (damaging) extremes become much more frequent with small shifts in the mean, and because significant breakpoints such as
melting points for
sea ice, wet - bulb temperatures too high for human survival, and heat tolerance for the most significant human food crops are all «in play» — the model forecasts using reasonable emissions inputs ought to be more than enough for anyone using sensible risk analysis to know that we making very bad choices right now.
[Aug. 9, 8:04 p.m. Updated Joe Romm has predictably assailed my view of Arctic
sea ice trends and their implications, straying into discussions of
melting permafrost (which is an entirely different issue laden with its own questions — one being why the last big retreat of permafrost, in the Holocene's warmest stretch, didn't have a greenhouse - gas
impact) and my refusal to proclaim a magically safe level of carbon dioxide (which I discuss here).
The Arctic
sea ice melting out above 75N would have almost no
impact at all if that is the forcing change of glaciers down to Chicago and
sea ice down to 45N (at lower latitudes where the Albedo has much more
impact).
Does anyone have any interest in climatalogical
impact of
sea ice melt or is it all about breaking records?
Surface winds can
impact the
sea ice both through accelerated freezing or
melting (via heat transfer from the atmosphere to and from the surface) and by blowing the
ice from one place to another.
The stunning documentary «Chasing
Ice» conveys the drama and mystery in all that
melting, and the
impact of warmer
sea water on the areas where Greenland's glaciers meet the
sea.
In the past (pre-1990s) this low would have just spread the
ice pack out and increased
sea ice extent, but with how thin the
ice is, this just allows heat to
melt the scattered
ice from all sides and have a bigger
impact on
sea ice extent.
Joe Romm has predictably assailed my rejection of his «death spiral» depiction of Arctic
sea ice trends, straying into discussions of
melting permafrost (which is an entirely different issue laden with its own questions — one being why the last big retreat of permafrost, in the Holocene's warmest stretch, didn't have a greenhouse - gas
impact) and my refusal to proclaim a magically safe level of carbon dioxide (which I discuss here).
Hotter temperatures have led to rising
sea levels,
melting glaciers, vanishing Arctic
sea ice, wildlife migrations, and more extreme weather among other
impacts.
In addition to direct MYI
melt due to high - latitude warming, the
impact of enhanced upper - ocean solar heating through numerous leads in decaying Arctic
ice cover and consequent
ice bottom
melting has resulted in an accelerated rate of
sea -
ice retreat via a positive
ice - albedo feedback mechanism.
As far as an
impact to humanity - the
ice melting is a good thing — unless it result in a secondary harm such as a
sea level rise.
Some mechanisms for that are hypothesized, e.g. methane release from polar regions, increased
melting of Greenland leading to stopping the Gulf Stream, rapid reduction of Arctic
sea -
ice and its positive feedback, collapse of Antarctic
ice shelves, loss of the Amazon, large volcanoes, asteroid
impacts, unexpected solar variation.
Some of which include more variable weather, increasing
sea ice melt, rising
sea levels and ocean waters with more CO2, also called ocean acidification, which can harm ecosystems and has an
impact on coral reefs.
Requires the Director of the National Science Foundation and the Administrator of the National Oceanic and Atmospheric Administration (NOAA) to enter into an arrangements with NAS to study: (1) the current status of
ice sheet
melt, as caused by climate change, with implications for global
sea level rise; and (2) the current state of the science on the potential
impacts of climate change on patterns of hurricane and typhoon development and the implications for hurricane - prone and typhoon - prone coastal regions.
Warming over 2 degrees celsius would have dramatic consequences: the planet's
ice sheets would be far more likely to
melt, triggering more
sea level rise, than at 1.5 degrees, which is considered the safer limit, according to Hans Joachim Schellnhuber, a physicist who heads the Potsdam Institute for Climate
Impact Research in Germany.
Freshwater and
ice flows into polar oceans have a direct
impact on
sea level and (in conjunction with the
melt of
sea ice) are important in maintaining the thermohaline circulation.
Melting of sea ice has no impact on sea level — water or ice that is already floating does not change the sea level by melting / fr
Melting of
sea ice has no
impact on
sea level — water or
ice that is already floating does not change the
sea level by
melting / fr
melting / freezing.
Of critical importance at this conference will be a discussion around the role that the Antarctic
ice sheet plays in regulating the Earth's climate and the potential
impact of
melting ice on rising
sea levels.
Perhaps some gross thermomechanical process of restructuring the climate mechanisms (some small fraction of these were identified in the Stadium Wave paper, for instance) is ongoing, and the energy of restructuring —
melting, subliming and carrying away Arctic
sea ice and Greenland and Antarctic land
ice net to the atmosphere, higher humidity absorbing gross water amounts to a level
impacting sea level rise on the millimeter or sub-millimeter level, expansion of land due heat, or more likely erosion, silting and subsidence, and so on — is responsible for a Black Swan.
Furthermore, the sustained
melting of Greenland
ice and other
ice stores under climate warming, coupled with the
impacts of a possible abrupt shut - down of the Atlantic meridional overturning circulation (MOC) after 2100, provide additional uncertainty to
sea - level rise for Europe (Gregory et al., 2004; Levermann et al., 2005; Wigley, 2005; Meehl et al., 2007).
With the
impact of
melting Antarctic
ice potentially devastating in the world's fight against rising
sea levels, this conference could be vital in solving one of our greatest challenges.
The stronger fresh water hurricanes is neat, but the Arctic storm with fresh
sea ice melt would have a huge
impact on Northern Hemisphere heat loss.
«The CCR - II report correctly explains that most of the reports on global warming and its
impacts on
sea - level rise,
ice melts, glacial retreats,
impact on crop production, extreme weather events, rainfall changes, etc. have not properly considered factors such as physical
impacts of human activities, natural variability in climate, lopsided models used in the prediction of production estimates, etc..
Since 2013, Mr. Sinclair has been Media Director of The Dark Snow Project, an ongoing science communication effort that focuses on clarifying and communicating the emerging story of
melting ice in Greenland and its
impact on global weather and
sea level rise.
For instance, the large
sea - level rise (up to 12 m) that would result from the
melting of the Greenland and Antarctic
ice sheets would have major
impacts on coastal areas, with effects both on biological systems and human populations.
For more on the terrestrial foods topic, see my detailed discussion in this previous post, and this recent (March 30) ScienceNews report on yet another, largely anecdotal «polar bears resort to bird eggs because of declining
sea ice» story (see photo below, based on a new paper by Prop and colleagues), which was also covered March 31 at the DailyMail («Polar bears are forced to raid seabird nests as Arctic sea ice melts — eating more than 200 eggs in two hours,» with lots of hand - wringing and sea ice hype but little mention of the fact that there are many more bears now than there were in the early 1970s around Svalbard or that the variable, cyclical, AMO (not global warming) has had the largest impact on sea ice conditions in the Barents Se
sea ice» story (see photo below, based on a new paper by Prop and colleagues), which was also covered March 31 at the DailyMail («Polar bears are forced to raid seabird nests as Arctic
sea ice melts — eating more than 200 eggs in two hours,» with lots of hand - wringing and sea ice hype but little mention of the fact that there are many more bears now than there were in the early 1970s around Svalbard or that the variable, cyclical, AMO (not global warming) has had the largest impact on sea ice conditions in the Barents Se
sea ice melts — eating more than 200 eggs in two hours,» with lots of hand - wringing and
sea ice hype but little mention of the fact that there are many more bears now than there were in the early 1970s around Svalbard or that the variable, cyclical, AMO (not global warming) has had the largest impact on sea ice conditions in the Barents Se
sea ice hype but little mention of the fact that there are many more bears now than there were in the early 1970s around Svalbard or that the variable, cyclical, AMO (not global warming) has had the largest
impact on
sea ice conditions in the Barents Se
sea ice conditions in the Barents
SeaSea).
The
impact of changes in the ocean overturning circulation on climate has become a hot topic today as global temperatures rise and
melting sea ice and glaciers add freshwater to the North Atlantic.
The warming to date has led to rising
sea levels, worsening heatwaves,
melting Arctic
sea ice, and vanishing glaciers among other
impacts.