Lack of Arctic
Ocean ice ultimately gave Katrina's warmer Gulf of Mexico SST's, worldwide heat has reached a new balance.
Not exact matches
Retreating sea
ice in the Iceland and Greenland Seas may be changing the circulation of warm and cold water in the Atlantic
Ocean, and could
ultimately impact the climate in Europe, says a new study by an atmospheric physicist from the University of Toronto Mississauga (UTM) and his colleagues in Great Britain, Norway and the United States.
Ultimately, that could make the
ice flow faster to the
ocean.
What they found was that local destabilization of the Amundsen Sea region of West Antarctica
ultimately causes the entire
ice sheet to fall into the
ocean over several centuries to several thousands of years, gradually adding 3 meters to global sea levels, they report online today in the Proceedings of the National Academy of Sciences.
So, if Larsen C
ultimately breaks up, researchers are concerned that could be a sign that other
ice shelves holding back a large amount of land
ice could cause
oceans to rise.
If more
ice is lost at the margins than gained at the core, the
ice sheet shrinks,
ultimately affecting albedo as (depending on the underlying geography) lakes form, some rockbed is exposed and areas are reconquered by the
ocean.
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 US CLIVAR Greenland
Ice Sheet -
Ocean Interactions Working Group was formed to foster and promote interaction between the diverse oceanographic, glaciological, atmospheric and climate communities, including modelers and field and data scientists within each community, interested in glacier / ocean interactions around Greenland, to advance understanding of the process and ultimately improve its representation in climate mo
Ocean Interactions Working Group was formed to foster and promote interaction between the diverse oceanographic, glaciological, atmospheric and climate communities, including modelers and field and data scientists within each community, interested in glacier /
ocean interactions around Greenland, to advance understanding of the process and ultimately improve its representation in climate mo
ocean interactions around Greenland, to advance understanding of the process and
ultimately improve its representation in climate models.
Less
ice cover leads to more solar heating throughout the Arctic
Ocean, and ocean photosynthesis increases as more light penetrates into the water, ultimately resulting in «changes at the base of the ocean food chain,» according to the v
Ocean, and
ocean photosynthesis increases as more light penetrates into the water, ultimately resulting in «changes at the base of the ocean food chain,» according to the v
ocean photosynthesis increases as more light penetrates into the water,
ultimately resulting in «changes at the base of the
ocean food chain,» according to the v
ocean food chain,» according to the video.
These vastly irresponsible actions will further heat the atmosphere and
ocean — melting a greater share of the world's land
ice and forcing seas to
ultimately rise even more.
Since to me (and many scientists, although some wanted a lot more corroborative evidence, which they've also gotten) it makes absolutely no sense to presume that the earth would just go about its merry way and keep the climate nice and relatively stable for us (though this rare actual climate scientist pseudo skeptic seems to think it would, based upon some non scientific belief — see second half of this piece), when the earth changes climate easily as it is, climate is
ultimately an expression of energy, it is stabilized (right now) by the
oceans and
ice sheets, and increasing the number of long term thermal radiation / heat energy absorbing and re radiating molecules to levels not seen on earth in several million years would add an enormous influx of energy to the lower atmosphere earth system, which would mildly warm the air and increasingly transfer energy to the earth over time, which in turn would start to alter those stabilizing systems (and which, with increasing
ocean energy retention and accelerating polar
ice sheet melting at both ends of the globe, is exactly what we've been seeing) and start to reinforce the same process until a new stases would be reached well after the atmospheric levels of ghg has stabilized.
Using satellite and field work after an extreme melt event in Greenland, a UCLA - led study finds that melt - prone areas on its
ice sheet develop a remarkably efficient drainage system of stunning blue streams and rivers that carry meltwater into moulins (sinkholes) and
ultimately the
ocean.
I can only list a few regular «goings on'that I KNOW affect sea level; I'm certain that there are others: Change in overall temperature of the
oceans (a few millidegrees / mm), plate tectonics, slit from rivers, erosion of seashores, extraction of ground water which
ultimately returns to the
oceans, marine life and its products building up the
ocean floors, melting land
ice, undersea discharges of a variety of «stuff» from literally hundreds of thousands of sources, often at temperatures in the 1 - 2 thousand degree range, which we are only now beginning to notice, wind carrying dust from the land and dropping it on the
ocean.