Sentences with phrase «arctic sea water»

Not exact matches

He said that sensitivity includes water vapour and arctic sea ice, but I suspect that the changes in sea ice in the models are much less than we are seeing in practice.
WILD POLLOCK OIL FROM THE ARCTIC WATERS OF ALASKA Living in the pristine, icy cold waters of the Bering Sea, wild Alaskan Pollock is an excelWATERS OF ALASKA Living in the pristine, icy cold waters of the Bering Sea, wild Alaskan Pollock is an excelwaters of the Bering Sea, wild Alaskan Pollock is an excellen...
WILD POLLOCK OIL FROM THE ARCTIC WATERS OF ALASKA Living in the pristine, icy cold waters of the Bering Sea, wild Alaskan Pollock is an excellent and sustainable natural source of fish oil rich in Omega - 3 fatty WATERS OF ALASKA Living in the pristine, icy cold waters of the Bering Sea, wild Alaskan Pollock is an excellent and sustainable natural source of fish oil rich in Omega - 3 fatty waters of the Bering Sea, wild Alaskan Pollock is an excellent and sustainable natural source of fish oil rich in Omega - 3 fatty acids.
Apart albedo, shouldn't we expect a classical water vapour feedback (and so DLF forcing) as arctic ice is melting and arctic seas / ocean warming?
Also less ice cover allows the vastly warmer sea water to warm the much colder arctic air.
A good point as arctic regions that are hit with warmer water streams will prevent sea ice extent while those with colder ones can massivly increase in volume when the air is cold enough though no growth would be visible from the top down view.
[2] Expected impacts include a sea level rise up to 6 - 7m, melting permafrost in the arctic regions, large - scale agricultural losses, increased water scarcity, a collapse of the Gulf Stream in the Atlantic Ocean and an increase of extreme weather events such as floods, droughts or devastating storms.
IMO, none of this supports the «open water» nonsense we got from the press last winter unless you want to restrict global arctic sea ice to the Hudson Bay.
It emphasises that there is a strong internal relationship between the formation, stability and extent of sea ‐ ice and the structure of the upper layer of the Arctic ocean: it is the relative area and depth of low - salinity arctic water above the halocline that are paramount to ice formation and its summer survival.
To summarise the arguments presented so far concerning ice - loss in the arctic basin, at least four mechanisms must be recognised: (i) a momentum - induced slowing of winter ice formation, (ii) upward heat - flux from anomalously warm Atlantic water through the surface low ‐ salinity layer below the ice, (iii) wind patterns that cause the export of anomalous amounts of drift ice through the Fram Straits and disperse pack - ice in the western basin and (iv) the anomalous flux of warm Bering Sea water into the eastern Arctic of the mid 1990s.
And, once the summer season is passed, the ever - colder Arctic air masses remove even more heat from the under - ice water up through the sea ice by conduction into the -25 deg arctic air.
Zhang, J., M. Steele, and R. Woodgate, The role of Pacific water in the dramatic retreat of arctic sea ice during summer 2007, J. Polar Science, 19 (2), 93 - 107, 2008.
There are useful things that can be said related to Atlantic temperatures, sea level, and water vapour, but the specific circulation link to arctic sea ice is tenuous at best, and completely speculative at worst.
Spraying sea water into the arctic is ******** moronic.
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