Not exact matches
Worldwide, particularly in deeply buried permafrost and in
high -
latitude ocean sediments
where pressures are
high and temperatures are below freezing, icy deposits called hydrates hold immense amounts of methane (SN: 6/25/05, p. 410).
Collectively, these observations can be used to project trends of
ocean acidification in
higher latitude marine surface waters
where inorganic carbon chemistry is largely influenced by sea ice meltwater.
That first linkage will be the start of a quickly expanding Greenland Sea,
where the ice dynamics will closely resemble those of the current Arctic
Ocean — except that it will be at a lower
latitude and
higher temperatures.
Specifically, he pinpoints the slow response to
ocean heat uptake in the
high latitude regions,
where the
oceans are most unstable to vertical mixing.
First, the deep
ocean and
high -
latitude surface
ocean where deep water forms are approaching the freezing point in the Late Cenozoic.
When a large surge of polar air moves equatorward it draws a pulse of energy from the
oceans in the lower latitudes and pumps it into the stratosphere
where most of that energy is pushed out to space but a portion is not pushed out and descends again thus strengthening the
high pressure systems on the poleward side of the mid
latitude jets.