The cooling increases
polar sea level pressure pushing the storms circling the pole into higher latitudes.
Not exact matches
Freshwater injection into the North Atlantic and Southern oceans increases
sea level pressure at middle latitudes and decreases it at
polar latitudes (Figs. 20, S22), but the impact is different in the North Atlantic than in the Southern Ocean.
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.
Substantial weakening of the
polar cell due to increase in
sea -
level pressure over
polar latitudes leads to a negative trend of the winter AO index.
The strength of these currents is influenced by the location of the
polar fronts as determined by
sea level pressures in the Southern and Northern Annular Modes.
The
polar front changes largely in response to
sea level pressure difference between the pole and the sub-Antarctic — as measured by the Southern Annular Mode (SAM) index.
The
polar changes in
sea level pressure seem to be driven by ozone and UV interactions in the stratosphere.
This in turn is influenced by
sea level pressure patterns in
polar and subpolar regions — as more or less wind and currents are pushed north (Roemmich et al, 2007, Qiu, Bo et al 2006).
Sea level pressure in the polar and sub polar regions are measured in the Southern and Northern Annular Modes — the changes in sea level pressure creates the potential for the anomalous movement of atmospheric mass into lower latitud
Sea level pressure in the
polar and sub
polar regions are measured in the Southern and Northern Annular Modes — the changes in
sea level pressure creates the potential for the anomalous movement of atmospheric mass into lower latitud
sea level pressure creates the potential for the anomalous movement of atmospheric mass into lower latitudes.