This matters because the north /
south temperature difference is one of the main drivers of the jet stream.
Not exact matches
The
difference between ocean and air
temperature also tends to create heavy morning fog during the summer months, known as the marine layer, driven by an onshore wind created by the local high pressure sunny portions of the Salinas Valley, which extend north and
south from Salinas and the Bay.
It hardly takes imagination to posit that while initial aerosol dimming might depress
temperatures, the aerosols and atmosphere might react in ways that change heat balance in other directions as they disperse, through stratospheric chemistry, and the fact that, unsurprisingly, there is a
difference in aerosol behaviour depending on day vs night (you can't reduce the sunlight that reaches the
south pole on June 23rd....).
Average July
temperatures range from 2.4 °C to 3.6 °C on the
south coast but notable
differences in
temperature occur with
differences in terrain, and in the intermontane depressions,
temperatures can reach 10 °C.
One hypothesis suggests that the shrinking
temperature difference between the Arctic and the mid-latitudes will lead to a slowing of the jet stream, which circles the northern latitudes and normally keeps frigid polar air sharply separated from warmer air in the
south.
In the past, a high
difference in
temperature from north to
south helped drive a prevailing wind pattern called the Jet Stream which kept weather systems moving across the Northern Hemisphere.
The new twist in this story is that the Arctic has been warming at at least double the pace of the rest of the globe, meaning that the
difference in
temperature between the Arctic and areas farther
south has been shrinking.
The
temperature difference projected for the 30 % reduction in RGGI emission is equivalent to going
south 159 feet.
But as the
difference between north and
south temperatures dropped, weather systems tended to stall.
The increase in average
temperature between the nineteenth and twentieth centuries exceeded the
temperature difference between all other consecutive centuries in each region, except Antarctica and
South America.»
And since the
temperature difference between the Arctic and the tropics is narrowing, and since it's the
temperature difference that drives wind and ocean currents, then the jet stream that normally whizzes around the Arctic circle — thus keeping frozen air in one place and separating it from the warm breezes of the
south — is, the theory goes, slowing, thus allowing warm moist air to penetrate into the north.
Since the Arctic is warming faster than the midlatitudes to the
south, the
temperature difference between these two regions is smaller.
The
difference in
temperature between the Arctic and areas to the
south is what drives the jet stream, a fast - moving river of air that encircles the northern hemisphere.