The waters that underlie the near - surface subtropical waters have freshened due to
equatorward circulation of the freshened subpolar surface waters; in particular, the fresh intermediate water layer (at ~ 1,000 m) in the SH has freshened in both the Atlantic and Pacific Oceans.
Not exact matches
Where the poleward &
equatorward currents of this intensified
circulation converge — the centre of the gyres — surface water is pumped downwards into the ocean interior in a process known as Ekman pumping.
Thus, the subtropical gyre
circulation is a horizontal
circulation with poleward mass transport along the western boundary, and
equatorward transport everywhere east of that, and providing no net northward mass transport integrated across the basin (which is what Bryden et al have done).
I note that the subtropical arid zone tends to be located
equatorward of about 30 degrees, subject to various modifications due to
circulation and hemispheric asymmetry and whatnot.
The Atlantic Meridional Overturning
Circulation (AMOC)- the transport of warm tropical surface water northward - is indeed propelled by dense water sinking in the North Atlantic and travelling
equatorward in the deeper layers, but it also has a wind - driven component to it.
Additionally, the Atlantic Ocean is the only basin in which there is an
equatorward warm surface current (part of the Meridional Overturning
Circulation) and this ultimately carries heat to the North Atlantic - where it sinks.
The
circulation pattern described above — ascent in the equatorial trough, poleward movement in the upper troposphere, descent in the subtropical ridges, and
equatorward movement in the trade winds — is in effect a direct heat engine, which meteorologists call the Hadley cell.
At high latitudes the upwelling brings air rich in the heavy molecular constituents N2 and O2 to high altitudes and the
circulation carries this molecular - rich air to midlatitudes, especially in the summer hemisphere, where the mean meridional
circulation is already
equatorward.
The surface katabatic wind regime, directed
equatorwards and down the Antarctic coastal escarpment, closes the lower branch of the
circulation (Parish and Bromwich 2007).
The air
circulation systems move latitudinally poleward or
equatorward depending on whether there is net cooling or warming of the air at a gradual if variable rate all the time and climate shifts in any given location depend mainly on the changing position of that location in relation to the latitudinal position of the major air
circulation systems.
The thing is that as regards the sequence of observed events leading to changes in tropospheric temperature trends and the cyclical poleward and
equatorward shifts in the air
circulation systems the NCM is pretty robust.
xii) All regional climate changes are a result of movement in relation to the locally dominant air
circulation systems which move cyclically poleward and
equatorward.
It says nothing about real world events since then which, despite increasing ghgs, have gone into reverse with a cessation of stratospheric cooling and a return back
equatorward of the air
circulation systems.
The air
circulation systems in both hemispheres move back
equatorward and the ITCZ moves nearer the equator as the speed of the hydrological cycle decreases due to the warming stratosphere reducing the temperature differential between stratosphere and surface.
By AO being» stronger» I mean «negative» because it is the negative phase that pushes the air
circulation systems
equatorward.
Thus as sea ice expands in a cooler climate, the high - latitude oceanic heat loss to the atmosphere is inhibited, the thermohaline
circulation weakens, and the sinking regions move
equatorward, leading to a shallower and weaker deep
circulation.