It has been noted in a five - member multi-model ensemble analysis that, associated with the changes in temperature of the upper ocean in Figure 10.7, the tropical
Pacific Ocean heat transport remains nearly constant with increasing greenhouse gases due to the compensation of the subtropical cells and the horizontal gyre variations, even as the subtropical cells change in response to changes in the trade winds (Hazeleger, 2005).
Not exact matches
By analogy, a warmer world wouldn't be rainier (or cloudier); it's an imperfect analogy, because rain isn't absolutely correlated with cloudiness, and lateral
transport of energy by
ocean, air, and latent heat currents in and out of the E & W Pacific Ocean areas won't scale to global wa
ocean, air, and latent
heat currents in and out of the E & W
Pacific Ocean areas won't scale to global wa
Ocean areas won't scale to global warming
Consenquently, the associated SST pattern is slightly cooler in the deep convection upwelling regions of the Equitorial
Pacific and the Indian
Ocean, strongly cooler in the nearest deep convection source region of the South Atlantic near Africa and the Equator, warm over the bulk of the North Atlantic, strongly warmer where the gulf stream loses the largest portion of its
heat near 50N 25W, and strongly cooler near 45N 45W, which turns out to be a back - eddy of the Gulf Stream with increased
transport of cold water from the north whenever the Gulf Stream is running quickly.
There is a tremendous amount of
ocean heat transport from both the
Pacific and the Atlantic going on in the Arctic.
In addition to the shallow La Niña — like patterns in the
Pacific that were the previous focus, we found that the slowdown is mainly caused by
heat transported to deeper layers in the Atlantic and the Southern
oceans, initiated by a recurrent salinity anomaly in the subpolar North Atlantic.
The evolution of global mean surface temperatures, zonal means and fields of sea surface temperatures, land surface temperatures, precipitation, outgoing longwave radiation, vertically integrated diabatic
heating and divergence of atmospheric energy
transports, and
ocean heat content in the
Pacific is documented using correlation and regression analysis.
For instance, if over 50 % of actual downwards
heat transport takes place in the West
Pacific / Southern Indian
Ocean (s), could differences in tropical cyclonic activity be driving the major differences in
heat flow?