Cameron's thesis is entitled Understanding Climatic Adjustments to Variations in
Tropical Ocean Heat Transport.
Not exact matches
A continual cycle of
heat and moisture is pulled from the
tropical ocean and
transported around the globe on belts of atmospheric energy.
And no, there is no huge plunge in
tropical or global surface air temperatures when the
ocean circulation spins up because there is a near - compensating decrease in poleward
heat transport via the atmospheric circulation.
A good explanation of the details is provided here: Koll & Abbot (2013)-- Why
Tropical Sea Surface Temperature is Insensitive to
Ocean Heat Transport Changes.
If
tropical cyclone occurrence decreases, less of the
heat is dissipated, and unless
ocean circulation in some way compensates by
transporting the additional thermal energy elsewhere (i.e. for example out of the «main development region» of the Atlantic) some day a storm will tap the enhanced energy source.
Stronger vertical mixing invigorates the MOC [Meridonal Overturning Circulation] by an order of magnitude, increases
ocean heat transport by 50 — 100 %, reduces the zonal mean equator - to - pole temperature gradients by up to 6 °C, lowers
tropical peak terrestrial temperatures by up to 6 °C, and warms high - latitude
oceans by up to 10 °C.»
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, 2
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, 2
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).
Heat from anomalously warm
ocean temperatures is
transported vertically and eventually northward by unusually active
tropical convection (thunderstorms), warming the upper atmosphere in the lower latitudes.
We find that an increase in poleward
heat transport by the
tropical ocean results in a warming of the extra-tropics, relatively little change in the
tropical temperatures, moistening of the subtropical dry zones, and partial but incomplete compensation of the planetary - scale energy
transport by the atmosphere.
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?
Effects of
tropical cyclones on
ocean heat transport in a high resolution coupled general circulation model.