Initially, shallow circulations driven by differential
radiative cooling induce a self - aggregation of the convection into a single band, as has become familiar from simulations over idealized sea surfaces.
Not exact matches
Another important paper of recent is by Easterling and Wehner that demonstrates that
cooling on timescales of years to a decade or two are not that unusual even when the system is undergoing a long - term warming trend
induced by
radiative forcing.
This is primarily based on the idea that the
radiative flux would
induce significant warming, but then the evaporation from the oceans and convective transport have a
cooling effect.
Our results show that repeated clusters of volcanic eruptions can
induce a net negative
radiative forcing that results in a centennial and global scale
cooling trend via a decline in mixed - layer oceanic heat content.
The skin itself
cools by about 0.3 or 0.4 K due to
radiative fluxes at the skin surface, which is a change that is two orders of magnitude greater than the alleged heat change in the skin layer
induced by GHGs.