ENSO has been proposed as a self - regulator of temperature that increases in convective activity in
response to temperature differential.
Not exact matches
Vegetation
responses to climate and rising CO2 are often cited as causal factors for
differential temperature increase near the surface.
In this way, the
response of LW fluxes (PR) and convection (CR) tend
to spread the
temperature response vertically from where forcings occur — not generally eliminating the effect of RF distribution over height, although in the case with convection driven by
differential radiative heating within a layer, CR can
to a first approximation evenly distribute a
temperature response over such a layer.
MD wave fades moving deeper into SH due
to lack of land mass & land impediment
to antarctic circumpolar (southern ocean) flow --(need midlatitude zonal land - sea contrast for meridional deflection of westerlies =
differential land - sea equator - pole column - integrated -
temperature gradient
response to solar forcing, easily measured using a simple wavelet tachometer, which detects externally governed universal constraint)