A diabatic heating scheme was later added, to allow for multiple isentropic levels with transport between them on longer timescales, although the name " SLIMCAT " has remained despite the multiple levels.
2.
Furthermore, diabatic heating perturbations are also shown to be linked to cross-equatorial SST changes, with positive anomalies being observed over the warmer Northern hemisphere waters and negative ones over the Southern hemisphere.
3.
Therefore, because of internal diabatic heating / cooling by molecular / turbulent diffusion, the overall heating experienced by a stratified fluid always occurs at greater pressure than the total cooling, even if the external cooling / heating occur at the same pressure.
4.
As a result, internal diabatic heating / cooling due to molecular diffusion explains why laboratory experiments show evidence of circulations developing as the result of surface heating / cooling ( Park and Whitehead, 2000 ) or even when the heating is above the cooling ( Coman et al ., 2006 ).
5.
A 2005 National Research Council report concluded " regional variations in radiative forcing may have important regional and global climate implications that are not resolved by the concept of global mean radiative forcing . " and " Regional diabatic heating can cause atmospheric teleconnections that influence regional climate thousands of kilometers away from the point of forcing ."
6.
Where f _ 0 is the Coriolis parameter, approximated by the constant 1e " 4 s " 1; R is the atmospheric ideal gas constant; \ beta is the latitudinal change in the Coriolis parameter \ beta = \ frac { \ partial f } { \ partial y }; \ sigma is a static stability parameter; c _ p is the specific heat at constant pressure; p is pressure; T is temperature; anything with a subscript g indicates geostrophic; anything with a subscript a indicates ageostrophic; J is a diabatic heating rate; and \ omega is the Lagrangian rate change of pressure with time . \ omega = \ frac { Dp } { Dt }.
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