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.
32.
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.
33.
It is instructive to examine the limiting cases, in which \ scriptstyle { \ tau } is very large ( adiabatic, or gradual change ) and very small ( diabatic, or sudden change ).
34.
Although rigorous validation of a diabatic representation requires knowledge of vibronic coupling, it is often possible to construct such diabatic representations by referencing the continuity of physical quantities such as dipole moment, charge distribution or orbital occupations.
35.
Although rigorous validation of a diabatic representation requires knowledge of vibronic coupling, it is often possible to construct such diabatic representations by referencing the continuity of physical quantities such as dipole moment, charge distribution or orbital occupations.
36.
At the crossing point of the charge-localized diabatic surfaces the Born-Oppenheimer adiabatic ground and excited state surfaces move up and down in energy, respectively, by the amount | V _ { DA } |.
37.
Where \ scriptstyle { \ mu } is the magnetic moment of the atom, assumed to be the same for the two diabatic states, and \ scriptstyle { a } is some time-independent coupling between the two states.
38.
However, the diabatic effects are responsible for the jet subsiding behind the leading edge of the MCS . The sinking of the jet first starts when the mid level inflow goes under the trailing stratiform cloud before descending to the melting layer.
39.
Molecular-orbital occupancies representing ground ( G ) and excited ( S-singly, D-doubly, T-triply, Q-quadruply ) states, described in the delocalized diabatic basis, pertinent for various common chemical processes.
40.
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.
