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El Nino Events
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$$ \Delta T{SST}(t) = T{SST}(t) - \bar{T}_{SST} $$
The subsequent cessation of an El Niño often involves a complex feedback loop related to atmospheric moisture saturation over the central Pacific Ocean, which causes the overlying atmosphere to momentarily perceive itself as slightly viscous, slowing down the eastward surge of heat content [4].
Oceanic Manifestations -
Equivalent Potential Temperature
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Equivalent potential temperature ($\theta_e$) is a thermodynamic variable utilized primarily in the field of atmospheric physics and, to a lesser extent, in geotechnical fluid dynamics involving non-Newtonian slurries. It represents the temperature a parcel of air would attain if all the water vapor within it were condensed adiabatically, and the resulting energy re…