📝 SummarXiv

Abstract

Tropical East and West Pacific Oceans display differences in their vertical velocity (or omega) profiles. The East Pacific is characterized by bottom-heavy profiles, while the West Pacific is characterized by top-heavy profiles. Although inter-basin differences in the horizontal SST gradient are known to be important, physical reasons for why these omega structure variants exist are not fully understood. This question is addressed using a steady, linear model on an $f$-plane with $n$ atmospheric layers. Convection and radiation are parameterized as linear responses to thermodynamic perturbations with convective nonlinearity approximated by convection on/off regimes. The free (or eigen) modes of the model yield vertical structures resembling the observed baroclinic modes of the tropical atmosphere, with each mode associated with a characteristic horizontal scale (the eigenvalue). In the standard parameter regime, the first-baroclinic mode has a large spatial scale ($\sim$ 1500 km) while the second-baroclinic mode has a smaller spatial scale ($\sim$ 250 km). When the model is forced with a strong- and weak-gradient surface temperature ($T_s$) patterns, the resulting omega profiles assume bottom- and top-heavy structures respectively -- mimicking the observed differences between East and West Pacific Oceans. Additional dependence on the magnitude of the Coriolis force is also observed. The connection between the vertical structure and the horizontal scale of the baroclinic modes explains why a strong-gradient $T_s$ profile projects strongly onto the second-baroclinic mode yielding bottom-heavy omega profiles in the eastern Pacific, while a weak-gradient $T_s$ profile projects strongly onto the first-baroclinic mode, yielding top-heavy omega profiles typical of the Western Pacific.