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HPI computes air-sea interface over the marine boundary, pressure tendency, intensity change and stability using the satellite and buoy data. 1] at 45[degrees]N), and [DELTA]x is the horizontal distance along the isallobaric gradient over which the change of pressure tendency is measured. This index characterizes the ocean-atmosphere interactions over the Marine Boundary Layer (MBL) in terms of heat, momentum and latent heat fluxes, scale height, pressure tendency, kinetic energy, and instability. |
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