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• W2094701727 abstract "Abstract The quasigeostrophic geopotential tendency equation is derived using P vectors in both pressure and entropy coordinates. This vector form of the geostrophic forcing in the geopotential tendency equation is similar to the Q-vector form of the ω equation. It is shown that the horizontal components of P are the advection of geostrophic momentum and the vertical component of P is the horizontal temperature advection. The P vectors are shown to be related to Q and C vectors, as well as the ageostrophic circulation. The three-dimensional pseudocurl of the P vector gives the C vector that equals the ageostrophic pseudovorticity in the quasigeostrophic model. The horizontal components of the pseudocurl of P are perpendicular and proportional to the Q. The horizontal divergence of the P vector is the geostrophic absolute vorticity advection while the three-dimensional divergence of the P vector is the geostrophic quasigeostrophic potential vorticity advection. The ageostrophic wind can be partitioned into..." @default.
• W2094701727 created "2016-06-24" @default.
• W2094701727 creator A5017863962 @default.
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• W2094701727 date "1995-03-01" @default.
• W2094701727 modified "2023-09-27" @default.
• W2094701727 title "Pvectors as a Diagnostic Tool for Synoptic-Scale Circulations" @default.
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• W2094701727 doi "https://doi.org/10.1175/1520-0493(1995)123<0776:vaadtf>2.0.co;2" @default.
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