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- W3022341812 abstract "Baroclinic eddy equilibration under a Northern Hemisphere‐like seasonal forcing is studied using a modified multilayer quasigeostrophic channel model to investigate the widely used ‘‘quick baroclinic eddy equilibration’’ assumption and to understand to what extent baroclinic adjustment can be applied to interpret the midlatitude climate.Under aslowly varyingseasonalforcing, the eddyand meanflow seasonalbehavioris characterized by four clearly divided time intervals: an eddy inactive time interval in summer, a mainly dynamically determined eddy spinup time interval starting in midfall and lasting less than one month, and a quasi-equilibrium time interval for the zonal mean flow available potential energy from late fall to late spring, with a mainly external forcing determined spindown time interval for eddy activity from late winter to late spring. The baroclinic adjustment can be clearly observed from late fall to late spring. The sensitivity studyof the eddyequilibrationto the time scale of the external forcing indicatesthat the time scale separation between the baroclinic adjustment and the external forcing in midlatitudes is only visible for external forcing cycles one year and longer. In spite of the strong seasonality of the eddy activity, similar to the observations, a robust potential vorticity (PV)structureisstillobservedthroughalltheseasons.However,itisfoundthatbarocliniceddyisnottheonly candidatemechanismtomaintaintherobustPVstructure.Theroleoftheboundarylayerthermalforcingand the moistconvectionin maintaining the lower-levelPV structureisdiscussed. Theadjustment and thevertical variation of the lower-level stratification play an important role in all of these mechanisms." @default.
- W3022341812 created "2020-05-13" @default.
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- W3022341812 date "2010-08-01" @default.
- W3022341812 modified "2023-09-28" @default.
- W3022341812 title "Baroclinic Eddy Equilibration under Specified Seasonal Forcing" @default.
- W3022341812 hasPublicationYear "2010" @default.
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