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- W2058142715 abstract "In the extratropics the analysis of the time–space structure of the dynamical tropopause shows a marked signature of nonpropagating, low-frequency (time-scale >10 d), ultra-long (zonal wavenumber <5) waves. This suggests the extension of theories relating the tropopause height to the baroclinic adjustment to the orographic-baroclinic disturbances, generally operating in the low-frequency domain. Such an extension is here proposed. By analysing Eady modes in a Boussinesq atmosphere, it has been found that the form-drag instability must be accounted for in an extended theory of baroclinic neutralization. The produced unstable standing waves carry a poleward large amount of heat at planetary scale for most of the external parameter settings and their spatial structure strongly resembles the observed winter mid-latitude eddy fields. Furthermore, we show how a simple representation of the stratosphere affects the tropopause neutralization requirements." @default.
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- W2058142715 date "2004-01-01" @default.
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- W2058142715 title "On the mid-latitude tropopause height and the orographic-baroclinic adjustment theory" @default.
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- W2058142715 doi "https://doi.org/10.3402/tellusa.v56i4.14423" @default.
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