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• W2015364557 abstract "The transformed Eulerian‐mean momentum and continuity equations are used to calculate the residual mean meridional circulations for the lower stratosphere and troposphere. Momentum and temperature fluxes required for the computation are estimated from U.K. Meteorological Office (UKMO) analyzed geopotential heights. National Center for Atmospheric Research (NCAR) CCM2 model output is used to assess the errors associated with the calculation. The model comparisons showed that the method works reasonably well for solstice seasons, but is inadequate for equinox seasons. In addition, it is found that some parameterization of gravity wave drag needs to be included with the planetary wave forcing to accurately estimate the residual mean circulation using this method." @default.
• W2015364557 created "2016-06-24" @default.
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• W2015364557 date "1993-06-20" @default.
• W2015364557 modified "2023-10-04" @default.
• W2015364557 title "Estimates of the stratospheric residual circulation using the downward control principle" @default.
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• W2015364557 doi "https://doi.org/10.1029/93jd00392" @default.
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