Abstract
In this paper we present a comparison between observed data and a number of simulations of early winter 1991/1992, carried out with a mechanistic model of the middle atmosphere (based upon the U.K.M.O. Stratosphere-Mesosphere Model). The model was integrated from early November 1991 through to mid January 1992, a period when the real atmosphere was in the throes of a very significant stratospheric warming.
The simulations differed mainly in that they were performed with a variety of parameterizations of the gravity wave drag. It is seen that the various gravity wave parameterizations have significant effects on the modelled evolution leading up to the observed mid-January warming. The simulated sequence of events is shown to be sensitive to the scheme used and the strength of the wave breaking resulting. It is found that the impact of the mesospheric wave drag is seen low in the stratosphere. The simulations are compared with observations obtained by the Improved Stratospheric and Mesospheric Sounder (ISAMS) which flew aboard the upper Atmosphere Research Satellite (UARS) and collected data during late 1991 and some of 1992.
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Lawrence, B.N. (1997). The Effect of Parameterized Gravity Wave Drag on Simulations of the Middle Atmosphere during Northern Winter 1991/1992 — General Evolution. In: Hamilton, K. (eds) Gravity Wave Processes. NATO ASI Series, vol 50. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-60654-0_20
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DOI: https://doi.org/10.1007/978-3-642-60654-0_20
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