D. Pendlebury

Processes of the upper stratosphere and lower mesosphere in reanalyses

Reanalyses generally have low model tops. Some, however, extend into the upper stratosphere and lower mesosphere, and it is of interest to examine the dynamical processes that are present in this region including. The talk will focus on recent studies of some of these phenomena in reanalysis data, including stratospheric sudden warmings and tides, and on comparing the reanalyses that extend past 10 hPa.
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