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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