Monday, 10 January 2000
This paper will present an assessment of the impact to the
stratospheric circulation of the DAO-GEOS2 (Data Assimilation Office
-Goddard Earth Observing System) attributable to an improved 1DVaritional
retrieval of heights. The assimilated heights are retrieved from both
the TOVS (TIROS Operational Vertical Sounder) and the ATOVS (Advanced TOVS)
sounders. Each sounder's sensitivity to temperature changes in the
stratosphere will be addressed and its relationship to the model's
background flow evaluated. Also detailed are the steps to ensure
the quality of the data being assimilated. Finally the temporal and
spatial scales, important to the stratospheric mean flow, will be
evaluated in terms of the DAO-GEOS2 response to the assimilated
heights.
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