Assessment of Geo-Kompsat-2A Atmospheric Motion Vector Data and Its Assimilation Impact in the GEOS Atmospheric Data Assimilation System
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Date
2022-10-22
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Citation of Original Publication
Lee, Eunhee, Ricardo Todling, Bryan M. Karpowicz, Jianjun Jin, Akira Sewnath, and Seon Ki Park. 2022. "Assessment of Geo-Kompsat-2A Atmospheric Motion Vector Data and Its Assimilation Impact in the GEOS Atmospheric Data Assimilation System" Remote Sensing 14, no. 21: 5287. https://doi.org/10.3390/rs14215287
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Attribution 4.0 International (CC BY 4.0)
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Abstract
Korea’s second geostationary meteorological satellite, Geo-Kompsat-2A (GeostationaryKorean Multi-Purpose Satellite-2A, GK2A), was successfully launched on 4 December 2018. GK2A
generates Atmospheric Motion Vectors (AMVs) every 10 min in the full disk area. This data has
been disseminated via Global Telecommunication System (GTS) since 25 October 2019. This article
evaluates the quality of GK2A AMVs in the Goddard Earth Observing System (GEOS) atmospheric
data assimilation system (ADAS). The data show slow wind speed biases at 200–300 hPa and 600–800
hPa in the northern and southern hemispheres. These biases are caused by observation height
assignment errors near jet streams. The Equivalent Blackbody Temperature (EBBT) method of GK2A
tends to assign clouds at higher altitude, which mainly causes slow wind speed biases, especially in
the lower atmosphere. The IR/WV intercept method of GK2A assigns clouds slightly lower in the
atmospheric layers below the altitude of 400 hPa, which causes positive biases. Quality control (QC)
criteria to select the most suitable GK2A AMV data for assimilation are presented based on these
quality assessments. A new QC criterion utilizing height errors within the GEOS ADAS is introduced
to exclude data with slow wind speed biases and large errors. GEOS forecast accuracy is slightly
improved after assimilating GK2A AMVs along with other conventional, radiance, and satellite
winds which include AMVs made by the Himawari-8 satellite in nearly the same observational area
of GK2A. Additionally, the present work shows that GEOS forecasts can be significantly improved,
especially in the tropics and southern hemisphere after assimilating GK2A data in the absence of
Himawari-8 AMVs. This study demonstrates that GK2A AMV data is a valuable data source to
enhance the robustness of GEOS ADAS.