The Impact of ATOVS Radiance in MERRA Reanalysis

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$A 10 year climatology of cloud fraction and vertical distribution ...$

At most areas, the analysis temperature increment try to coolthe atmosphere which is warmed up by the moisture processdriven by moisture increment.
The additional precipitation from moisture increment warms theatmosphere. The warm effect is almost offset by the negativetemperature increment.
Page 1 and 2: The Impact of ATOVSRadiance in MERR
Page 3 and 4: At the Beginning, the Idea of Reana
Page 5 and 6: Features in the NASA MERRA reanalys
Page 8 and 9: Radiosonde, PIBAL wind, aircraft re
Page 10 and 11: The impact of NOAA15 (ATOVS)A two y
Page 12 and 13: The precipitation difference betwee
Page 14 and 15: Change of moisture mainly in the lo
Page 16 and 17: Precipitation removes the additiona
Page 20 and 21: Associated with the introduction of

The Impact of ATOVS Radiance in MERRA Reanalysis

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