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Improving forecast skill by assimilation of quality‐controlled AIRS temperature retrievals under partially cloudy conditions
Author(s) -
Reale O.,
Susskind J.,
Rosenberg R.,
Brin E.,
Liu E.,
Riishojgaard L. P.,
Terry J.,
Jusem J. C.
Publication year - 2008
Publication title -
geophysical research letters
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.007
H-Index - 273
eISSN - 1944-8007
pISSN - 0094-8276
DOI - 10.1029/2007gl033002
Subject(s) - atmospheric infrared sounder , environmental science , troposphere , geopotential height , depth sounding , data assimilation , forecast skill , radiance , meteorology , polar vortex , tropopause , cloud cover , anomaly (physics) , satellite , climatology , geopotential , northern hemisphere , remote sensing , cloud computing , geology , computer science , geography , physics , precipitation , oceanography , condensed matter physics , aerospace engineering , engineering , operating system
The National Aeronautics and Space Administration (NASA) Atmospheric Infrared Sounder (AIRS) on board the Aqua satellite is now recognized as an important contributor towards the improvement of weather forecasts. At this time only a small fraction of the total data produced by AIRS is being used by operational weather systems. In fact, in addition to effects of thinning and quality control, the only AIRS data assimilated are radiance observations of channels unaffected by clouds. Observations in mid‐lower tropospheric sounding AIRS channels are assimilated primarily under completely clear‐sky conditions, thus imposing a very severe limitation on the horizontal distribution of the AIRS‐derived information. In this work it is shown that the ability to derive accurate temperature profiles from AIRS observations in partially cloud‐contaminated areas can be utilized to further improve the impact of AIRS observations in a global model and forecasting system. The analyses produced by assimilating AIRS temperature profiles obtained under partial cloud cover result in a substantially colder representation of the northern hemisphere lower midtroposphere at higher latitudes. This temperature difference has a strong impact, through hydrostatic adjustment, in the midtropospheric geopotential heights, which causes a different representation of the polar vortex especially over northeastern Siberia and Alaska. The AIRS‐induced anomaly propagates through the model's dynamics producing improved 5‐day forecasts.