Validation of the Aura MLS cloud ice water content measurements

Retrieval and validation of upper tropospheric ice water content (IWC) measurements with the Aura Microwave Limb Sounder (MLS) are described. The MLS version 2.2 (V2.2) IWC, derived from 240‐GHz cloud‐induced radiances (Tcir) at high tangent heights, is scientifically useful at 215–83 hPa. The V2.2...

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Bibliographic Details
Published in:Journal of Geophysical Research: Atmospheres 2008-08, Vol.113 (D15), p.n/a
Main Authors: Wu, Dong L., Jiang, Jonathan H., Read, William G., Austin, Richard T., Davis, Cory P., Lambert, Alyn, Stephens, Graeme L., Vane, Deborah G., Waters, Joe W.
Format: Article
Language:English
Subjects:
cloud ice
Clouds
Computer simulation
Geophysics
Inhomogeneity
microwave
Moisture content
Probability density functions
Retrieval
Tangents
troposphere
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Summary:Retrieval and validation of upper tropospheric ice water content (IWC) measurements with the Aura Microwave Limb Sounder (MLS) are described. The MLS version 2.2 (V2.2) IWC, derived from 240‐GHz cloud‐induced radiances (Tcir) at high tangent heights, is scientifically useful at 215–83 hPa. The V2.2 IWC represents a bulk cloud property averaged over a ∼300 × 7 × 4 km3 volume near the pointing tangent height. Precision, accuracy, and spatial resolution of the V2.2 IWC are determined through model simulations and comparisons with CloudSat observations. Comparisons of MLS V2.2 and CloudSat R03 IWCs are made for the months of January and July in terms of normalized probability density function (PDF). The differences between MLS and CloudSat IWC PDFs are generally less than 50% over the IWC range where the MLS technique is valid. At pressures
ISSN:0148-0227
2169-897X
2156-2202
2169-8996
DOI:10.1029/2007JD008931