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Oct. 21 AIRS Meeting - AIRS Moisture Validation

Oct. 21 AIRS Meeting - AIRS Moisture Validation. Larry McMillin, Jiang Zhao, James Yoe, M. K. Rama Varma Raja, Seth Gutman Climate Research and Applications Division National Environmental Satellite, Data, and Information Service Washington, D.C. Larry.McMillin@noaa.gov.

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Oct. 21 AIRS Meeting - AIRS Moisture Validation

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  1. Oct. 21 AIRS Meeting - AIRS Moisture Validation Larry McMillin, Jiang Zhao, James Yoe, M. K. Rama Varma Raja, Seth Gutman Climate Research and Applications Division National Environmental Satellite, Data, and Information Service Washington, D.C. Larry.McMillin@noaa.gov L.M. McMillin NOAA/NESDIS/ORA

  2. 3 Way Moisture Comparisons • The following show 3-way comparisons of total precipitable water • Radiosondes • AIRS • GPS • The radiosondes that have close by GPS sites have been selected and matched with the GPS and AIRS data • The color shows the radiosonde types L.M. McMillin NOAA/NESDIS/ORA

  3. RAOB versus GPS L.M. McMillin NOAA/NESDIS/ORA

  4. AIRS versus GPS L.M. McMillin NOAA/NESDIS/ORA

  5. AIRS versus raob L.M. McMillin NOAA/NESDIS/ORA

  6. Comparisons looking along the major direction. The largest scatter is in the AIRS – raob direction L.M. McMillin NOAA/NESDIS/ORA

  7. Average Precipitable Water (mm) L.M. McMillin NOAA/NESDIS/ORA

  8. Covariances (mm2) L.M. McMillin NOAA/NESDIS/ORA

  9. Correlations - AIRS/GPS is slightly higher than AIRS/raob, GPS/raob is lowest L.M. McMillin NOAA/NESDIS/ORA

  10. Eigenvector direction • Direction of the major eigenvector • Raob 0.995545 • AIRS 1.000000 • GPS 0.997518 • Again AIRS is slightly better fit to GPS L.M. McMillin NOAA/NESDIS/ORA

  11. Conclusions • AIRS agrees well with radiosondes and GPS • AIRS has a slightly better fit with GPS • Both GPS and radiosondes show a larger total range of values than AIRS • Note AIRS retrievals are limited to clear areas so there could a natural bias • Even cloud cleared values represent the areas between clouds in partly cloud regions • AIRS seems to be slightly biased high with respect to the others • Next step is to use the GPS values to adjust the radiosondes and examine the vertical profiles • Initial results how improvement at lower levels and degradation at upper levels - raobs can have a dry bias at upper levels and two dry biases (raob and AIRS) can agree without being right ? L.M. McMillin NOAA/NESDIS/ORA

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  14. Layer Precipitable Water AIRS V3.0.8 with QAFlag=0 RAOB Type 61 Viasalla RS-80 expected dry bias L.M. McMillin NOAA/NESDIS/ORA

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  20. Layer Precipitable Water AIRS V3.0.8 with QAFlag=0 RAOB Type 71 Viasalla RS 90 smaller bias Upper levels are probably not reliable L.M. McMillin NOAA/NESDIS/ORA

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  30. Layer Average Temperature Airs v3.0.8 , QAFlag=0 All RAOB types L.M. McMillin NOAA/NESDIS/ORA

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