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AIRS science team meeting, Greenbelt, 31 March 2003 Holger Vömel University of Colorado and NOAA/CMDL Cryogenic Frost point Hygrometer (CFH) Measurements.

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Presentation on theme: "AIRS science team meeting, Greenbelt, 31 March 2003 Holger Vömel University of Colorado and NOAA/CMDL Cryogenic Frost point Hygrometer (CFH) Measurements."— Presentation transcript:

1 AIRS science team meeting, Greenbelt, 31 March 2003 Holger Vömel University of Colorado and NOAA/CMDL Cryogenic Frost point Hygrometer (CFH) Measurements during AWEX and previous RS90 comparisons

2 Overview The University of Colorado Cryogenic Frost point Hygrometer (CU-CFH) Accuracies SnowWhite comparison with CFH RS90 comparisons with NOAA/CMDL hygrometer

3 CU-CFH Sonde Weight: ~ 500 gr Microprocessor controlled Digital interface with ECC Easy to use and robust Continuous measurements between surface and 28 km

4 Night launch, Oklahoma

5 Accuracy Measurement uncertainty of frostpoint temperature (AWEX)<.5K (2 σ) Air temperature measurement <.2K  Uncertainty in RH< 4…8% of RH value depending on altitude and uncertainty in air temperature Uncertainty in TPW < 5% Use WMO formulas to calculate vapor pressures (similar to Hyland and Wexler, which Vaisala uses)

6 CFH sounding Oklahoma MR

7 Mean comparison to Snow White vs CFH, Oklahoma

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9 RS90 comparisons with NOAA/CMDL hygrometer

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11 Take home message CFH measures on the 5% accuracy level. Snow White has no bias issue, but some performance limitations RS90 may have a slight dry bias 5-10% possibly due to contamination

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13 Snow White upper tropospheric limit Upper tropospheric limit depends on frost-point temperature At T FP < -75°C the Snow White does no longer measure reliably

14 Snow White upper tropospheric limit Upper tropospheric limit depends on frost-point temperature At T FP < -75°C the Snow White does no longer measure reliably


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