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Published byศิริโชค เก่งงาน Modified over 5 years ago
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Comparisons of TPARC P3DWL Wind Profiles with Dropsondes in the Presence of Clouds
D. Emmitt, K. Godwin and S. Greco Simpson Weather Associates WG-SBLW 2-3 February, 2010
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P3DWL for TPARC/TCS-08 1.6 um coherent WTX (ARL/LMCT)
10 cm bi-axis scanner (NASA) P3 and other parts (NRL) Analyses software (SWA/CIRPAS)
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Bi-axial scanner and instrument rack
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Typhoon Hagupit (0200GMT , September 22, 2008,)
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Multi layer clouds (0151 9/22)
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Deep aerosol layer capped with thin stratus
(0232 9/22)
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Multi cloud layers ( /22)
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Deep aerosol “misty” layer
(0111 9/22)
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High dense cloud (0131 9/22)
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Multi layer clouds (0151 9/22)
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Deep aerosol layer capped with thin stratus
(0232 9/22)
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Flight level clouds (0245 9/22)
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Summary Airborne DWL is beyond the technology demo and potpourri science stage Unique and “critical mass” observations are now available for use in PBL investigations and model validation/development Airborne DWL investigations for 2010 will focus upon tropical cyclones…. Noteworthy: active optical remote sensing inside a phenomena defined in large part by clouds.
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