1985
DOI: 10.1175/1520-0477(1985)066<1111:anowvw>2.0.co;2
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A Note on Water-Vapor Wind Tracking Using VAS Data on McIDAs

Abstract: Eleven data sets where water-vapor winds were obtained from the GOES-5 6.7-micrometer measurement over the United States are compared with rawinsondes. Over 2000 point comparisons are made for: a) an arbitrary height assignment of 400 mb; and b) a height assignment determined by matching the measured brightness temperature to the temperature structure represented in the LFM (Limited Area Fine Mesh) analysis. It is shown that the water vapor winds provide uniform horizontal coverage of midlevel flow with high a… Show more

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Cited by 32 publications
(14 citation statements)
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“…Temperature retrievals were performed using the AERI methodology 24 . The results shown in figure 10 reveal very close agreement between the three independent observations, all three illustrating the low level inversion during the night-time hours (12-15 GMT) eroding rapidly after sunrise during the morning hours (15)(16)(17)(18) and becoming a strong lapse rate condition during the early afternoon hours (18)(19)(20)(21)(22). Absolute differences between the GIFTS temperature profiles and the AERI and Radiosonde profiles are not considered to be significant since the GIFTS radiance calibration did not include a correction for detector/readout system non-linearity.…”
Section: Gifts Engineering Demonstration Unit (Edu) Science Resultssupporting
confidence: 82%
See 1 more Smart Citation
“…Temperature retrievals were performed using the AERI methodology 24 . The results shown in figure 10 reveal very close agreement between the three independent observations, all three illustrating the low level inversion during the night-time hours (12-15 GMT) eroding rapidly after sunrise during the morning hours (15)(16)(17)(18) and becoming a strong lapse rate condition during the early afternoon hours (18)(19)(20)(21)(22). Absolute differences between the GIFTS temperature profiles and the AERI and Radiosonde profiles are not considered to be significant since the GIFTS radiance calibration did not include a correction for detector/readout system non-linearity.…”
Section: Gifts Engineering Demonstration Unit (Edu) Science Resultssupporting
confidence: 82%
“…Such a feature-tracking approach that employs imager and sounder radiance fields is now used operationally and has been shown to provide improved weather forecasts on both regional and global scales 15,16,17 . However, the current GOES application only provides water vapor tracked winds derived from three broad water vapor channels 18,3 , which limits the vertical resolution and accuracy of the wind product. More complete vertical profiles of wind velocity are needed to realize the full potential of satellite measurements to improve both regional scale intense weather forecasts and global scale synoptic weather predictions 2,19 .…”
Section: Gifts Science Applicationsmentioning
confidence: 99%
“…The root-mean square vector difference was approximately 9 m/s. Comparable differences have been reported in other comparisons of radiosonde and satellite winds (e.g., see Stewart et al, 1985).…”
Section: Datamentioning
confidence: 99%
“…Monitoring of cloud motions has a positive influence on synoptic-scale analyses and forecasts (Virji, 1981) but demands the use of automated methods of tracking (Endlich and Wolf, 1981;Tsuchiya and Downey, 1981). In cloud-free areas, winds can often be derived with useful accuracy from water vapor data (Stewart et al, 1985).…”
Section: Satellite Windsmentioning
confidence: 99%