Sea surface winds derived from cloud motion vectors over the tropical Atlantic
✍ Scribed by Silke Zank
- Publisher
- Springer
- Year
- 1980
- Tongue
- English
- Weight
- 529 KB
- Volume
- 19
- Category
- Article
- ISSN
- 0006-8314
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✦ Synopsis
The relationship between satellite-derived low-level cloud motion, surface wind and geostrophic wind vectors is examined using GATE data. In the trades, surface wind speeds can be derived from cloud motion vectors by the linear relation: V = 0.62 V, + 1.9 m s-l with a mean scatter of f 1.3 m s-l. The correlation coefficient between surface and satellite wind speed is 0.25. Considering baroclinicity, i.e., the influence of the thermal wind, the correlation coefficient does not increase, because of the uncertainty of the thermal wind vectors. The ratios of surface to geostrophic wind speed and surface to satellite wind speed are 0.7 and 0.8, respectively, with a statistical uncertainty of i0.3. Calculations of the ratio of surface to geostrophic wind speed on the basis of the resistance law yield V/V, = 0.8rt 0.2, in agreement with experimental results. The mean angle difference between the surface and the satellite wind vectors amounts to (Y = 18", taking into account baroclinicity. This value is in good agreement with the mean ageostrophic angle (Y = 25".