Abstract
Upper tropospheric temperature anomalies are detected in brightness temperature data from the Nimbus 6 Scanning Microwave Spectrometer (SCAMS). Brightness temperature anomalies are related to surface pressure anomalies through the radiative transfer and hydrostatic equation. Surface wind speeds at outer radii are then estimated using the gradient wind equation and a shearing parameter. The method is first tested using simulated satellite data constructed from temperature, pressure and height data recorded by aircraft reconnaissance of four hurricanes. Wind speeds in the 80–95 kPa region are estimated with 2–3 m s−1 accuracy, Next, 55.45 GHz SCAMS data over eight typhoons during 1975 are used to estimate the radii of 15.4 m s−1 (30 kt) and 27.5 m a−1 (50 kt) winds. Accuracies of about ±80 and ±70 km, respectively, are found. It is suggested that the technique be further tested using data from the Microwave Sounding Unit (MSU) on board the TIROS-N and NOAA 6 satellites.
