A Diagnostic Study of the Low-Level Jet during TAMEX IOP 5

Abstract During 31 May–2 June 1987 a low pressure center developed around 28°N, 102°E in the lee of the Tibetan Plateau during the passage of a midlatitude trough. It moved northeastward and intensified over the Yangtze River valley and produced widespread rainfall over southeastern China. A strong southwest flow developed in the lower troposphere over southern China as the cyclone deepened. At 0000 UTC 1 June, a well-defined low-level jet (LLJ) was found between the 850- and 700-hPa levels with wind speed exceeding 15 m s−1 at the 850-hPa level and 20 m s−1 at the 700-hPa level. The LLJ transported warm, moist air from the subtropical ocean, increased the moist static energy, and provided a favorable environment for the development of widespread precipitation. It is shown that the development of the LLJ is closely related to the developing lee cyclone to the east of the Tibetan Plateau. Our analysis reveals that the diagnosed secondary circulation associated with the jet-front system differs from those p...