A diagnostic study of the low-level jet during TAMEX IOP 5

Abstract

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 favourable 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. The transverse secondary circulation across the front is characterized by a thermally direct circulation across the baroclinic zone with warm air rising within the southwest monsoon flow and cold air sinking in the postfrontal northeasterlies. A very weak thermally indirect circulation was observed to the south. -from Authors