The Instability of the Gravity-inertia wave and its Relation to Low-level Jet and Heavy Rainfall

Author:

Chen Qiushi1

Affiliation:

1. Department of Atmospheric Sciences, University of California

Publisher

Meteorological Society of Japan

Subject

Atmospheric Science

Reference19 articles.

1. Akiyama, T., 1973: Frequent occurrence of heavy rainfall along the north side of the low-level jet stream in the Bain season. Paper Met. Geophys., 24, 379-388.

2. Chen, C. S., 1963: On the formation and destruction of the thermal wind in a simple baroclinic atmosphere, (1) and (2). Acta. Met. Sinica., 33, 51-63, 153-162.

3. Chen, C. S., 1964: The convective instability of the inertia wave and physical analysis of the formation of the typhoon in the early stage. Acta. Met. Sinica., 34, 433-442.

4. Chen, C. S., (Q. Chen), 1981: The physical mechanism of baroclinic instability and its downstream propagation based on the splitting method. Mon. Wea. Rev., 109, 2464-2473.

5. Ding, Yi-Hui, et al., 1980: On the physical conditions of occurrence of heavy rainfall and severe convective weather. Preprints, 8th conf. on Weather forecasting and analysis, 371-377.

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