The Instability of the Gravity-inertia wave and its Relation to Low-level Jet and Heavy Rainfall
- 1 January 1982
- journal article
- Published by Meteorological Society of Japan in Journal of the Meteorological Society of Japan. Ser. II
- Vol. 60 (5) , 1041-1057
- https://doi.org/10.2151/jmsj1965.60.5_1041
Abstract
No abstract availableThis publication has 11 references indexed in Scilit:
- The Physical Mechanism of Baroclinic Instability and Its Downstream Propagation Based on the Splitting MethodMonthly Weather Review, 1981
- Frequent Occurrence of Heavy Rainfall along the North Side to the Low-Level Jet Stream in the Baiu SeasonPapers in Meteorology and Geophysics, 1973
- Atmospheric Frontogenesis Models: Mathematical Formulation and SolutionJournal of the Atmospheric Sciences, 1972
- Characteristic Features of “Baiu” Front Associated with Heavy RainfallJournal of the Meteorological Society of Japan. Ser. II, 1971
- On the Mesoscale and Medium-scale Structure of a Cold Front and the Relevant Vertical CirculationJournal of the Meteorological Society of Japan. Ser. II, 1971
- On the Applicability of the Geostrophic Approximation to Upper-Level Frontal-Scale MotionsJournal of the Atmospheric Sciences, 1970
- Severe Convective StormsPublished by Elsevier ,1967
- The vertical circulation at meteorological fronts and its relation to frontogenesisProceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences, 1956
- FRONTOGENESIS AND FRONTOLYSIS AS A THREE-DIMENSIONAL PROCESSJournal of Meteorology, 1954
- CONFLUENCE THEORY OF THE HIGH TROPOSPHERIC JET STREAMJournal of Meteorology, 1949