Computation of tendencies and vertical motion with a two‐parameter model of the atmosphere
- 1 January 1954
- journal article
- Published by Wiley in Quarterly Journal of the Royal Meteorological Society
- Vol. 80 (343) , 16-25
- https://doi.org/10.1002/qj.49708034304
Abstract
No abstract availableKeywords
This publication has 14 references indexed in Scilit:
- NUMERICAL INTEGRATION OF THE QUASI-GEOSTROPHIC EQUATIONS FOR BAROTROPIC AND SIMPLE BAROCLINIC FLOWSJournal of Meteorology, 1953
- On the theory of large‐scale disturbances in a two‐dimensional baroclinic equivalent of the atmosphereQuarterly Journal of the Royal Meteorological Society, 1953
- Note on Weather Computing and the so-called 2½-dimensional ModelTellus, 1952
- SYMPOSIUM ON NUMERICAL FORECASTING: Simplified Dynamic Models of the Atmosphere, designed for the Purpose of Numerical Weather PredictionTellus, 1952
- Note on Weather Computing and the so-called 2½-dimensional ModelTellus A: Dynamic Meteorology and Oceanography, 1952
- A SIMPLE THREE-DIMENSIONAL MODEL FOR THE STUDY OF LARGE-SCALE EXTRATROPICAL FLOW PATTERNSJournal of Meteorology, 1951
- Numerical Tendency Computations from the Barotropic Vorticity EquationTellus, 1951
- Numerical Tendency Computations from the Barotropic Vorticity EquationTellus A: Dynamic Meteorology and Oceanography, 1951
- Numerical Integration of the Barotropic Vorticity EquationTellus, 1950
- Numerical Integration of the Barotropic Vorticity EquationTellus A: Dynamic Meteorology and Oceanography, 1950