Abstract
A linear steady-state primitive equation model has been developed for the computation of stationary atmospheric waves that are forced by anomalies in surface conditions. The response of the model indicates that a heating in the tropics can have a substantial influence on the middle and high latitudes, provided that part of the heating is in the westerlies.-from Authors
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CITATION STYLE
Opsteegh, J. D., & Van Den Dool, H. M. (1980). Seasonal differences in the stationary response of a linearized primitive equation model: prospects for long-range weather forecasting? Journal of the Atmospheric Sciences, 37(10), 2169–2185. https://doi.org/10.1175/1520-0469(1980)037<2169:SDITSR>2.0.CO;2
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