Abstract
The analysis of Conditional Instability of the Second Kind (CISK) for a resting atmosphere leads to a maximum growth rate at zero width of the rain area. However, if the process takes place in a uniform current moving relative to the ground with a velocity 27, and the width of the rain area is 2a, an Ekman boundary layer cannot be established in the rain area when 2a
Cite
CITATION STYLE
APA
Charney, J. (1973). Movable CISK. Journal of the Atmospheric Sciences, 30(1), 50–52. https://doi.org/10.1175/1520-0469(1973)030<0050:mc>2.0.co;2
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