Abstract
A case study of a developing cyclone is used to show that the three-dimensional distribution of height change during development can be strongly sensitive to temperature changes which occur in the lower stratosphere in association with an evolving tropopause undulation. Quantitative analysis of the storm with a geopotential height tendency equation indicates that a synergistic process developed between the stratosphere and troposphere, whereby the vertical motion pattern maintained and intensified the upper-level temperature anomalies while the subsequent upper-level temperature advection led to an enhanced vertical circulation. Using the results of this diagnostic study, a conceptual model is constructed. -from Authors
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CITATION STYLE
Hirschberg, P. A., & Fritsch, J. M. (1991). Tropopause undulations and the development of extratropical cyclones. Part II: diagnostic analysis and conceptual model. Monthly Weather Review, 119(2), 518–550. https://doi.org/10.1175/1520-0493(1991)119<0518:TUATDO>2.0.CO;2
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