Mesoscale spiral vortex embedded within a Lake Michigan snow squall band: high resolution satellite observations and numerical model simulations

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Abstract

An exceptional and often neglected source of data for mesoscale cloud studies is the ultrahigh resolution multispectral data produced by Landsat satellites. On 19 October 1972, a clearly defined spiral vortex was noted in a Landsat-1 image near the southern end of Lake Michigan during an exceptionally early cold air outbreak over a still very warm lake. In a numerical simulation using a 3-D Eulerian hydrostatic primitive equation mesoscale model, with an initially uniform wind field, a definite analog to the observed vortex was generated. This suggests that intense surface heating can be a principal cause in the development of a low-level mesoscale vortex. -from Authors

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APA

Pease, S. R., Lyons, W. A., Keen, C. S., & Hjelmfelt, M. (1988). Mesoscale spiral vortex embedded within a Lake Michigan snow squall band: high resolution satellite observations and numerical model simulations. Monthly Weather Review, 116(6), 1374–1380. https://doi.org/10.1175/1520-0493(1988)116<1374:MSVEWA>2.0.CO;2

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