A comparison of simulated precipitation by hybrid isentropic-sigma and sigma models

Simulations of dry and moist baroclinic development from 10- and 22-layer hybrid isentropic-sigma coordinate models are compared with those from 11-, 27-, and 35-layer sigma coordinate models. The ability of the models to transport water vapor and simulate equivalent potential temperature is examine...

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Veröffentlicht in:Monthly weather review 1993-07, Vol.121 (7), p.2088-2114
Hauptverfasser: Johnson, Donald R., Zapotocny, Tom H., Reames, Fred M., Wolf, Bart J., Pierce, R. B.
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container_end_page 2114
container_issue 7
container_start_page 2088
container_title Monthly weather review
container_volume 121
creator Johnson, Donald R.
Zapotocny, Tom H.
Reames, Fred M.
Wolf, Bart J.
Pierce, R. B.
description Simulations of dry and moist baroclinic development from 10- and 22-layer hybrid isentropic-sigma coordinate models are compared with those from 11-, 27-, and 35-layer sigma coordinate models. The ability of the models to transport water vapor and simulate equivalent potential temperature is examined. Predictions of the timing, location, and amount of precipitation are compared. Several analytical distributions of water vapor are specified initially. It is shown that when the relative humidity is vertically uniform through a substantial extent of the atmosphere, all the models produce very similar precipitation distributions. However, when water vapor is confined to relatively shallow layers, the ability of the sigma coordinate models to simulate the timing, location, and amount of precipitation is severely compromised.
doi_str_mv 10.1175/1520-0493(1993)121<2088:ACOSPB>2.0.CO;2
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source AMS Journals (Meteorology); NASA Technical Reports Server; Alma/SFX Local Collection; EZB Electronic Journals Library
subjects Earth, ocean, space
Exact sciences and technology
External geophysics
Meteorology
Meteorology And Climatology
Weather analysis and prediction
title A comparison of simulated precipitation by hybrid isentropic-sigma and sigma models
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