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 |
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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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B.</creatorcontrib><title>A comparison of simulated precipitation by hybrid isentropic-sigma and sigma models</title><title>Monthly weather review</title><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.</description><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Meteorology</subject><subject>Meteorology And Climatology</subject><subject>Weather analysis and prediction</subject><issn>0027-0644</issn><issn>1520-0493</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1993</creationdate><recordtype>article</recordtype><sourceid>CYI</sourceid><recordid>eNqFkU2LFDEQhoMoOK7-Aw99ENFDzybpfHRUhLFZV2FhhNVzqE7SGukvUz2H-femt5e97ikFeXireB9CLhndM6blJZOcllSY6h0zpnrPOPvEaV1_ODTH2x9fPvM93TfHj_wJ2T2QT8mOUq5LqoR4Tl4g_qWUKiX4jtweCjcNM6SI01hMXYFxOPWwBF_MKbg4xwWWmL_ac_Hn3Kboi4hhXNI0R1di_D1AAaMvtmmYfOjxJXnWQY_h1f17QX59vfrZfCtvjtffm8NN6QSXS6mBtq7zpmPaeUlBcgZctIoLGoLWoVbee90CyFZLI7hQSulQKeXy7dD66oK83XLnNP07BVzsENGFvocxTCe0XBpd1Uo-CrKa52qFfhxURtSm4hm83kCXJsQUOjunOEA6W0btqsmu5du1fLtqslmTXTXZTZPlltrmaNekN_crAR30XYLRRXyIE9rkw1jGXm_YCAg29493uVmjqLWq_gMJSZ6n</recordid><startdate>19930701</startdate><enddate>19930701</enddate><creator>Johnson, Donald R.</creator><creator>Zapotocny, Tom H.</creator><creator>Reames, Fred M.</creator><creator>Wolf, Bart J.</creator><creator>Pierce, R. 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B.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>A comparison of simulated precipitation by hybrid isentropic-sigma and sigma models</atitle><jtitle>Monthly weather review</jtitle><date>1993-07-01</date><risdate>1993</risdate><volume>121</volume><issue>7</issue><spage>2088</spage><epage>2114</epage><pages>2088-2114</pages><issn>0027-0644</issn><eissn>1520-0493</eissn><coden>MWREAB</coden><abstract>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.</abstract><cop>Legacy CDMS</cop><pub>American Meteorological Society</pub><doi>10.1175/1520-0493(1993)121<2088:ACOSPB>2.0.CO;2</doi><tpages>27</tpages><oa>free_for_read</oa></addata></record> |
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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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