Concurrent Sensitivities of an Idealized Deep Convective Storm to Parameterization of Microphysics, Horizontal Grid Resolution, and Environmental Static StabilitySource: Monthly Weather Review:;2015:;volume( 143 ):;issue: 006::page 2082DOI: 10.1175/MWR-D-14-00271.1Publisher: American Meteorological Society
Abstract: his study investigated the sensitivity of idealized deep convective storm simulations to microphysics parameterization, horizontal grid spacing (?x), and environmental static stability. Three different bulk microphysics schemes in the Weather Research and Forecasting Model were tested for ?x between 0.125 and 2 km and three different environmental soundings, modified by altering static stability above 5 km. Horizontally and temporally averaged condensation and surface precipitation rates and convective updraft mass flux were sensitive to microphysics scheme and ?x for all environmental soundings. Microphysical sensitivities were similar for 0.125 < ?x < 1 km, but they varied for different soundings. Sensitivities of these quantities to ?x were less robust and varied with microphysics scheme. Other statistical convective characteristics, such as the mean updraft width and strength, exhibited similar sensitivities to ?x for all of the microphysics schemes. Microphysical sensitivities were primarily attributed to interactions between microphysics, cold pools, and dynamics that affected the spatial coverage of convective updrafts and hence the horizontally averaged convective mass flux, condensation rate, and surface precipitation. However, these linkages were less clear for the lowest convective available potential energy (CAPE) sounding, and in this case other mechanisms compensated to give a similar spatial coverage of convective updrafts even in simulations without a cold pool. For higher CAPE, there was considerable production of rimed ice from all of the microphysics schemes and its assumed characteristics, especially the fall speed, were important in explaining sensitivity via microphysical impacts on the cold pool. These results highlight the need for continued improvement in representing the production of rimed ice and its characteristics in microphysics schemes.
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contributor author | Morrison, Hugh | |
contributor author | Morales, Annareli | |
contributor author | Villanueva-Birriel, Cecille | |
date accessioned | 2017-06-09T17:32:33Z | |
date available | 2017-06-09T17:32:33Z | |
date copyright | 2015/06/01 | |
date issued | 2015 | |
identifier issn | 0027-0644 | |
identifier other | ams-86976.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4230593 | |
description abstract | his study investigated the sensitivity of idealized deep convective storm simulations to microphysics parameterization, horizontal grid spacing (?x), and environmental static stability. Three different bulk microphysics schemes in the Weather Research and Forecasting Model were tested for ?x between 0.125 and 2 km and three different environmental soundings, modified by altering static stability above 5 km. Horizontally and temporally averaged condensation and surface precipitation rates and convective updraft mass flux were sensitive to microphysics scheme and ?x for all environmental soundings. Microphysical sensitivities were similar for 0.125 < ?x < 1 km, but they varied for different soundings. Sensitivities of these quantities to ?x were less robust and varied with microphysics scheme. Other statistical convective characteristics, such as the mean updraft width and strength, exhibited similar sensitivities to ?x for all of the microphysics schemes. Microphysical sensitivities were primarily attributed to interactions between microphysics, cold pools, and dynamics that affected the spatial coverage of convective updrafts and hence the horizontally averaged convective mass flux, condensation rate, and surface precipitation. However, these linkages were less clear for the lowest convective available potential energy (CAPE) sounding, and in this case other mechanisms compensated to give a similar spatial coverage of convective updrafts even in simulations without a cold pool. For higher CAPE, there was considerable production of rimed ice from all of the microphysics schemes and its assumed characteristics, especially the fall speed, were important in explaining sensitivity via microphysical impacts on the cold pool. These results highlight the need for continued improvement in representing the production of rimed ice and its characteristics in microphysics schemes. | |
publisher | American Meteorological Society | |
title | Concurrent Sensitivities of an Idealized Deep Convective Storm to Parameterization of Microphysics, Horizontal Grid Resolution, and Environmental Static Stability | |
type | Journal Paper | |
journal volume | 143 | |
journal issue | 6 | |
journal title | Monthly Weather Review | |
identifier doi | 10.1175/MWR-D-14-00271.1 | |
journal fristpage | 2082 | |
journal lastpage | 2104 | |
tree | Monthly Weather Review:;2015:;volume( 143 ):;issue: 006 | |
contenttype | Fulltext |