Impact of Radar Data Assimilation on the Numerical Simulation of a Severe Storm in Croatia

A severe thunderstorm hit the northwestern part of Croatia in the late afternoon and evening of 24 June 2008. This severe event is used as a test case for the Advanced Regional Prediction System (ARPS) high resolution numerical prediction model and for exploring the impact of assimilating convention...

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Main Authors: Antonio Stanesic, Keith A. Brewster
Format: Article
Language:English
Published: Borntraeger 2016-02-01
Series:Meteorologische Zeitschrift
Subjects:
Online Access:http://dx.doi.org/10.1127/metz/2015/0574
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spelling doaj-e58a4abe1d02438cbbc11af88b50a7ea2020-11-24T23:24:03ZengBorntraegerMeteorologische Zeitschrift0941-29482016-02-01251375310.1127/metz/2015/057484894Impact of Radar Data Assimilation on the Numerical Simulation of a Severe Storm in CroatiaAntonio StanesicKeith A. BrewsterA severe thunderstorm hit the northwestern part of Croatia in the late afternoon and evening of 24 June 2008. This severe event is used as a test case for the Advanced Regional Prediction System (ARPS) high resolution numerical prediction model and for exploring the impact of assimilating conventional and radar data. Radar radial velocity data were assimilated using three-dimensional variational analysis (3DVAR). Radar reflectivity data were used through a cloud analysis procedure where hydrometeors and cloud fields are defined, and adjustments to the in-cloud temperature and moisture fields are made. Results show that without data assimilation, the models were not able to represent the development of the storm nor the proper environment for it. Assimilation of surface observations in the mesoscale outer model provided spatial distribution of convection ingredients that established a proper environment for storm initiation and propagation. Without that, the inner storm-scale model, even with radar data assimilation, is unable to simulate storm development. Using the outer model with assimilation of surface data in combination with an inner model including assimilation of radar data provided the best simulation of storm initiation and development.http://dx.doi.org/10.1127/metz/2015/0574radar data assimilationsevere stormnumerical weather predictionARPS
collection DOAJ
language English
format Article
sources DOAJ
author Antonio Stanesic
Keith A. Brewster
spellingShingle Antonio Stanesic
Keith A. Brewster
Impact of Radar Data Assimilation on the Numerical Simulation of a Severe Storm in Croatia
Meteorologische Zeitschrift
radar data assimilation
severe storm
numerical weather prediction
ARPS
author_facet Antonio Stanesic
Keith A. Brewster
author_sort Antonio Stanesic
title Impact of Radar Data Assimilation on the Numerical Simulation of a Severe Storm in Croatia
title_short Impact of Radar Data Assimilation on the Numerical Simulation of a Severe Storm in Croatia
title_full Impact of Radar Data Assimilation on the Numerical Simulation of a Severe Storm in Croatia
title_fullStr Impact of Radar Data Assimilation on the Numerical Simulation of a Severe Storm in Croatia
title_full_unstemmed Impact of Radar Data Assimilation on the Numerical Simulation of a Severe Storm in Croatia
title_sort impact of radar data assimilation on the numerical simulation of a severe storm in croatia
publisher Borntraeger
series Meteorologische Zeitschrift
issn 0941-2948
publishDate 2016-02-01
description A severe thunderstorm hit the northwestern part of Croatia in the late afternoon and evening of 24 June 2008. This severe event is used as a test case for the Advanced Regional Prediction System (ARPS) high resolution numerical prediction model and for exploring the impact of assimilating conventional and radar data. Radar radial velocity data were assimilated using three-dimensional variational analysis (3DVAR). Radar reflectivity data were used through a cloud analysis procedure where hydrometeors and cloud fields are defined, and adjustments to the in-cloud temperature and moisture fields are made. Results show that without data assimilation, the models were not able to represent the development of the storm nor the proper environment for it. Assimilation of surface observations in the mesoscale outer model provided spatial distribution of convection ingredients that established a proper environment for storm initiation and propagation. Without that, the inner storm-scale model, even with radar data assimilation, is unable to simulate storm development. Using the outer model with assimilation of surface data in combination with an inner model including assimilation of radar data provided the best simulation of storm initiation and development.
topic radar data assimilation
severe storm
numerical weather prediction
ARPS
url http://dx.doi.org/10.1127/metz/2015/0574
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