Impact of the assimilation of lightning data on the precipitation forecast at different forecast ranges

This study investigates the impact of the assimilation of total lightning data on the precipitation forecast of a numerical weather prediction (NWP) model. The impact of the lightning data assimilation, which uses water vapour substitution, is investigated at different forecast time ranges, name...

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Main Authors: S. Federico, M. Petracca, G. Panegrossi, C. Transerici, S. Dietrich
Format: Article
Language:English
Published: Copernicus Publications 2017-06-01
Series:Advances in Science and Research
Online Access:https://www.adv-sci-res.net/14/187/2017/asr-14-187-2017.pdf
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author S. Federico
M. Petracca
G. Panegrossi
C. Transerici
S. Dietrich
author_facet S. Federico
M. Petracca
G. Panegrossi
C. Transerici
S. Dietrich
author_sort S. Federico
collection DOAJ
description This study investigates the impact of the assimilation of total lightning data on the precipitation forecast of a numerical weather prediction (NWP) model. The impact of the lightning data assimilation, which uses water vapour substitution, is investigated at different forecast time ranges, namely 3, 6, 12, and 24 h, to determine how long and to what extent the assimilation affects the precipitation forecast of long lasting rainfall events (&gt; 24 h). The methodology developed in a previous study is slightly modified here, and is applied to twenty case studies occurred over Italy by a mesoscale model run at convection-permitting horizontal resolution (4 km). The performance is quantified by dichotomous statistical scores computed using a dense raingauge network over Italy. <br><br> Results show the important impact of the lightning assimilation on the precipitation forecast, especially for the 3 and 6 h forecast. The probability of detection (POD), for example, increases by 10 % for the 3 h forecast using the assimilation of lightning data compared to the simulation without lightning assimilation for all precipitation thresholds considered. The Equitable Threat Score (ETS) is also improved by the lightning assimilation, especially for thresholds below 40 mm day<sup>−1</sup>. <br><br> Results show that the forecast time range is very important because the performance decreases steadily and substantially with the forecast time. The POD, for example, is improved by 1–2 % for the 24 h forecast using lightning data assimilation compared to 10 % of the 3 h forecast. The impact of the false alarms on the model performance is also evidenced by this study.
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spelling doaj.art-4576cab3d2284c9b96ce1d617c3d1cd72022-12-21T23:56:12ZengCopernicus PublicationsAdvances in Science and Research1992-06281992-06362017-06-011418719410.5194/asr-14-187-2017Impact of the assimilation of lightning data on the precipitation forecast at different forecast rangesS. Federico0M. Petracca1G. Panegrossi2C. Transerici3S. Dietrich4ISAC-CNR, UOS of Rome, via del Fosso del Cavaliere 100, 00133-Rome, ItalyISAC-CNR, UOS of Rome, via del Fosso del Cavaliere 100, 00133-Rome, ItalyISAC-CNR, UOS of Rome, via del Fosso del Cavaliere 100, 00133-Rome, ItalyISAC-CNR, UOS of Rome, via del Fosso del Cavaliere 100, 00133-Rome, ItalyISAC-CNR, UOS of Rome, via del Fosso del Cavaliere 100, 00133-Rome, ItalyThis study investigates the impact of the assimilation of total lightning data on the precipitation forecast of a numerical weather prediction (NWP) model. The impact of the lightning data assimilation, which uses water vapour substitution, is investigated at different forecast time ranges, namely 3, 6, 12, and 24 h, to determine how long and to what extent the assimilation affects the precipitation forecast of long lasting rainfall events (&gt; 24 h). The methodology developed in a previous study is slightly modified here, and is applied to twenty case studies occurred over Italy by a mesoscale model run at convection-permitting horizontal resolution (4 km). The performance is quantified by dichotomous statistical scores computed using a dense raingauge network over Italy. <br><br> Results show the important impact of the lightning assimilation on the precipitation forecast, especially for the 3 and 6 h forecast. The probability of detection (POD), for example, increases by 10 % for the 3 h forecast using the assimilation of lightning data compared to the simulation without lightning assimilation for all precipitation thresholds considered. The Equitable Threat Score (ETS) is also improved by the lightning assimilation, especially for thresholds below 40 mm day<sup>−1</sup>. <br><br> Results show that the forecast time range is very important because the performance decreases steadily and substantially with the forecast time. The POD, for example, is improved by 1–2 % for the 24 h forecast using lightning data assimilation compared to 10 % of the 3 h forecast. The impact of the false alarms on the model performance is also evidenced by this study.https://www.adv-sci-res.net/14/187/2017/asr-14-187-2017.pdf
spellingShingle S. Federico
M. Petracca
G. Panegrossi
C. Transerici
S. Dietrich
Impact of the assimilation of lightning data on the precipitation forecast at different forecast ranges
Advances in Science and Research
title Impact of the assimilation of lightning data on the precipitation forecast at different forecast ranges
title_full Impact of the assimilation of lightning data on the precipitation forecast at different forecast ranges
title_fullStr Impact of the assimilation of lightning data on the precipitation forecast at different forecast ranges
title_full_unstemmed Impact of the assimilation of lightning data on the precipitation forecast at different forecast ranges
title_short Impact of the assimilation of lightning data on the precipitation forecast at different forecast ranges
title_sort impact of the assimilation of lightning data on the precipitation forecast at different forecast ranges
url https://www.adv-sci-res.net/14/187/2017/asr-14-187-2017.pdf
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AT gpanegrossi impactoftheassimilationoflightningdataontheprecipitationforecastatdifferentforecastranges
AT ctranserici impactoftheassimilationoflightningdataontheprecipitationforecastatdifferentforecastranges
AT sdietrich impactoftheassimilationoflightningdataontheprecipitationforecastatdifferentforecastranges