Assessment of physical schemes for WRF model in convection-permitting mode over southern Iberian Peninsula

Fuente: arXiv
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Autori principali: Solano-Farías, Feliciano, Ojeda, Matilde García-Valdecasas, Donaire-Montaño, David, Rosa-Cánovas, Juan José, Castro-Diez, Yolanda, Esteban-Parra, Maria Jesús, Gámiz-Fortis, Sonia Raquel
Natura: Preprint
Pubblicazione: 2024
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author Solano-Farías, Feliciano
Ojeda, Matilde García-Valdecasas
Donaire-Montaño, David
Rosa-Cánovas, Juan José
Castro-Diez, Yolanda
Esteban-Parra, Maria Jesús
Gámiz-Fortis, Sonia Raquel
author_facet Solano-Farías, Feliciano
Ojeda, Matilde García-Valdecasas
Donaire-Montaño, David
Rosa-Cánovas, Juan José
Castro-Diez, Yolanda
Esteban-Parra, Maria Jesús
Gámiz-Fortis, Sonia Raquel
contents Convection-permitting models (CPMs) enable the representation of meteorological variables at horizontal high resolution spatial scales (higher than 4 km), where convection plays a significant role. Physical schemes need to be evaluated considering factors in the studied region such as orography and climate variability. This study investigates the sensitivity of the WRF model as CPM to the use of different physics schemes on Andalusia, a complex orography region in southern Iberian Peninsula (IP). A set of 1-year WRF simulations was completed based on two one-way nested domains: the parent domain (d01) spanning the entire IP with 5 km spatial resolution and the nested domain (d02) for the region of Andalusia at 1 km of spatial resolution. 12 physic schemes were examined from combinations of microphysics (MP) schemes including THOMPSON, WRF single moment 6-class (WSM6), and WRF single moment 7-class (WSM7), and different options for the convection in d01, the Grell 3D (G3), Grell-Freitas (GF), Kain-Fritsch (KF), and deactivated cumulus parameterization (OFF). The simulated precipitation and 2-m temperature for the year 2018, a very wet year, were compared with observational datasets to determine the optimal WRF configuration, including point-to-point and station-point comparisons at different time aggregations. In general, greater differences were shown when comparing the results of convection schemes in d01. Simulations completed with GF or OFF presented better performance compared to the reference datasets. Concerning the MP, although THOMPSON showed a better fit in high mountain areas, it generally presents a worse agreement with the reference datasets. In terms of temperature, the results were very similar and, therefore, the selection of the best configuration was based mainly on the precipitation results with the WSM7-GF scheme being suitable for Andalusia region.
format Preprint
id arxiv_https___arxiv_org_abs_2404_19327
institution arXiv
publishDate 2024
record_format arxiv
spellingShingle Assessment of physical schemes for WRF model in convection-permitting mode over southern Iberian Peninsula
Solano-Farías, Feliciano
Ojeda, Matilde García-Valdecasas
Donaire-Montaño, David
Rosa-Cánovas, Juan José
Castro-Diez, Yolanda
Esteban-Parra, Maria Jesús
Gámiz-Fortis, Sonia Raquel
Atmospheric and Oceanic Physics
Applied Physics
Convection-permitting models (CPMs) enable the representation of meteorological variables at horizontal high resolution spatial scales (higher than 4 km), where convection plays a significant role. Physical schemes need to be evaluated considering factors in the studied region such as orography and climate variability. This study investigates the sensitivity of the WRF model as CPM to the use of different physics schemes on Andalusia, a complex orography region in southern Iberian Peninsula (IP). A set of 1-year WRF simulations was completed based on two one-way nested domains: the parent domain (d01) spanning the entire IP with 5 km spatial resolution and the nested domain (d02) for the region of Andalusia at 1 km of spatial resolution. 12 physic schemes were examined from combinations of microphysics (MP) schemes including THOMPSON, WRF single moment 6-class (WSM6), and WRF single moment 7-class (WSM7), and different options for the convection in d01, the Grell 3D (G3), Grell-Freitas (GF), Kain-Fritsch (KF), and deactivated cumulus parameterization (OFF). The simulated precipitation and 2-m temperature for the year 2018, a very wet year, were compared with observational datasets to determine the optimal WRF configuration, including point-to-point and station-point comparisons at different time aggregations. In general, greater differences were shown when comparing the results of convection schemes in d01. Simulations completed with GF or OFF presented better performance compared to the reference datasets. Concerning the MP, although THOMPSON showed a better fit in high mountain areas, it generally presents a worse agreement with the reference datasets. In terms of temperature, the results were very similar and, therefore, the selection of the best configuration was based mainly on the precipitation results with the WSM7-GF scheme being suitable for Andalusia region.
title Assessment of physical schemes for WRF model in convection-permitting mode over southern Iberian Peninsula
topic Atmospheric and Oceanic Physics
Applied Physics
url https://arxiv.org/abs/2404.19327