Evaluation of the WRF-ARW model during an extreme rainfall event: Subtropical storm Guará

This study simulates an unusual extreme rainfall event that occurred in Salvador city, Bahia, Brazil, on December 9, 2017, which was named subtropical storm Guará and had precipitation of approximately 24 mm within less than 1 h. Numerical simulations were conducted using the Weather Research and Fo...

ver descrição completa

Detalhes bibliográficos
Autores: Lago Kitagawa, Yasmin Kaore, Sperandio Nascimento, Erick Giovani, Perini Souza, Noéle Bissoli, Junior Zucatelli, Pedro, Kumar, Prashant, de Almeida Albuquerque, Taciana Toledo, Romero de Moraes, Marcelo, Martins Moreira, Davidson
Tipo de documento: artigo
Estado:Versão publicada
Data de publicação:2022
País:México
Recursos:UNIVERSIDAD NACIONAL AUTÓNOMA DE MÉXICO
Repositório:Atmósfera
Idioma:inglês
OAI Identifier:oai:ojs.pkp.sfu.ca:article/52977
Acesso em linha:https://www.revistascca.unam.mx/atm/index.php/atm/article/view/52977
Access Level:Acceso aberto
Palavra-chave:atmospheric modeling
WRF model
extreme rainfall
northeastern Brazil
physical parameterization
Descrição
Resumo:This study simulates an unusual extreme rainfall event that occurred in Salvador city, Bahia, Brazil, on December 9, 2017, which was named subtropical storm Guará and had precipitation of approximately 24 mm within less than 1 h. Numerical simulations were conducted using the Weather Research and Forecasting (WRF) model over three domains with horizontal resolutions of 9, 3, and 1 km. Different combinations of seven microphysics, three cumulus, and three planetary boundary layer schemes were evaluated based on their ability to simulate the hourly precipitation during this rainfall event. Statistical indices (MB = –0.69; RMSE = 4.11; MAGE = 1.74; r = 0.55; IOA = 0.66; FAC2 = 0.58) and time series plots showed that the most suitable configurations for this weather event were the Mellor-Yamada-Janjić, Grell-Freitas, and Lin formulations for the planetary boundary layer, cumulus, and microphysics schemes, respectively. The results were compared with the data measured at meteorological stations located in Salvador city. The WRF model simulated well the arrival and occurrence of this extreme weather event in a tropical and coastal region, considering that the region already has intense convective characteristics and is constantly influenced by sea breezes, which could interfere in the model results and compromise the performance of the simulations.