Dexterity of WRF and GFS models in contrast with vertical radiosonde profiles

The study focused on evaluating the dexterity of numerical prediction models using radiosonde data, which consists of collecting information from the atmospheric profile, which is fundamental for the initialization of the models. For this analysis, two models, GFS and WRF, were compared with radioso...

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Detalles Bibliográficos
Autores: Bezerra, Diego Pereira, Silva, Julio Tota da, Andrade, Antonio Marcos Delfino de, Silva, Arthur Wendell Duarte, Mendes, Ana Vitória Padilha, Mota, Beatriz Freire, Santana, Raoni Aquino Silva de, Andrade, Aurilene Barros dos Santos de, Neves, Theomar Trindade de Araujo Tiburtino, Fitzjarrald, David Roy
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2024
País:Brasil
Institución:Universidade Federal de Santa Maria (UFSM)
Repositorio:Revista Ciência e Natura (Online)
Idioma:portugués
OAI Identifier:oai:ojs.pkp.sfu.ca:article/87743
Acceso en línea:https://periodicos.ufsm.br/cienciaenatura/article/view/87743
Access Level:acceso abierto
Palabra clave:Radiossonda
WRF
Modelo
Radiosonde
Model
Descripción
Sumario:The study focused on evaluating the dexterity of numerical prediction models using radiosonde data, which consists of collecting information from the atmospheric profile, which is fundamental for the initialization of the models. For this analysis, two models, GFS and WRF, were compared with radiosonde observations. The observations used are from the radiosondes launched from the International Airport of Santarém/PA - Maestro Wilson Fonseca. Overall, both models underestimated air temperature measurements at low levels but aligned better at high altitudes. As for the zonal wind, the GFS overestimated at some levels, while the WRF had smaller discrepancies. The models face challenges in predicting air temperature, suggesting limitations in region-specific physics and boundary conditions. Both models had similar performance in the zonal wind forecast. The study highlights the importance of considering such discrepancies in weather forecasting and how these tools can be adjusted to improve their forecasts.