Artículo

Why did numerical weather forecasting systems fail to predict the Hurricane Otis’s development?

Guillermo Montiel, Juan Carlos; Martínez López, Benjamín; Ochoa Moya, Carlos Abraham; Quintanar, Ignacio Arturo; Cabos Narváez, William David

Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM, publicado en Atmósfera y cosechado de y cosechado de Revistas UNAM

Licencia de uso

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Procedencia del contenido

Entidad o dependencia
Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM
Revista
Repositorio
Contacto
Revistas UNAM. Dirección General de Publicaciones y Fomento Editorial, UNAM en revistas@unam.mx

Cita

Guillermo Montiel, Juan Carlos, et al. (2024). Why did numerical weather forecasting systems fail to predict the Hurricane Otis’s development?. Atmósfera; Vol. 38, 2024; 829-862. Recuperado de https://repositorio.unam.mx/contenidos/4158785

Descripción del recurso

Autor(es)
Guillermo Montiel, Juan Carlos; Martínez López, Benjamín; Ochoa Moya, Carlos Abraham; Quintanar, Ignacio Arturo; Cabos Narváez, William David
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Why did numerical weather forecasting systems fail to predict the Hurricane Otis’s development?
Fecha
2024-09-12
Resumen
Hurricane Otis (HO) occurred in the eastern tropical Pacific (ETP), intensifying rapidly and unexpectedly, making landfall near Acapulco at 06:25 UTC on October 25, 2023 as a category five hurricane. Official and unofficial national weather forecasts (NWF) failed to predict HO’s development, trajectory, and intensification. To analyze the reasons for the failure of the NWF, we conducted two experiments using the Weather Research and Forecasting (WRF) model, with Global Forecast System (GFS) and fifth-generation ECMWF atmospheric reanalysis (ERA5) data as initial condition (IC). Our results showed that some fields in the GFS data, such as relative humidity, convective available potential energy, and even sea surface temperature, were more favorable for the development and intensification of the disturbance compared to ERA5. However, the three-dimensional structure of the wind field in the ETP in GFS did not contribute to the initial development of HO. Additionally, we explored the WRF’s sensitivity to different model configurations to simulate the trajectory and intensity of the hurricane using a coupled ocean-atmosphere system composed of WRF and a three-dimensional upper-ocean circulation model based on Price-Weller-Pinkel. Our numerical experiments involve modifications in the IC, cumulus parameterizations (CP), roughness coefficients, spatial resolutions, different time steps, and an idealized coupled model. The sensitivity test reveals the significance of the CP scheme, where the Kain-Fritsch was the only one that helped simulate the HO properly, altogether with increased spatial resolution. Furthermore, ocean-atmosphere coupling improves the prediction of the landfall time and location of the HO. However, no experiment captured the intensity or rapid intensification of HO.
Tema
Hurricane Otis development; Initial condition; ERA5 reanalysis; cumulus parameterization scheme; coupled ocean-atmosphere system; WRF-PWP
Idioma
eng
ISSN
ISSN electrónico: 2395-8812; ISSN impreso: 0187-6236

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