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650.#.4.x: Físico Matemáticas y Ciencias de la Tierra

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336.#.#.a: Artículo

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856.4.0.u: https://www.revistascca.unam.mx/atm/index.php/atm/article/view/8438/7908

100.1.#.a: Birol Kara, A.; Elsner, James B.

524.#.#.a: Birol Kara, A., et al. (1999). Characteristics of the atmospheric boundary layer for coastal and inland locations around the Gulf of Mexico. Atmósfera; Vol. 12 No. 1, 1999. Recuperado de https://repositorio.unam.mx/contenidos/4122421

245.1.0.a: Characteristics of the atmospheric boundary layer for coastal and inland locations around the Gulf of Mexico

502.#.#.c: Universidad Nacional Autónoma de México

561.1.#.a: Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM

264.#.0.c: 1999

264.#.1.c: 2009-10-05

506.1.#.a: La titularidad de los derechos patrimoniales de esta obra pertenece a las instituciones editoras. Su uso se rige por una licencia Creative Commons BY-NC 4.0 Internacional, https://creativecommons.org/licenses/by-nc/4.0/legalcode.es, para un uso diferente consultar al responsable jurídico del repositorio por medio del correo electrónico editora@atmosfera.unam.mx

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041.#.7.h: eng

520.3.#.a: This paper examines aspects of the atmospheric boundary layer (ABL) for several U. S. coastal and inland locations around the Gulf of Mexico. Simulations are performed using the Oregon State University (OSU) planetary boundary layer model under a Gulf of Mexico return-flow event. For the model analyses, the ABL heights are obtained using soil moisture values from the Eta model. The ABL heights obtained from these 24-hr forecasts are then compared with other standard formulations. It is shown poor forecasts of the ABL height in the model under very stable conditions can be prevented by using an interpolation formula. Results confirm that friction velocity in the boundary layer along the Gulf coast is small. A strong relationship between friction velocity and Monin-Obukhov length at coastal locations is likely due to surface fluxes with relatively unimportant heat flux. At coastal locations of Florida and Texas, mechanical turbulence causes large temperature structure parameter at the surface since wind speed is usually calm in the model forecasts.

773.1.#.t: Atmósfera; Vol. 12 No. 1 (1999)

773.1.#.o: https://www.revistascca.unam.mx/atm/index.php/atm/index

046.#.#.j: 2021-10-20 00:00:00.000000

022.#.#.a: ISSN electrónico: 2395-8812; ISSN impreso: 0187-6236

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264.#.1.b: Instituto de Ciencias de la Atmósfera y Cambio Climático, UNAM

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harvesting_date: 2023-06-20 16:00:00.0

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245.1.0.b: Characteristics of the atmospheric boundary layer for coastal and inland locations around the Gulf of México

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Artículo

Characteristics of the atmospheric boundary layer for coastal and inland locations around the Gulf of Mexico

Birol Kara, A.; Elsner, James B.

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

Licencia de uso

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

Birol Kara, A., et al. (1999). Characteristics of the atmospheric boundary layer for coastal and inland locations around the Gulf of Mexico. Atmósfera; Vol. 12 No. 1, 1999. Recuperado de https://repositorio.unam.mx/contenidos/4122421

Descripción del recurso

Autor(es)
Birol Kara, A.; Elsner, James B.
Tipo
Artículo de Investigación
Área del conocimiento
Físico Matemáticas y Ciencias de la Tierra
Título
Characteristics of the atmospheric boundary layer for coastal and inland locations around the Gulf of Mexico
Fecha
2009-10-05
Resumen
This paper examines aspects of the atmospheric boundary layer (ABL) for several U. S. coastal and inland locations around the Gulf of Mexico. Simulations are performed using the Oregon State University (OSU) planetary boundary layer model under a Gulf of Mexico return-flow event. For the model analyses, the ABL heights are obtained using soil moisture values from the Eta model. The ABL heights obtained from these 24-hr forecasts are then compared with other standard formulations. It is shown poor forecasts of the ABL height in the model under very stable conditions can be prevented by using an interpolation formula. Results confirm that friction velocity in the boundary layer along the Gulf coast is small. A strong relationship between friction velocity and Monin-Obukhov length at coastal locations is likely due to surface fluxes with relatively unimportant heat flux. At coastal locations of Florida and Texas, mechanical turbulence causes large temperature structure parameter at the surface since wind speed is usually calm in the model forecasts.
Idioma
eng
ISSN
ISSN electrónico: 2395-8812; ISSN impreso: 0187-6236

Enlaces