Numerical prediction of the sea surface temperature in the Pacific and Atlantic oceans
Adem, Julián; Mendoza, Víctor Manuel; Villanueva, Elba E.
Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM
dor_id: 4132745
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351.#.#.b: Geofísica Internacional
351.#.#.a: Artículos
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856.4.0.u: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/730/1181
100.1.#.a: Adem, Julián; Mendoza, Víctor Manuel; Villanueva, Elba E.
524.#.#.a: Adem, Julián, et al. (1995). Numerical prediction of the sea surface temperature in the Pacific and Atlantic oceans. Geofísica Internacional; Vol. 34 Núm. 2: Abril 1, 1995; 149-160. Recuperado de https://repositorio.unam.mx/contenidos/4132745
245.1.0.a: Numerical prediction of the sea surface temperature in the Pacific and Atlantic oceans
502.#.#.c: Universidad Nacional Autónoma de México
561.1.#.a: Instituto de Geofísica, UNAM
264.#.0.c: 1995
264.#.1.c: 1995-04-01
653.#.#.a: predicción mensual; temperatura superficial oceánica; modelo climático; Monthly prediction; sea surface temperature; climatic model
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884.#.#.k: http://revistagi.geofisica.unam.mx/index.php/RGI/article/view/730
001.#.#.#: 063.oai:revistagi.geofisica.unam.mx:article/730
041.#.7.h: spa
520.3.#.a: The conservation of thermal energy equation applied to the upper mixed layer of the oceans is used for the prediction of the sea surface temperature anomalies and their month - to - month changes in the Northern Hemisphere. The equation includes horizontal transport of heat by ocean currents and by horizontal turbulent mixing as well as heating by short and long wave radiation, evaporation and sensible heat. As input we use the sea surface temperature, the 850 mb temperature and the atmospheric surface pressure in the previous month as well as their corresponding normal values. A comparative study is carried out on the relative importance of the heating and transport terms and of the change in the grid distance. An objetive verification of the prediction is presented for the Pacific and Atlantic oceans, for the 48-month period from June 1980 to May 1984. Some degree of skill in the predictions is due to the heating terms. The best skill is obtained when the horizontal transport of heat by turbulent mixing and surface ocean currents is also included. The skill is substantially increased in the semi-prediction for which the wind drift ocean currents and the heating are computed with the atmospheric surface pressure and the 850 mb-temperature for the current month, instead of the previous month.
773.1.#.t: Geofísica Internacional; Vol. 34 Núm. 2: Abril 1, 1995; 149-160
773.1.#.o: http://revistagi.geofisica.unam.mx/index.php/RGI
022.#.#.a: ISSN-L: 2954-436X; ISSN impreso: 0016-7169
310.#.#.a: Trimestral
300.#.#.a: Páginas: 149-160
264.#.1.b: Instituto de Geofísica, UNAM
doi: https://doi.org/10.22201/igeof.00167169p.1995.34.2.730
handle: 00f42df56afa59c0
harvesting_date: 2023-06-20 16:00:00.0
856.#.0.q: application/pdf
file_creation_date: 2022-07-07 10:49:46.0
file_modification_date: 2022-07-14 18:06:09.0
file_creator: J. Adem
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245.1.0.b: Numerical prediction of the sea surface temperature in the Pacific and Atlantic oceans
last_modified: 2023-06-20 16:00:00
license_url: https://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.es
license_type: by-nc-sa
Adem, Julián; Mendoza, Víctor Manuel; Villanueva, Elba E.
Instituto de Geofísica, UNAM, publicado en Geofísica Internacional, y cosechado de Revistas UNAM
Adem, Julián, et al. (1995). Numerical prediction of the sea surface temperature in the Pacific and Atlantic oceans. Geofísica Internacional; Vol. 34 Núm. 2: Abril 1, 1995; 149-160. Recuperado de https://repositorio.unam.mx/contenidos/4132745