Preliminary experiments on the prediction of sea surface temperatura anomalies in the Gulf of Mexico

Main Article Content

J. Adem
E. E. Villanueva
V. M. Mendoza

Abstract

A thermodynamic model is used to predict the mean monthly sea surface temperature anomalies and their month-to-month changes in the Gulf of Mexico. The basic predicting equation of the Model is the thermal energy equation applied to the upper mixed layer of the ocean, which includes the horizontal transport of heat by seasonal ocean currents and by turbulent eddies, as well as the heating by short and long-wave radiation, evaporation and sensible heat. A comparative study is carried out on the relative importance for the prediction of the heating and transport terms. An objective verification of the predictions is presented for each season and for the whole period from March 1986 to February 1987, which shows skill in the signs correctly predicted of the sea surface temperature anomalies, as well as of their month-to-month changes, when the heating terms are only included in the predictions. However, the skill is increased when the horizontal transport of heat is also included.

Article Details

How to Cite
Adem, J., Villanueva, E. E., & Mendoza, V. M. (1994). Preliminary experiments on the prediction of sea surface temperatura anomalies in the Gulf of Mexico. Geofisica Internacional, 33(4), 511–521. https://doi.org/10.22201/igeof.00167169p.1994.33.4.585
Section
Article

References

ADEM, J., 1964a. On the physical basis for the numerical prediction of monthly and seasonal temperatures in the troposphere-ocean-continent system. Mon. Wea. Rev., 92, 91-103. DOI: https://doi.org/10.1175/1520-0493(1964)092<0091:OTPBFT>2.3.CO;2

ADEM, J., 1964b. On the normal thermal state of the troposphere ocean-continent system in the Northern Hemisphere. Geofísica Internacional, 4, 3-32. DOI: https://doi.org/10.22201/igeof.2954436xe.1964.4.1.1652

ADEM, J., 1967. Parameterization of atmospheric humidity using cloudiness and temperature. Mon. Wea. Rev., 95, 2, 83-88. DOI: https://doi.org/10.1175/1520-0493(1967)095<0083:POAHUC>2.3.CO;2

ADEM, J., 1970a. On the prediction of mean monthly ocean temperature. Tellus, 22, 4, 410-430. DOI: https://doi.org/10.1111/j.2153-3490.1970.tb00507.x

ADEM, J., 1970b. Incorporation of advection of heat by mean winds and by ocean currents in a thermodynamic model for long-range weather prediction. Mon. Wea. Rev., 98, 10,776-786. DOI: https://doi.org/10.1175/1520-0493(1970)098<0776:IOAOHB>2.3.CO;2

ADEM, J., 1975. Numerical-thermodynamical prediction of mean monthly ocean temperatures. Tellus., 27, 6, 541-551. DOI: https://doi.org/10.1111/j.2153-3490.1975.tb01709.x

ADEM, J., 1976. Predicción de Ia temperatura media mensual en Ia superficie de los oceanos utilizando un modelo termodinámico. ICCRA-II Symposium on Progress in Marine Research in the Caribbean and Adjacent Regions. FAO Fisheries Report No. 200. Supplement, 9-20.

ADEM, J., 1991. Review of the development and applications of the Adem thermodynamic climate model. Climate Dynamics. 5, 145-160. DOI: https://doi.org/10.1007/BF00251806

ADEM, J. and V. M. MENDOZA, 1987. Sensitivity experiments on ocean temperature predictions with a thermodynamic climate model. Geofísica Internacional, 26, 4, 525-543. DOI: https://doi.org/10.22201/igeof.00167169p.1987.26.4.1102

ADEM, J. and V. M. MENDOZA, 1988. Recent numerical thermodynamic experiments on sea surface temperature prediction. Geofísica Internacional, 27, 3, 309-325. DOI: https://doi.org/10.22201/igeof.00167169p.1988.27.3.1203

ADEM, J., V. M. MENDOZA, E. E. VILLANUEVA-URRUTIA and M. A. MONREAL-GOMEZ,1991. On the simulation of the sea surface temperature in the Gulf of Mexico using a thermodynamic model. Atmósfera. 4, 2, 87-99.

ADEM, J., E. E. VILLANUEVA and V. M. MENDOZA, 1993. A new method for estimating the seasonal cycle of the heat balance at the ocean surface, with application to the Gulf of Mexico. Geofísica Internacional, 32, 1, 21-34. DOI: https://doi.org/10.22201/igeof.00167169p.1993.32.1.1149

BUDYKO, M. I., 1974. Climate and life. International Geophysics Series, 18, Academic Press, Inc. 508 pp.

COLON, J. A., 1963. Seasonal variations in heat flux from the sea surface to the atmosphere over the Caribbean Sea. J. Geophys. Res., 68, 1421-1430. DOI: https://doi.org/10.1029/JZ068i005p01421

ELLIOT, B. A., 1982. Anticyclonic rings in the Gulf of Mexico. J. Phys. Oceanogr. 12, 1292-1309. DOI: https://doi.org/10.1175/1520-0485(1982)012<1292:ARITGO>2.0.CO;2

ETTER, P. C., 1983. Heat and freshwater budgets of the Gulf of Mexico. J. Phys. Oceanogr. 13, 2058-2069. DOI: https://doi.org/10.1175/1520-0485(1983)013<2058:HAFBOT>2.0.CO;2

HASTENRATH, S. L., 1968. Estimates of the latent and sensible heat flux for the Caribbean Sea and the Gulf of Mexico. Limnol. Oceanogr.,13, 322-331. DOI: https://doi.org/10.4319/lo.1968.13.2.0322

HASTENRATH, S. L. and P. J. LAMB, 1977. Climatic Atlas of the Tropical Atlantic and Eastern Pacific Oceans. University of Wisconsin Press. 54 pp.

HUANG, J. C. K., 1978. Numerical simulation studies of oceanic anomalies in the North Pacific Basin: I. The ocean model and the long-term mean state. J. Phys. Oceanogr., 8, 755-778. DOI: https://doi.org/10.1175/1520-0485(1978)008<0755:NSSOOA>2.0.CO;2

HURLBURT, H. E. and J. D. THOMPSON, 1980. A numerical study of Loop Current intrusions and eddy shedding. J. Phys. Oceanogr., 10, 1611-1651. DOI: https://doi.org/10.1175/1520-0485(1980)010<1611:ANSOLC>2.0.CO;2

ISEMER, H. and L. HASSE, 1987. The Bunket: Climate Atlas of the North Atlantic Ocean. Volume 2: Air-Sea Interactions. Springer-Verlag. 252 pp. DOI: https://doi.org/10.1007/978-3-642-72537-1_1

JACOBS, W. C., 1951. The energy exchange between the sea and the atmosphere and some of its consequences. Bull. Scripps Inst. of Oceanography. University of California, 6, 27-122.

LEWIS, J. K. and S. A. HSU, 1992. Mesoscale air-sea interactions to tropical and extratropical storms in the Gulf of Mexico. J. Geophys. Res., 97, C2, 2215-2228. DOI: https://doi.org/10.1029/91JC01447

MONREAL-GOMEZ, M. A., 1985. Modélisation du mode barotrope et du premier mode barocline dans le Golfe du Mexique. Ph. D. dissertation. University of Liège-, Belgium.

MONTGOMERY, R. B., 1939. Ein Versuch, den ver-tikalen und seitlichen Austausch in der Tiefe der Sprungschicht im äquatorialen Atlantischen Ozean zu bestimmen. Annalen der Hydrographie and Maritimen Meteorologie 67, 242-246.

PRICE, J. F., 1981. Upper ocean response to a hurricane. J. Phys. Ocean., 11, 153-175. DOI: https://doi.org/10.1175/1520-0485(1981)011<0153:UORTAH>2.0.CO;2

PRICE, J. F., 1983. Internal wave wake of a moving storm. Part I: Scales, energy budget and observations. J. Phys. Ocean., 13, 949-965. DOI: https://doi.org/10.1175/1520-0485(1983)013<0949:IWWOAM>2.0.CO;2

SECRETARIA DE MARINA, 1974. Atlas Oceanográfico del Golfo de Mexico y Mar Caribe. Secc. 1. Mareas y Corrientes. OSM.1000.

SEMTNER, A. J., Jr. and Y. MINTZ, 1977. Numerical simulation of the Gulf Stream and mid-ocean eddies. J. Phys. Oceanogr., 7, 208-230. DOI: https://doi.org/10.1175/1520-0485(1977)007<0208:NSOTGS>2.0.CO;2

Most read articles by the same author(s)