Central America and the Caribbean span the deep tropics and subtropics. Because of the tropical maritime location temperature changes throughout the region are generally small, and rainfall is by far the most important meteorological element. In general the climate of the region is controlled by the migration of synoptic features, and the mean climate strongly reflects the annual cycle of these features.
The most dominant synoptic influence is the subtropical high of the north Atlantic. Subsidence associated with the spreading of the subtropical high from the north Atlantic to the north American landmass dominates during boreal winter, as do the strong easterly trades found on its equatorward flank. Coupled with a strong trade inversion, a cold ocean and reduced atmospheric humidity, the region is generally at its driest during the winter. With the onset of boreal spring, however, the subtropical high moves offshore and trade wind intensity decreases, with convergence characterizing...
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Bibliography
Alfaro, E.J., 2000a. Response of air surface temperatures over Central America to oceanic climate variability indices. Topicos Meteorologicos y Oceanograficos, 7(2): 63–72.
Alfaro, E.J., 2000b. Some characteristics of the annual precipitation cycle in Central America and their relationships with its surrounding tropical oceans. Topicos Meteorologicos y Oceanograficos, 7(2): 99–115.
Alvarado, L., 1999. Alteración de la atmósfera libre sobre Costa Rica durante eventos de El Niño. Degree thesis in Meteorology, School of Physics, University of Costa Rica, San José, Costa Rica.
Amador, J., 1998. A climate feature of the tropical Americas: the trade wind easterly jet. Topicos Meteorologicos y Oceanograficos, 5(2): 91–102.
Banichevich, A., and Lizano, O., 1998. Interconexión a nivel ciclónicoatmosférico entre el Caribe y el PacÍfico centroamericanos. Revista de Biologia Tropical, 46(Suppl. 5): 9–22.
Chacon, R., and Fernandez, W., 1985. Temporal and spatial rainfall variability in the mountain region of the Reventazon river basin, Costa Rica. J. Climate, 5: 175–188.
Cortez, M., 2000. Variaciones intraestacionales de la actividad convectiva en México y América Central. Atmósfera, 13(2): 95–108.
Fernandez, W., Chacon, R., and Melgarejo, J., 1996. On the rainfall distribution with altitude over Costa Rica. Revista Geofisica, 44: 57–72.
Giannini, A., Kushnir, Y., and Cane, M.A., 2000. Interannual variability of Caribbean rainfall, ENSO and the Atlantic Ocean. Journal of Climate, 13: 297–311.
Gray, W.M., 1984. Atlantic seasonal hurricane frequency: Part I: El Niño and 30-mb quasi-bienniel oscillation influences. Monthly Weather Review, 112: 1649–1668.
Goldenberg, S.B., Landsea, C.W., Mestas-Nuñez, A.M., and Gray, W.M., 2001. The recent increase in Atlantic hurricane activity: causes and implications. Science, 293: 474–479.
Inoue, M., Handoh, I.C., and Bigg, G.R., 2002. Bimodal distribution of tropical cyclogenesis in the Caribbean: characteristics and environmental factors. Journal of Climate, 15: 2897–2905.
Magaña, V., Amador, J.A., and Medna, S., 1999. The midsummer drought over Mexico and Central America. Journal of Climate, 12: 1577–588.
Martis, A., Van Oldenborgh, G.J., and Burgers, G., 2002. Predictign rainfall in the Dutch Caribbean — more than El Niño? International Journal of Climatology, 22: 1219–1234.
Rudloff, W., 1981. World-Climates, with Tables of Climatic Data and Practical Suggestions. Wissenschaftliche Verlagsgesellschaft mbH Stuttgart.
Schwerdtfeger, W. (ed.), 1976. Climates of Central and South America, vol. l12: World Survey of Climatology. New York: Elsevier.
Taylor, M.A., Enfield D.B., and Anthony Chen, A., 2002. The influence of the tropical Atlantic vs. the tropical Pacific on Caribbean rainfall. Journal of Geophysical Research, 107(C9) 3127, doi:10.1029/2001JC001097.
Wang, C., and Enfield, D., 2001. The tropical Western Hemisphere Warm Pool. Geophysical Research Letters, 28(8): 1635–1638.
Wang, C., and Enfield, D., 2003. A further study of the tropical Western Hemisphere Warm Pool. Journal of Climate, 16: 1476–1493.
Cross-references
Azores (Bermuda) High
Humid Climates
Intertropical Convergence Zone
Orographic Precipitation
Trade Winds and the Trade Wind Inversion
Tropical and Equatorial Climates
Tropical Cyclones
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Taylor, M.A., Alfaro, E.J. (2005). Central America and the Caribbean, Climate of. In: Oliver, J.E. (eds) Encyclopedia of World Climatology. Encyclopedia of Earth Sciences Series. Springer, Dordrecht . https://doi.org/10.1007/1-4020-3266-8_37
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