Encyclopedia of World Climatology

2005 Edition
| Editors: John E. Oliver

Central America and the Caribbean, Climate of

  • Michael A. Taylor
  • Eric J. Alfaro
Reference work entry
DOI: https://doi.org/10.1007/1-4020-3266-8_37

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

  1. 1.
    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.Google Scholar
  2. 2.
    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.Google Scholar
  3. 3.
    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.Google Scholar
  4. 4.
    Amador, J., 1998. A climate feature of the tropical Americas: the trade wind easterly jet. Topicos Meteorologicos y Oceanograficos, 5(2): 91–102.Google Scholar
  5. 5.
    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.Google Scholar
  6. 6.
    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.Google Scholar
  7. 7.
    Cortez, M., 2000. Variaciones intraestacionales de la actividad convectiva en México y América Central. Atmósfera, 13(2): 95–108.Google Scholar
  8. 8.
    Fernandez, W., Chacon, R., and Melgarejo, J., 1996. On the rainfall distribution with altitude over Costa Rica. Revista Geofisica, 44: 57–72.Google Scholar
  9. 9.
    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.Google Scholar
  10. 10.
    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.Google Scholar
  11. 11.
    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.Google Scholar
  12. 12.
    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.Google Scholar
  13. 13.
    Magaña, V., Amador, J.A., and Medna, S., 1999. The midsummer drought over Mexico and Central America. Journal of Climate, 12: 1577–588.Google Scholar
  14. 14.
    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.Google Scholar
  15. 15.
    Rudloff, W., 1981. World-Climates, with Tables of Climatic Data and Practical Suggestions. Wissenschaftliche Verlagsgesellschaft mbH Stuttgart.Google Scholar
  16. 16.
    Schwerdtfeger, W. (ed.), 1976. Climates of Central and South America, vol. l12: World Survey of Climatology. New York: Elsevier.Google Scholar
  17. 17.
    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.Google Scholar
  18. 18.
    Wang, C., and Enfield, D., 2001. The tropical Western Hemisphere Warm Pool. Geophysical Research Letters, 28(8): 1635–1638.Google Scholar
  19. 19.
    Wang, C., and Enfield, D., 2003. A further study of the tropical Western Hemisphere Warm Pool. Journal of Climate, 16: 1476–1493.Google Scholar

Cross-references

  1. 1.
    Azores (Bermuda) HighGoogle Scholar
  2. 2.
    Humid ClimatesGoogle Scholar
  3. 3.
    Intertropical Convergence ZoneGoogle Scholar
  4. 4.
    Orographic PrecipitationGoogle Scholar
  5. 5.
    Trade Winds and the Trade Wind InversionGoogle Scholar
  6. 6.
    Tropical and Equatorial ClimatesGoogle Scholar
  7. 7.
    Tropical CyclonesGoogle Scholar

Copyright information

© Springer 2005

Authors and Affiliations

  • Michael A. Taylor
  • Eric J. Alfaro

There are no affiliations available