Evidencias de la oscilación del tiempo Madden y Julian en el Caribe colombiano
DOI:
https://doi.org/10.26640/22159045.119Keywords:
Colombia Caribbean, Santa Marta, IDEAM, INVEMAR, meteorological and oceanographic dataAbstract
This paper presents the analysis of meteorological and oceanographic data series from some IDEAM (Instituto de Hidrología, Meteorología y Estudios Ambientales) and INVEMAR (Instituto de Investigaciones Marinas) stations along the Colombian Caribbean northeast coast. Using the spectral time series analysis the climatic behavior in a complicated region dueto the influence of the Santa Marta mountain (Sierra Nevada de Santa Marta) that have 4500 mts high close to the coast is described. As a result 8 different oscillations (90, 20, 14.7, 11, 8, 6 and 4 days period) and evidence of the intraseasonal Madden Julian Oscillation (30-60) in the data sets were found.Downloads
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References
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LAU, K.M., Subseasonal Oscillations. bimodal climate state luid the el Niño Southern Oscillation. Coupled Ocean-Atmosphere Model. J. Nihoul_ Ed.. Elscvier. 1985a.
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LAU, K.M., and P.H., CHANG.. Short tenn climate variability and atmospheric teleconection as inferred fi-om outgoing 1011gWaVC radiation. J. Atinas. Sci., 1983a. 40, 2735-2750.
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_________ and ____________ Description of Global-Scale Circulation Cells in the Tropics widí a 40-50 Day Period. J. Atmos. Sci, 29, 1972. p. 1109- 1123.
_________ and ____________ Observation of the 40-50 day tropical oscillation a review. Mon. Wea. RCV.. 1994. 122.814-837.
MADDEN R.A. Seasonal variations of the 40-50 day oscillation in the tropics. Journal of the Atmospheric Sciences, 43(24). 1987, p.3138-3158.
MURAKAMI T. and Nakazawa T.. Tropical 45 day osciIlations during the 1979 Northem Hemisphere sum men J. Atmos. Sci._ 42. 1985, p. 1 107 - 1122.
MARTINEZ, R.. Estudio del comportamiento de ondas lineales baron-ópicas en la atmósfera tropical y el litoral ecuatoriano-colombiano en un periodo determinado. Cartagena de Indias, 1996. Trabajo de grado (Oceanografía Física). Escuela naval de Cadetes Almirante Padilla. Facultad de Oceanografía.
MÜLLER K., Interrelaciones entre salinidad y temperatura en la Bahía de Santa Marta. An. lns. Invanar Punta de Betín. 11. 1979, p. 219- 226.
PARKER. DE., Equatorial Kelvin waves al 100 milibars. Quart. J. Roy. Meteor. Soc.. l973.99 116-129.
SALZWEDEL 11. and K. Müller. A. Summary of Meteorological and Hidrological data from the Bay of Santa Marta, Colom bian Caribbean. ApInstinv.Mar. Punta de Betín. 13. 1983. p. 67-83.
SCHNETTER. R. Untersuchungen zum Stzmdortklima im trockengebeit von Santa Marta. Kolumbien. Mitt. Inst. Colombo Aleman Invest. Cient. 1970. 4: 45-75.
FRANCO, A.S. Analise Espectral, Teoría e practica Instituto de Pesquisas Tecnológicas do Estado de Sao Paulo (IPT) 1984.
GILL, A. E., Some simple solutions for heat- induced tropical circulation. Quart. J. R. Met. Soc.. 106. 1980,p. 447-462.
HENDON. H. H. and M. L. Salln. The life cycle of (the Madden-Julian oscillation. J. Atmos. Sci., 51, 1994, p. 2225-2237.
HERRMANN R. Las Causas de la Sequía Climática en la Región Costanera de Santa Marta Colombia, Rey, de la Academia Colombiana de Ciencias Exactas Físicas \ Naturales. Vol. 13, 52. 1970. p. 479-485.
____________. Deutungsverstich der Entstehung dcr -Brisa, cines fühnwindartigen Fallwindes der norclwestlichen Sierra Nevada de Santa Marta_ Kolumbien.Mitt. Inst. Colombo-Alemán Invest. Cient. 1970. Vo14. 83 -95
KNUTSON, T.R. K.M. WEICKMANN and J.E. KUTZBACH: Global scale intraseasonal oscillation of outgoing longwave radialioli and 250 mb zonal wind during northern hemisphere summer. Mon. Wea. Rev., 1986.114. 605-523.
LAU, K.M., Subseasonal Oscillations. bimodal climate state luid the el Niño Southern Oscillation. Coupled Ocean-Atmosphere Model. J. Nihoul_ Ed.. Elscvier. 1985a.
LAU, K.M., Elements of a stochastic dynamical theory of the long-term variability of el Niño Southern Oscillation.. J. Atmos. Sci.. 1985b. 42, 1557-1558
LAU, K.M., and P.H., CHANG.. Short tenn climate variability and atmospheric teleconection as inferred fi-om outgoing 1011gWaVC radiation. J. Atinas. Sci., 1983a. 40, 2735-2750.
LAU, K. M.. and L. PENG, 1987: Origin of low- frequency (intraseasonal) oscillations in the tropical atmosphere. Part I: basic theory. J. Atmos. Sci.. (44), 950-972.
MADDEN R.A. and P.R. Julian, Detection of a 40- 50 day oscillation in the zonal wind in the tropical Pacific. J. Atmos. Sci, 28, 1971, p. 702-708.
_________ and ____________ Description of Global-Scale Circulation Cells in the Tropics widí a 40-50 Day Period. J. Atmos. Sci, 29, 1972. p. 1109- 1123.
_________ and ____________ Observation of the 40-50 day tropical oscillation a review. Mon. Wea. RCV.. 1994. 122.814-837.
MADDEN R.A. Seasonal variations of the 40-50 day oscillation in the tropics. Journal of the Atmospheric Sciences, 43(24). 1987, p.3138-3158.
MURAKAMI T. and Nakazawa T.. Tropical 45 day osciIlations during the 1979 Northem Hemisphere sum men J. Atmos. Sci._ 42. 1985, p. 1 107 - 1122.
MARTINEZ, R.. Estudio del comportamiento de ondas lineales baron-ópicas en la atmósfera tropical y el litoral ecuatoriano-colombiano en un periodo determinado. Cartagena de Indias, 1996. Trabajo de grado (Oceanografía Física). Escuela naval de Cadetes Almirante Padilla. Facultad de Oceanografía.
MÜLLER K., Interrelaciones entre salinidad y temperatura en la Bahía de Santa Marta. An. lns. Invanar Punta de Betín. 11. 1979, p. 219- 226.
PARKER. DE., Equatorial Kelvin waves al 100 milibars. Quart. J. Roy. Meteor. Soc.. l973.99 116-129.
SALZWEDEL 11. and K. Müller. A. Summary of Meteorological and Hidrological data from the Bay of Santa Marta, Colom bian Caribbean. ApInstinv.Mar. Punta de Betín. 13. 1983. p. 67-83.
SCHNETTER. R. Untersuchungen zum Stzmdortklima im trockengebeit von Santa Marta. Kolumbien. Mitt. Inst. Colombo Aleman Invest. Cient. 1970. 4: 45-75.
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2003-12-01
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How to Cite
Evidencias de la oscilación del tiempo Madden y Julian en el Caribe colombiano. (2003). CIOH Scientific Bulletin, 21, 101–113. https://doi.org/10.26640/22159045.119
