INVESTIGADORES
DRAGANI walter Cesar
artículos
Título:
Sea level oscillations in coastal waters of the Buenos Aires Province, Argentina
Autor/es:
DRAGANI, WALTER; MAZIO, CARLOS; NUÑEZ, MARIO
Revista:
CONTINENTAL SHELF RESEARCH
Editorial:
Elsevier
Referencias:
Año: 2002 vol. 22 p. 779 - 790
ISSN:
0278-4343
Resumen:
Sea level oscillations, with periods ranging from a few minutes to almost 2 h, have been observed at various tide stations located on the coast of Buenos Aires.Simultaneous records of sea level elevation measured in Mar de Aj! o, Pinamar and Mar del Plata during 1982 have been spectrally analyzed.Significant spectral energy has been detected between 0.85 and 4.69 cycles per hour (cph) and the most energetic peaks have frequencies between 1.17 and 1.49 cph. Spectra, coherence, and phase difference have been analyzed for the most energetic event of the year.During that event, the most intensive spectral peak is at 1.17 cph for Mar de Aj!o and Pinamar, and at 1.49 cph for Mar del Plata. Simultaneous total energy peaks at Mar de Aj! o, Pinamar and Mar del Plata, and the coherence function estimated between Mar de Aj!o and Pinamar suggests that sea level oscillations could be a regional phenomenon.The analyzed data suggest that sea level oscillations could be forced by atmospheric gravity waves associated with frontal passages.! o, Pinamar and Mar del Plata during 1982 have been spectrally analyzed.Significant spectral energy has been detected between 0.85 and 4.69 cycles per hour (cph) and the most energetic peaks have frequencies between 1.17 and 1.49 cph. Spectra, coherence, and phase difference have been analyzed for the most energetic event of the year.During that event, the most intensive spectral peak is at 1.17 cph for Mar de Aj!o and Pinamar, and at 1.49 cph for Mar del Plata. Simultaneous total energy peaks at Mar de Aj! o, Pinamar and Mar del Plata, and the coherence function estimated between Mar de Aj!o and Pinamar suggests that sea level oscillations could be a regional phenomenon.The analyzed data suggest that sea level oscillations could be forced by atmospheric gravity waves associated with frontal passages.
