The enhanced nodal equilibrum ocean tide and polar motion
Contenido principal del artículo
Resumen
El análisis de los datos recientes del movimiento polar señalan la presencia de un componente cuya prioridad se corresponde con el movimiento lunar ascendente. Se ha procesado una investigación sobre la respuesta tidal del océano a las fuerzas impelentes durante largos periodos.
Los resultados de esta investigación señalan la posibilidad de excitación de un componente ondulatorio o de “cabeceo" con la amplitud y frecuencia coincidentes con los datos registrados. Se ha postulado, así, una función de facilitación dcl equilibrio, bajo la forma de una expansión en las armonías zonales y los coeficientes de dicha expansión parecen llenar las condiciones de componentes de movimiento polar de la magnitud requerida.
Detalles del artículo
Esta obra está bajo una licencia internacional Creative Commons Atribución-NoComercial-SinDerivadas 4.0.
Citas
AGNEW, D. C. and W. E. FARRELL, 1978. "Self-consistent equilibrium ocean tides," Geophysical Journal of the Royal Astronomical Society, 55, pp. 171-181. DOI: https://doi.org/10.1111/j.1365-246X.1978.tb04755.x
BALMINO, G., K. LAMBECK, and W. M. KAULA, 1973. "A Spherical Harmonic Analysis of the Earth's Topography," Journal of Geophysical Research, 78, pp. 478-481. DOI: https://doi.org/10.1029/JB078i002p00478
CAMPBELL, J., W. E. MOORE, and H. WOLF, 1964. "Minmax: A general Purpose Adaptive Iterator for Nonlinear Problems," Analytical Mechanics Associates, Inc.
CARTWRIGHT, D. E. and A. C. EDDEN, 1973. "Corrected Tables of Tidal Harmonics, "Geophysical Journal of the Royal Astronomical Society, 33, pp. 253-264. DOI: https://doi.org/10.1111/j.1365-246X.1973.tb03420.x
DAHLEN, F. A., 1976. "The Passive Influence of the Oceans Upon the Rotation of the Earth," Geophysical Journal of the Royal Astronomical Society, 46, pp. 363-406. DOI: https://doi.org/10.1111/j.1365-246X.1976.tb04163.x
DARWIN, G., 1886. "On the dynamical theory of the tides of long period," Proceedings of the Royal Society, A, 41, pp. 319-336.
DICKMAN, S. R., 1979. "Consequences of an Enhanced Pole Tide," Journal of Geophysical Research, 84, pp. 5447-5456. DOI: https://doi.org/10.1029/JB084iB10p05447
HAUBRICH, R., and W. MUNK, 1959. "The Pole Tide," Journal of Geophysical Research, 64, No. 12, pp. 2373-2388. DOI: https://doi.org/10.1029/JZ064i012p02373
HENDERSHOLT, M. C., 1972. ''The Effects of Solid Earth Deformation on Global Ocean Tides," Geophysical Journal of the Royal Astronomical Society, 29, pp. 389-402. DOI: https://doi.org/10.1111/j.1365-246X.1972.tb06167.x
HOSOYAMA, K, I. NAITO, and N. SATO, 1976. "Tidal Admittance of Pole Tide," Journal of Physics of the Earth, 24, pp. 51-62. DOI: https://doi.org/10.4294/jpe1952.24.51
LIOUVILLE, J., 1858. Liouville's Journal, Third Volume.
MARKOWITZ, W., 1979. "Independent Polar Motions, Optical and Doppler; Chandler Uncertainties," Report to IAU Commissions 19 and 31, Montreal, August 1979.
NAITO, I., 1977. "Secular Variation of Pole Tide," Journal of Physics of the Earth, 25, pp. 221-231. DOI: https://doi.org/10.4294/jpe1952.25.221
NAITO, I., 1979. "Effects of the Pole Tide on the Chandler Wobble," Journal of Physics of the Earth, 27, pp. 7-20. DOI: https://doi.org/10.4294/jpe1952.27.7
PROUDMAN, J., 1960. "The Condition that a Long-Period Tide shall follow the Equilibrium-Law," Geophysical Journal of the Royal Astronomical Society, 3, pp. 244-249. DOI: https://doi.org/10.1111/j.1365-246X.1960.tb00392.x
ROTENBERG, M., R. BEVINS, N. METROPOLIS, and J. K. WOOTEN, 1959. The 3-j and 6-j Symbols, MIT Technology Press, Cambridge, Mass.
WINCH, D. E. and R. W. JAMES, 1973. "Computations with Spherical Harmonics and Fourier Series in Geomagnetism," in Methods in Computational Physics, Vol. 13, pp. 93-132, Academic Press. DOI: https://doi.org/10.1016/B978-0-12-460813-9.50009-6
WINSCH, C., 1967. "The Long-Period Tides, "Reviews of Geophysics, Vol. 5, No. 4, pp. 447-475. DOI: https://doi.org/10.1029/RG005i004p00447
