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Warianty tytułu
Języki publikacji
Abstrakty
The origins of the continuous free oscillations of the whole earth have been attributed to coupling between the solid earth and atmosphere primarily through the fundamental spheroidal mode 0S29 oscillation of ~3.7 mHz. The origins of these interference patterns have been attributed to an excitation source just above the Earth’s surface. However, comparable surface oscillations have been measured in the Sun’s photosphere. The cube root of the product of the gravitational constant, the spectral radiance of the sun, and the square of the frequency produced an acceleration value that was identical to the measured amplitude of the free Earth oscillations (~0.4∙10-11 m∙s-2). The quantitative convergence suggests these narrow-band accelerations may emerge within the Sun-Earth system as it moves through galactic space. Keywords: Earth’s free oscillations; gravitation; solar Rossby waves; nanoGals; spheroidal modes; solar spectral radiance.
Rocznik
Tom
Strony
11--14
Opis fizyczny
Bibliogr. 5 poz., wz.
Twórcy
autor
- Laurentian University, 935 Ramsey Lake Road, Sudbury, Ontario P3E 2C6, Canada
Bibliografia
- [1] J. Rhie, B. Romanowicz, Nature 431 (2004) 552-555.
- [2] K. Nishida, N. Kobayashi, Y. Fukao, Science 287 (2000) 2244-2246.
- [3] M. A. Persinger, International Journal of Geosciences 3 (2012) 192-194.
- [4] J. R. Kuhn, J. D. Armstrong, R. I. Bush, P. Scherrer, Nature 405 (2000) 544-547.
- [5] B. T. Dotta, K. S. Saroka, M. A. Persinger, Neuroscience Letters 513 (2012) 151-154.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-484fa9d9-8d8f-4426-aa59-8924715320ba