Possible source of nontidal fluctuations of the rate of the earth's diurnal rotation with T greater than or equal to 20 years and less than 100 years

Details Possible source of nontidal fluctuations of the rate of the earth's diurnal rotation with T greater than or equal to 20 years and less than 100 years Possible source of nontidal fluctuations of the rate of the earth's diurnal rotation with T greater than or equal to 20 years and less than 100 years

Oct 1985

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1985ge%26ae..25..833r&link_type=abstract

Geomagnetizm i Aeronomiia (ISSN 0016-7940), vol. 25, Sept.-Oct. 1985, p. 833-836. In Russian.

Physics

Angular Velocity, Earth Rotation, Long Term Effects, Secular Variations, Earth Core, Error Analysis, Solar Terrestrial Interactions

Scientific paper

A method is proposed for determining the error in calculating the nontidal-fluctuation curve delta-P for the change in the length of day during 1664-1974. It is shown that delta-P curves with T of approximately 70 and 22 years arose simultaneously after the middle of the 19th century. It is suggested that delta-P(70) and delta-P(22) are determined by different types of effects of solar activity on the earth's liquid core.

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