THE INFLUENCE OF CONTINENTAL WATER STORAGE ON THE ANNUAL WOBBLE OF POLAR MOTION, ESTIMATED BY INVERSE SOLUTION

dc.contributor.author	Jochmann H.
dc.date.accessioned	2020-12-29T10:10:03Z
dc.date.available	2020-12-29T10:10:03Z
dc.date.issued	1998
dc.identifier	https://elibrary.ru/item.asp?id=86775
dc.identifier.citation	Journal of Geodynamics, 1998, , 2, 147-160
dc.identifier.issn	0264-3707
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/21657
dc.description.abstract	Inverse solution is used to study the influence of continental water storage on polar motion. The difference between the total excitation of the annual wobble of polar motion and its atmospheric part is assumed to be caused by water storage. We assume this to be true and obtain two parameters of a relation between water storage and precipitation which take into account evapotranspiration, runoff, and the storage time of the water flowing in the basins.
dc.title	THE INFLUENCE OF CONTINENTAL WATER STORAGE ON THE ANNUAL WOBBLE OF POLAR MOTION, ESTIMATED BY INVERSE SOLUTION
dc.type	Статья

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