The influence of a zonal pressure field at the core-mantle boundary upon the Earth's shape and rotational eigenperiods.

Details The influence of a zonal pressure field at the core-mantle boundary upon the Earth's shape and rotational eigenperiods. The influence of a zonal pressure field at the core-mantle boundary upon the Earth's shape and rotational eigenperiods.

Mar 1989

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1989crasb.308..879l&link_type=abstract

Comptes Rendus de l'Academie des Sciences, Sér. II, Tome 308, No. 9, p. 879 - 882

Computer Science

Earth: Figure, Earth Rotation: Chandler Wobble

Scientific paper

A zonal degree 2 pressure field of about 3×107Pa acting at the core-mantle boundary is shown to be able to explain simultaneously the discrepancies between the observed and hydrostatic values for the geometrical and dynamical flattenings as well as the discrepancies between observed and classical Chandlerian and nearly diurnal rotational eigenperiods.

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