Zobrazeno 1 - 10
of 40
pro vyhledávání: '"M. G. Rochester"'
Publikováno v:
Geophysical Journal International. 209:1455-1461
Publikováno v:
Geophysical Journal International. 198:1848-1877
Autor:
M. G. Rochester, David Crossley
Publikováno v:
Geophysical Journal International. 198:1890-1905
Publikováno v:
Journal of Geophysical Research: Solid Earth. 123:9998
Autor:
M. G. Rochester
Publikováno v:
Journal of Elasticity. 98:111-114
The proof that being irrotational/solenoidal is sufficient for a displacement field in a homogeneous isotropic elastic solid to be propagated as a P/S wave is utterly familiar. Because a proof of the necessity of these conditions seems not to be give
Autor:
David Crossley, M. G. Rochester
Publikováno v:
Geophysical Journal International. 176:40-62
SUMMARY The two low-frequency wobble modes of the Earth are the Chandler wobble (CW) and the inner core wobble (ICW). The CW period is about 400 d for an ocean-free model, and the ICW period has previously been estimated to be about 6.6 yr. The latte
Autor:
M. G. Rochester, David Crossley
Publikováno v:
Geophysical Journal International. 125:830-840
SUMMARY This paper extends our earlier examinations of the utility of various approximations for treating the dynamics of the Earth’s liquid core on time-scales of the order of lo4 to lo8 s. We discuss the effects of representing the response of th
Publikováno v:
Journal of Geophysical Research. 116
Nutation amplitudes are computed in a displacement field approach that incorporates the influence of a prescribed magnetic field inside the Earth's core. The existence of relative nutational motions between the liquid core and its surrounding solid p
Publikováno v:
Geophysical Research Letters. 19:1679-1682
The recent claim by Smylie [1992] to have detected the Slichter modes of the Earth's inner core rests on what appears to be a remarkable agreement between theory and observation. However the theoretical eigenperiods which are used by Smylie conflict
Autor:
M. G. Rochester, David Crossley
Publikováno v:
Geophysical Journal International. 108:502-506
SUMMARY Scaling arguments have been used to justify the subseismic approximation (SSA) for analysing long-period oscillations of the Earth's liquid core. This approximation neglects the contribution of flow pressure to elastic compression relative to