A new nutation model of a non-rigid earth with ocean and atmosphere

SUMMARY By integrating the truncated complex scalar gravitational motion equations for an anelastic, rotating, slightly elliptical earth, the complex frequency-dependent earth transfer functions are computed directly. Unlike the conventional method, the contributions of both oceanic load and current...

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Published inGeophysical journal international Vol. 146; no. 1; pp. 126 - 133
Main Authors Huang, Cheng-li, Jin, Wen-jing, Liao, Xing-hao
Format Journal Article
LanguageEnglish
Published Oxford, UK Blackwell Publishing Ltd 01.07.2001
Blackwell Science Ltd
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Abstract SUMMARY By integrating the truncated complex scalar gravitational motion equations for an anelastic, rotating, slightly elliptical earth, the complex frequency-dependent earth transfer functions are computed directly. Unlike the conventional method, the contributions of both oceanic load and current to all nutation periods, as well as the atmospheric contributions to prograde annual, retrograde annual and retrograde semi-annual nutation, are included in the integration via outer surface boundary conditions, all of which are expanded to second order in ellipticity. A modified ellipticity profile of second-order accuracy for the non-hydrostatic earth is obtained from Clairaut's equation and the PREM earth model by adjusting both the ellipticity of the core-mantle boundary and the global dynamical ellipticity to modern observations. The effects of different earth models, anelastic models and ocean models are computed and compared. Finally, a complete new nutation series of 343 periods, including in-phase and out-of-phase parts of longitude and obliquity terms, for a more realistic earth is obtained and compared with other available nutation series and observations.
AbstractList By integrating the truncated complex scalar gravitational motion equations for an anelastic, rotating, slightly elliptical earth, the complex frequency-dependent earth transfer functions are computed directly. Unlike the conventional method, the contributions of both oceanic load and current to all nutation periods, as well as the atmospheric contributions to prograde annual, retrograde annual, and retrograde semi-annual nutation, are included in the integration via outer surface boundary conditions, all of which are expanded to second order in ellipticity. A modified ellipticity profile of second-order accuracy for the nonhydrostatic earth is obtained from Clairaut's equation and the PREM earth model by adjusting both the ellipticity of the core mantle boundary and the global dynamical ellipticity to modern observations. The effects of different earth models, anelastic models, and ocean models are computed and compared. Finally, a complete new nutation series of 343 periods, including in-phase and out-of-phase parts of longitude and obliquity terms, for a more realistic earth is obtained and compared with other available nutation series and observations. (Author)
SUMMARY By integrating the truncated complex scalar gravitational motion equations for an anelastic, rotating, slightly elliptical earth, the complex frequency-dependent earth transfer functions are computed directly. Unlike the conventional method, the contributions of both oceanic load and current to all nutation periods, as well as the atmospheric contributions to prograde annual, retrograde annual and retrograde semi-annual nutation, are included in the integration via outer surface boundary conditions, all of which are expanded to second order in ellipticity. A modified ellipticity profile of second-order accuracy for the non-hydrostatic earth is obtained from Clairaut's equation and the PREM earth model by adjusting both the ellipticity of the core-mantle boundary and the global dynamical ellipticity to modern observations. The effects of different earth models, anelastic models and ocean models are computed and compared. Finally, a complete new nutation series of 343 periods, including in-phase and out-of-phase parts of longitude and obliquity terms, for a more realistic earth is obtained and compared with other available nutation series and observations.
SUMMARY By integrating the truncated complex scalar gravitational motion equations for an anelastic, rotating, slightly elliptical earth, the complex frequency‐dependent earth transfer functions are computed directly. Unlike the conventional method, the contributions of both oceanic load and current to all nutation periods, as well as the atmospheric contributions to prograde annual, retrograde annual and retrograde semi‐annual nutation, are included in the integration via outer surface boundary conditions, all of which are expanded to second order in ellipticity. A modified ellipticity profile of second‐order accuracy for the non‐hydrostatic earth is obtained from Clairaut's equation and the PREM earth model by adjusting both the ellipticity of the core–mantle boundary and the global dynamical ellipticity to modern observations. The effects of different earth models, anelastic models and ocean models are computed and compared. Finally, a complete new nutation series of 343 periods, including in‐phase and out‐of‐phase parts of longitude and obliquity terms, for a more realistic earth is obtained and compared with other available nutation series and observations.
Author Liao, Xing-hao
Huang, Cheng-li
Jin, Wen-jing
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  givenname: Wen-jing
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  fullname: Jin, Wen-jing
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  fullname: Liao, Xing-hao
  email: clhuang@center.shao.ac.cn
  organization: 1 Shanghai Astronomical Observatory, NAO, CAS, 80 Nandan Road, Shanghai 200 030, China. E-mail: clhuang@center.shao.ac.cn
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Snippet SUMMARY By integrating the truncated complex scalar gravitational motion equations for an anelastic, rotating, slightly elliptical earth, the complex...
SUMMARY By integrating the truncated complex scalar gravitational motion equations for an anelastic, rotating, slightly elliptical earth, the complex...
By integrating the truncated complex scalar gravitational motion equations for an anelastic, rotating, slightly elliptical earth, the complex...
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SubjectTerms atmospheres
earth rotation
nutation
oceans
Title A new nutation model of a non-rigid earth with ocean and atmosphere
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