共查询到15条相似文献，搜索用时 796 毫秒
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研究了内核幌动（ICW）自由内核章动（FICN）。为了给出解析结果，采纳了一个简单地球模型。与以往的研究相比，本文的新结果包括了内核相对地幔的转速和倾角的影响。 相似文献
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由于地球自转导致的自由核章动(FCN)及内核自由章动(FICN)等地球简正模是地球内部动力学过程的重要表征,也是认识核幔边界和内外核边界的重要手段,其包含的物理信息可为目前地球深部的研究手段比较匮乏的情况下获得地球深内部结构及物理性质和研究核幔及内外核耦合提供非常重要的约束。本文围绕地球自由核章动利用全球地球动力学计划观测网提供的全球超导重力观测资料和国际VLBI服务组织提供的章动观测资料,采用不同方法研究了自由核章动的本征周期和品质因子等 相似文献
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同时顾及章动和极移的地球自转方程 总被引：13，自引：0，他引：13
郭俊义 《武汉测绘科技大学学报》2000,25(5):393-395,408
通过引进章动坐标系相对惯性参照系的转动角速度随时间的变化,导出了一个可同时解出章动和极移的地球自转方程,用这个方程可同时研究地球的强迫和自由转动,与现行研究地球自转的惯用方法相比,该方法综合性强,易于理解。 相似文献
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郭俊义 《武汉大学学报(信息科学版)》2000,25(5):393-395
通过引进章动坐标系相对惯性参照系的转动角速度随时间的变化 ,导出了一个可同时解出章动和极移的地球自转方程 ,用这个方程可同时研究地球的强迫和自由转动。与现行研究地球自转的惯用方法相比 ,该方法综合性强 ,易于理解。 相似文献
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地球自转的精确测定是高精度大地参考系建立的理论基础,也是天体测量学、大地测量学和地球物理学共同关注的研究领域。研究了液核弹性地球自转动力学的基本理论,主要内容包括:修正了固体潮和地球自转对地球惯量张量元影响的表达式;首次顾及了日月高阶岁差章动力矩对地球自转的影响,引进了周期满足小于等于0 5d和大于等于1 5d的其它摄动机制(例如:大气、海洋和地表水分布等)对地球自转的影响;形式上对Rochester的耗散力矩表达式进行了变换,使得耦合系数变为无量纲的参数。本文的推导理论上更为严格,形式上更为完美对称,并为以后定义液核地球模型的CEP轴和CIP轴打下基础。本文给出的理论公式可为动力大地测量学和天文地球动力学的研究提供理论参考和依据。 相似文献
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地球自转速率的潮汐变化与尺度因子成正比,影响尺度因子各种地球物理机制是复杂的,主要有液核、海洋动力学(平衡海潮和非平衡海潮)、大气、地幔滞弹性等.文中讨论了大气、地幔滞弹性,并对影响地球自转尺度因子的同一机制不同理论模型进行了对比分析. 相似文献
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主要章动项振幅与自由核章动的检测 总被引：1，自引：0，他引：1
章动观测值与理论值之间的差异提示人们，当前所使用的Ｗａｈｒ章动理论中存在一些未知的效应。本文利用ＶＬＢＩ观测资料和测纬资料，对主要章动项振幅和自由核章动周期进行了检验。实际计算表明，根据ＶＬＢＩ资料和测纬资料的处理，所得到的自由核章动周期是相同的。 相似文献
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We compare nutation time series determined by several International VLBI Service for geodesy and astrometry (IVS) analysis centers. These series were made available through the International Earth Rotation and Reference Systems Service (IERS). We adjust the amplitudes of the main nutations, including the free motion associated with the free core nutation (FCN). Then, we discuss the results in terms of physics of the Earth’s interior. We find consistent FCN signals in all of the time series, and we provide corrections to IAU 2000A series for a number of nutation terms with realistic errors. It appears that the analysis configuration or the software packages used by each analysis center introduce an error comparable to the amplitude of the prominent corrections. We show that the inconsistencies between series have significant consequences on our understanding of the Earth’s deep interior, especially for the free inner core resonance: they induce an uncertainty on the FCN period of about 0.5 day, and on the free inner core nutation (FICN) period of more than 1000 days, comparable to the estimated period itself. Though the FCN parameters are not so much affected, a 100 % error shows up for the FICN parameters and prevents from geophysical conclusions. 相似文献
13.
Analytical versus semi-analytical determinations of the Oppolzer terms for a non-rigid Earth 总被引：1，自引：1，他引：0
Estimations of the Oppolzer terms for the angular momentum and rotation axes of a non-rigid Earth are obtained from two different
approaches and compared. The first approach is an analytical method which relies on the solutions of the Liouville equations
for a two-layer Earth model. The Oppolzer terms are evaluated from analytical expressions. The results are then compared to
those calculated from Wahr's theory of nutation for a non-rigid Earth, which is the second approach used. Results are obtained
for the main nutation frequencies and for the precession case. The differences between the two solutions are generally quite
small (the relative error is most of the time under 8%) and are, for a large part, due to successive approximations and truncation
effects during their determination. Departures of the results from the two methods are significantly larger for frequencies
near the Free Core Nutation (FCN) resonance. This is particularly true for the Oppolzer terms of the angular momentum axis.
The Earth model adopted is a little bit different in each case: for the Liouville system solution, we have limited the model
to a homogeneous elastic mantle and a homogeneous liquid core. Another source of some of the small differences in the results
is the presence of a solid inner core in Wahr's theory. We confirm through the analytical calculation the strong effect of
the core on the Oppolzer terms of the angular momentum axis for a non-rigid Earth at the precession frequency. Finally, an
application is given in the determination of the axes' position at J2000 for a non-rigid Earth.
Received: 23 February 1998 /Accepted: 18 November 1998 相似文献
14.
The temporal change of the rotation vector of a rotating body is, in the first order, identical in a space-fixed system and
in a body-fixed system. Therefore, if the motion of the rotation axis of the earth relative to a space-fixed system is given
as a function of time, it should be possible to compute its motion relative to an earth-fixed system, and vice versa. This
paper presents such a transformation. Two models of motion of the rotation axis in the space-fixed system are considered:
one consisting only of a regular (i.e., strictly conical) precession and one extended by circular nutation components, which
are superimposed upon the regular precession. The Euler angles describing the orientation of the earth-fixed system with respect
to the space-fixed system are derived by an analytical solution of the kinematical Eulerian differential equations. In the
first case (precession only), this is directly possible, and in the second case (precession and nutation), a solution is achieved
by a perturbation approach, where the result of the first case serves as an approximation and nutation is regarded as a small
perturbation, which is treated in a linearized form. The transformation by means of these Euler angles shows that the rotation
axis performs in the earth-fixed system retrograde conical revolutions with small amplitudes, namely one revolution with a
period of one sidereal day corresponding to precession and one revolution with a period which is slightly smaller or larger
than one sidereal day corresponding to each (prograde or retrograde) circular nutation component. The peculiar feature of
the derivation presented here is the analytical solution of the Eulerian differential equations. 相似文献
15.
Due to the super rotation of the Earth’s inner core, the tilted figure axis of the inner core would progress with respect to the mantle and thus cause the variation of the Earth’s external gravity field. This paper improves the present model of the gravity field variation caused by the inner core super rotation. Under the assumption that the inner core is a stratifying ellipsoid whose density function is fitted out from PREM and the super rotation rate is 0.27～0.53°/yr, calculations show that the global temporal variations on the Earth’s surface have a maximum value of about 0.79～1.54×10?3 μGal and a global average intensity of about 0.45～0.89×10?3 μGal in the whole year of 2007, which is beyond the accuracy of the present gravimetry and even the super conducting gravimeter data. However, both the gravity variations at Beijing and Wuhan vary like sine variables with maximal variations around 0.33 μGal and 0.29 μGal, respectively, in one cycle. Thus, continuous gravity measurements for one or two decades might be able to detect the differential motion of the inner core. 相似文献