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91.
A scale free representation of a general non-isochoric 2D deformation is presented which is amenable to mathematical analysis. By describing deformation in 2D in terms of polar coordinates the stretching and rotational histories of linear elements separate and are easily analysed both qualitatively and quantitatively. An analysis of finite strain combined with dynamical considerations allows the derivation of equations which may be used to estimate finite strain, area change and kinematic vorticity number. Numerical investigation of method developed here was carried out and it was found to perform well unless large area changes occur in combination with large components of simple shear. A re-analysis of natural data indicates the method is consistent. 相似文献
92.
本文首次利用完全相同两颗卫星(CLUSTER C1和C3)的数据对地球激波前兆区太阳风的减速和偏转特性进行了统计研究.结果表明,在激波前兆坐标系中,太阳风减小的速度随观测点到激波的距离DBS增大而减小,随行星际磁场与激波法向夹角θBN增大也减小,在ULF波动区深度DWS小于6Re(Re为地球半径)的范围内最为显著;伴随着太阳风减速的另外一个现象——太阳风的偏转,也存在相似的规律.其最大减速和最大偏转角度分别为10 km/s和3°.太阳风减速和偏转,以及随之变化的太阳风动压,可能会引起地球磁层顶位置和形状发生改变,同时也为激波前兆区弥散(diffuse)离子的起源及加热提供了一种可能的机制. 相似文献
93.
Maria V. Pastor Josep L. Pelegrí Alonso Hernández-Guerra Jordi Font Jordi Salat Mikhail Emelianov 《Continental Shelf Research》2008
A historical data set is used to describe the coastal transition zone off Northwest Africa during spring 1973 and fall 1975, from 17° to 26°N, with special emphasis on the interaction between subtropical (North Atlantic Central Waters) and tropical (South Atlantic Central Waters) gyres. The near-surface geostrophic circulation, relative to 300 m, is quite complex. Major features are a large cyclonic pattern north of Cape Blanc (21°N) and offshore flow at the Cape Verde front. The large cyclone occurs in the region of most intense winds, and resembles a large meander of the baroclinic southward upwelling jet. The Cape Verde frontal system displays substantial interleaving that may partly originate as mesoscale features at the coastal upwelling front. Property–property diagrams show that the front is an effective barrier to all properties except temperature. The analysis of the Turner angle suggests that the frontal system is characterized by large heat horizontal diffusion as a result of intense double diffusion, which results in the smoothing of the temperature horizontal gradients. Nine cross-shore sections are used to calculate along-shore geostrophic water-mass and nutrient transports and to infer exchanges between the coastal transition zone and the deep ocean (import: deep ocean to transition zone; export: transition zone to deep ocean). These exchanges compare well with mean wind-induced transports and actual geostrophic cross-shore transport estimates. The region is divided into three areas: southern (18–21°N), central (21–23.5°N), and northern (23.5–26°N). In the northern area geostrophic import is roughly compensated with wind-induced export during both seasons. In the central area geostrophic import is greater than wind-induced export during spring, resulting in net import of both water (0.8 Sv) and nitrate (14 kmol s−1), but during fall both factors again roughly cancel. In the southern area geostrophy and wind join to export water and nutrients during both seasons, they increase from 0.6 Sv and 3 kmol s−1 during fall to 2.9 Sv and 53 kmol s−1 during spring. 相似文献
94.
95.
探讨了地质勘探线剖面三维坐标与剖面图二维坐标相互转换方法及其实现过程,建立了数学模型,并通过计算实例进行了验证。主要作法是,根据剖面图的特性选择勘探线剖面地表迹线与勘探基线所在垂直面的交点为转换计算基准点(B),以勘探线剖面内过基准点(B)的水平直线(L)为旋转轴,将勘探线剖面旋转至水平位置;再以基准点(B)为旋转点,将勘探线剖面在水平面内旋转至水平直线(L)成东西向,建立剖面内空间要素旋转前后的关系式,实现三维坐标向二维坐标转换。按相反的操作过程,已知转换后剖面图上点的二维坐标,可以计算出剖面上对应点的三维空间坐标,实现二维坐标向三维坐标转换。 相似文献
96.
97.
The Cartesian moments of the mass density of a gravitating body and the spherical harmonic coefficients of its gravitational
field are related in a peculiar way. In particular, the products of inertia can be expressed by the spherical harmonic coefficients
of the gravitational potential as was derived by MacCullagh for a rigid body. Here the MacCullagh formulae are extended to
a deformable body which is restricted to radial symmetry in order to apply the Love–Shida hypothesis. The mass conservation
law allows a representation of the incremental mass density by the respective excitation function. A representation of an
arbitrary Cartesian monome is always possible by sums of solid spherical harmonics multiplied by powers of the radius. Introducing
these representations into the definition of the Cartesian moments, an extension of the MacCullagh formulae is obtained. In
particular, for excitation functions with a vanishing harmonic coefficient of degree zero, the (diagonal) incremental moments
of inertia also can be represented by the excitation coefficients. Four types of excitation functions are considered, namely:
(1) tidal excitation; (2) loading potential; (3) centrifugal potential; and (4) transverse surface stress. One application
of the results could be model computation of the length-of-day variations and polar motion, which depend on the moments of
inertia.
Received: 27 July 1999 / Accepted: 24 May 2000 相似文献
98.
根据等效原理及理论自洽的要求,把光速不变原理推广到弯曲时空。并在此基础上阐明了坐标、坐标变换,物理量的描述与测量等最基本问题的物理意义。 相似文献
99.
A. J. Sarnecki 《Celestial Mechanics and Dynamical Astronomy》1996,66(4):425-451
Concepts from projective geometry are used to provide a coherent framework for the determination of orbits from observation data comprising lines of sight at three known times. A novel way of presenting the results in a finite diagram is introduced, The effectiveness of the approach is demonstrated by an example, using a simple spreadsheet. A computer-graphic implementation is recommended. 相似文献
100.
Indicator Kriging without Order Relation Violations 总被引:2,自引:1,他引:1
Raimon Tolosana-Delgado Vera Pawlowsky-Glahn Juan-Jose Egozcue 《Mathematical Geosciences》2008,40(3):327-347
Indicator kriging (IK) is a spatial interpolation technique aimed at estimating the conditional cumulative distribution function
(ccdf) of a variable at an unsampled location. Obtained results form a discrete approximation to this ccdf, and its corresponding
discrete probability density function (cpdf) should be a vector, where each component gives the probability of an occurrence
of a class. Therefore, this vector must have positive components summing up to one, like in a composition in the simplex.
This suggests a simplicial approach to IK, based on the algebraic-geometric structure of this sample space: simplicial IK
actually works with log-odds. Interpolated log-odds can afterwards be easily re-expressed as the desired cpdf or ccdf. An
alternative but equivalent approach may also be based on log-likelihoods. Both versions of the method avoid by construction
all conventional IK standard drawbacks: estimates are always within the (0,1) interval and present no order-relation problems
(either with kriging or co-kriging). Even the modeling of indicator structural functions is clarified. 相似文献