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71.
R. Lehmann 《Journal of Geodesy》1997,71(9):533-540
Geodetic surface integrals play an important role in the numerical solution of geodetic boundary-value problems. In many
cases they can be evaluated using fast methods in the frequency domain (FFT). However, this is not possible in general, because
the domain of integration may be non-trivial (as is the surface of the Earth), the kernel function may not be of convolution
type, or the data distribution may be heterogeneous. Therefore, fast evaluation strategies are also required in the space
domain. They are more difficult to design because only one property is left where a more or less fast evaluation strategy
can be built upon: the potential type of the kernel function. Consequently, the idea is not to replace well-established frequency
domain techniques, but to supplement them. Our approach to this problem goes in two directions: (1) we use advanced cubature
methods where the integration nodes automatically densify in the vicinity of the evaluation points; (2) we use powerful computer
hardware, namely MIMD computers with distributed memory. This enables us to evaluate geodetic surface integrals of any practical
complexity in reasonable time and accuracy. This is shown in a numerical example.
Received: 7 May 1996 / Accepted:17 March 1997 相似文献
72.
一种符合视觉规律的,基于地图数据的虚拟地景仿真 总被引:5,自引:1,他引:5
本文分析和解决了两个关键性问题,使计算机所生成的虚拟地景符合人的“越近看得越清”视觉规律,并通过实例对该方法的实现过程给予了详细的描述。 相似文献
73.
山区河流准三维水沙输运与河床演变模拟 总被引:1,自引:0,他引:1
在渠道水力学和河流动力学研究的基础上,对不规则河流形态下的纵向流速分布和弯道水流进行了讨论,并分析了任意断面和垂线位置的流场计算公式。在综合各种泥沙动力学研究成果基础之上,探讨了在天然河流中的悬移质输沙能力与沉积条件,分析了河床质起动的控制性因素及推移质输沙方程。提出了受冲淤影响的河床质粒径组成和动态递推公式。结合这些流场与泥沙计算方法及河床形态调整技术,作者提出一个准三维河流动力学模型。该模型只需要河流几何形状、人流条件以及泥沙级配参数,能够模拟出不规则几何形态的河道断面流速分布及平面流场分布,并且对于弯道水流特征与泥沙输送一沉积特征也能得到较好的表现。该模型是对有关河流演变理论和实验成果的综合应用,为研究山区高含沙水流下的河床变形以及洪水演进提供了强有力的工具。 相似文献
74.
滑坡稳定性判别的非计算方法 总被引:2,自引:6,他引:2
用计算来确定滑坡的稳定性,由于参数选取存不确定因素,就必然导致了其计算结果的不确定性。而滑坡稳定性判别的非计算方法,是通过对滑坡发育程度、形成条件的综合分析来确定滑坡的稳定程度的方法。文中通过归纳分析波坡的形成条件,然后从滑坡地貌条件、动力作用、堆积物特征、诱发因素等方面详细阐述了滑坡稳定性判别的方法,最后,例举了川藏公路102滑坡实例对该方法进行了验证。实践证明该方法是滑坡稳定性中非常实用和有效的方法。 相似文献
75.
本文根据线路平行线间面积计算的统一模型,分别推证了直线,圆曲和缓和曲线段平行线间面积计算的简捷模型,据此归纳出线路平行线间面积计算的统一简捷模型,它在线路土地征及用建材用料计算等方面都有广泛的应用。 相似文献
76.
本文给出了平差概括模型以及其它平差函数模型之间的关系,并根据概括平差模型编制了测量平差软件,该软件能完成,间接平差,条件平差,附有参数的条件平差,附有限制条件的间接平差,通过算例,证明该具有一定的实用性。 相似文献
77.
1 IntroductionThefastFouriertransform (FFT)techniqueisaverypowerfultoolfortheefficientevaluationofgravityfieldconvolutionintegrals.Thankstothegoodcomputationefficiency ,theFFTtechnique ,inthemid_1 980s ,begantofindwidespreaduseingeoiddetermination ,whencompar… 相似文献
78.
79.
The circulation of the Southern Ocean is studied in the eddy-resolving model POP (Parallel Ocean Program) by an analysis
of zonally integrated balances. The TEM formalism (Transformed Eulerian Mean) is extended to include topography and continental
boundaries, thus deviations from a zonally integrated state involve transient and standing eddies. The meridional circulation
is presented in terms of the Eulerian, eddy-induced, and residual streamfunctions. It is shown that the splitting of the meridional
circulation into Ekman and geostrophic transports and the component induced by subgrid and Reynolds stresses is identical
to a particular form of the zonally integrated balance of zonal momentum. In this balance, the eddy-induced streamfunctions
represent the interfacial form stresses by transient and standing eddies and the residual streamfunction represents the acceleration
of the zonal current by density fluxes in a zonally integrated frame. The latter acceleration term is directly related to
the surface flux of density and interior fluxes due to the resolved and unresolved eddies. The eddy-induced circulation is
extremely vigorous in POP. In the upper ocean a shallow circulation, reversed in comparison to the Deacon cell and mainly
due to standing eddies, appears to the north of Drake Passage latitudes, and in the Drake Passage belt of latitudes a deep-reaching
cell is induced by transient eddies. In the resulting residual circulation the Deacon cell is largely cancelled and the residual
advection of the zonal mean potential density is balanced by diapycnal eddy and subgrid fluxes which are strong in the upper
few hundred meters but small in the ocean interior. The balance of zonal momentum is consistent with other eddy-resolving
models; a new aspect is the clear identification of density effects in the zonally integrated balance. We show that the wind
stress and the stress induced by the residual circulation drive the eastward current, whereas both eddy species result in
a braking. Finally, we extend the Johnson–Bryden model of zonal transport to incorporate all relevant terms from the zonal
momentum balance. It is shown that wind stress and induction by the residual circulation carry an eastward transport while
bottom form stress and the stress induced by standing eddies yield westward components of transport.
Received: 26 June 2001 / Accepted: 2 November 2001 相似文献
80.