遥感影像配准误差传递模型及模拟分析   总被引：3，自引：0，他引：3  

葛咏  梁怡  马江洪  王劲峰 《遥感学报》2006,10(3):299-305

在遥感影像配准过程中,通常假设控制点是“完美的”。然而,在实际情况中,由于控制点本身不可避免的带有一定的误差导致这种假设在一定情况下并不成立,并且将会影响遥感影像几何校正的精度。普通最小二乘方法OLS(O rd inary Least Square)是遥感影像配准常用的校正估计模型,令人遗憾的是,在控制点存在误差的情况下,它的估计是有偏的,并且不能够正确传递和估计校正影像的误差大小。引入一致校正最小二乘方法CALS(ConsistentAd justed Least Squares),在此基础上提出的一个改进的方法,称之为松弛一致校正最小二乘方法RCALS(Relaxed ConsistentAd justed Least Squares)。这类回归模型具有改正控制点(解释变量)中的误差和跟踪回归模型中的误差传递的能力。为了验证CALS和RCALS模型的有效性,本文利用模拟影像进行分析。这里着重分析OLS,CALS和RCALS模型在几何校正过程中的比较。结果表明,RCALS和CALS的结果优于OLS估计结果。  相似文献   

Neotectonic Crustal Uplift on the Continents and its Possible Mechanisms. The Case of Southern Africa     

Eugene V. Artyushkov  Albrecht W. Hofmann 《Surveys in Geophysics》1998,19(5):369-415

According to a large volume of data an intensive crustal uplift began in the Oligocene over most of the continental areas after a long period of relative tectonic stability. This Neotectonic uplift formed most of the present positive topographic features on the continents, and its strong acceleration took place during the last several million years. In many regions the uplift was associated with magmatism. The main methods of studying the Neotectonic uplift are considered together with the data on the uplift of Southern Africa. In this area the uplift took place in the Early Miocene (up to 300 m) and in the Late Pliocene and Pleistocene (up to 900 m). It occurred without stretching or shortening of the crust. Rapid erosion of the lower part of mantle lithosphere by a plume material is proposed as a mechanism of the uplift. This material ascended from below and rapidly spread along the base of the lithosphere. Its spreading for 1000 km during a few million years is possible only under a low viscosity of normal asthenosphere (1019 Pa s) and a much lower viscosity of a plume material (2 × 1016 Pa s). As in Southern Africa, in most of the regions the Neotectonic uplift was associated with insignificant shortening or stretching of the crust. This indicates that in some regions a plume material ascended from below and rapidly spread along the base of the lithosphere and eroded the mantle lithosphere in vast areas beneath the continents. In regions with a hot asthenosphere a strong weakening of the mantle lithosphere which allows its erosion can be associated with a high temperature of the plume material. In regions where the asthenosphere is at moderate temperature weakening of the mantle lithosphere can result from infiltration of volatiles from the plume material.  相似文献   

Weather and traffic accidents in Hong Kong     

Yuk Yee Yan Department of Geography Hong Kong Baptist University Kowloon Tong  Hong Kong 《地理学报(英文版)》1998,(3)

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A simple, but useful, application of image analysis     

Eugene F. Stoermer 《Journal of Paleolimnology》1996,15(1):111-113

Available image analysis tools are useful aids to some common tasks necessary for diatom identification. In particular, availability of this technology allows easier and more certain enumeration of closely spaced and difficult to resolve striae. Dimensional information may also be easily and accurately measured and recorded.  相似文献   

Application of a quasi-nonhydrostatic parameterization for numerically modeling neutral flow over an isolated hill     

Jerome D. Fast  Eugene S. Takle 《Boundary-Layer Meteorology》1988,44(3):285-304

A parameterization of the nonhydrostatic pressure was modified and adapted to a nonlinear numerical model of the neutral atmospheric boundary layer. A hydrostatic model and the quasinonhydrostatic version were used to simulate neutral flow over a symmetrical hill of uniform roughness. Mean-flow quantities and some turbulence characteristics of the flow from both models are presented. These results were compared with observations, analytic theory, and other numerical models.The quasi-nonhydrostatic method produced qualitative features commonly observed in such flows that the hydrostatic model could not simulate. For instance, the observed velocity reduction at the hill base and the speedup at the summit both were simulated by the quasi-nonhydrostatic model. However, computation of vertical velocities from the incompressible continuity equation is inadequate above regions of recirculation and presents a limitation to the method.Journal Paper No. J-12741 of the Iowa Agriculture and Home Economics Experiment Station, Ames, Iowa. Project No. 2779.  相似文献   

OVER AGAIN ON WHAT IS HYDROGEOLOGY?     

Eugene V. Pinneker 《Ground water》1989,27(6):882-882

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The occurrence and toxicity of herbicides in reef building corals     

Peter W Glynn  L.S Howard  Eugene Corcoran  Ana D Freay 《Marine pollution bulletin》1984,15(10):370-374

Herbicide residues including 2,4-D and 2,4,5-T have been detected in the tissues of corals subject to massive mortality in the Gulf of Chiriquí, Panamá. Tolerance tests conducted using Pocillopora damicornis demonstrated a toxic effect of a commercial herbicide (incorporating 2,4-D) on this coral.  相似文献   

Mars: Subsurface properties from observed longitudinal variation of the 3.5-mm brightness temperature     

Eugene E. Epstein  Bryan H. Andrew  Frank H. Briggs  Bruce M. Jakosky  Frank D. Palluconi 《Icarus》1983,56(3):465-475

Measurements at 3.5 mm of the disk-average brightness temperature of Mars during the 1978 opposition can be represented by (The errors cited are from the internal scatter; the estimated absolute calibration uncertainty is 3%.) This longitudinal variation must be taken into account if Mars is to be used as a calibration source at millimeter wavelengths. The total range of the 3.5-mm variation is three to four times larger than both the 2.8-cm and 20-μm variations. This unexpected result can possibly be explained by subsurface scattering from rocks ?1.5-cm radius.  相似文献   

X-ray absorption fine structure determination of pH-dependent U-bacterial cell wall interactions     

S.D KellyK.M Kemner  J.B FeinD.A Fowle  M.I Boyanov  B.A BunkerN Yee 《Geochimica et cosmochimica acta》2002,66(22):3855-3871

X-ray absorption fine structure (XAFS) measurements was used at the U L3-edge to directly determine the pH dependence of the cell wall functional groups responsible for the absorption of aqueous UO₂²⁺ to Bacillus subtilis from pH 1.67 to 4.80. Surface complexation modeling can be used to predict metal distributions in water-rock systems, and it has been used to quantify bacterial adsorption of metal cations. However, successful application of these models requires a detailed knowledge not only of the type of bacterial surface site involved in metal adsorption/desorption, but also of the binding geometry. Previous acid-base titrations of B. subtilis cells suggested that three surface functional group types are important on the cell wall; these groups have been postulated to correspond to carboxyl, phosphoryl, and hydroxyl sites. When the U(VI) adsorption to B. subtilis is measured, observed is a significant pH-independent absorption at low pH values (<3.0), ascribed to an interaction between the uranyl cation and a neutrally charged phosphoryl group on the cell wall. The present study provides independent quantitative constraints on the types of sites involved in uranyl binding to B. subtilis from pH 1.67 to 4.80. The XAFS results indicate that at extremely low pH (pH 1.67) UO₂²⁺ binds exclusively to phosphoryl functional groups on the cell wall, with an average distance between the U atom and the P atom of 3.64 ± 0.01 Å. This U-P distance indicates an inner-sphere complex with an oxygen atom shared between the UO₂²⁺ and the phosphoryl ligand. The P signal at extremely low pH value is consistent with the UO₂²⁺ binding to a protonated phosphoryl group, as previously ascribed. With increasing pH (3.22 and 4.80), UO₂²⁺ binds increasingly to bacterial surface carboxyl functional groups, with an average distance between the U atom and the C atom of 2.89 ± 0.02 Å. This U-C distance indicates an inner-sphere complex with two oxygen atoms shared between the UO₂²⁺ and the carboxyl ligand. The results of this XAFS study confirm the uranyl-bacterial surface speciation model.  相似文献   

Space, citizenship, and the right to the city: A brief overview     

Eugene J. McCann 《GeoJournal》2002,58(2-3):77-79

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