共查询到17条相似文献，搜索用时 234 毫秒
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重力垂直梯度异常反应了重力异常的空间变化率,在地球物理勘探等多学科中得到越来越多的应用。利用南海局部区域实测重力异常数据和Sandwell测高重力异常数据,将搜索范围、距离和精度多种因素融合考虑并对Shepard算法进行改进,给出了南海局部区域(19°N~20.5°N,114°E~115.5°E)分辨率1'×1'的重力异常并反演了对应分辨率的重力垂直梯度异常。结果表明,基于Shepard改进算法的高精度船测重力和测高重力的有机融合,增强了单一测高重力数据反演重力垂直梯度异常的细节纹理,提高了反演重力垂直梯度异常的分辨率和精度。 相似文献
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基于重力地质法(GGM)采用卫星重力异常数据反演了中国南海112°E~119°E,16°N~20°N范围1'×1'的海底地形模型,通过船测水深数据的直接格网化结果和ETOP01模型的检核进行了精度评价。结果表明,GGM模型较船测水深的直接格网化结果更为精细,在船测控制点分布均匀的海域,GGM模型能获得比ETOP01模型更高的精度。为进一步验证GGM模型受海底地形特征影响的情况,采用GGM模型与ETOP01模型分别内插出9356个检核点处的水深,并统计得到两模型差值的较差结果平均值为19.560m,标准差为130.156m,相对精度为4.79%。经分析得出:GGM模型与ETOP01模型在坡度变化平缓深海区有着较好的一致性,随着水深的依次变浅,二者的差异逐渐显现,在多海山的海域差异达到最大。最后,为充分发挥重力地质法在海底地形反演中的优势总结了其最佳适用条件。 相似文献
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海底地形是全球地形的重要组成部分,对地球物理科学研究、经济活动等具有重要作用。基于Parker公式,利用卫星测高重力异常和船测水深数据,采用频域的方法反演了疑似马航MH370失事区域的留尼汪海域的10°×10°的海底地形。最后将反演的水深和船测水深、国际通用的海深模型ETOPO1作比较进行精度评估,结果表明:本文反演结果与船测水深相比误差平均值为-26.038 m,标准差为176.588 m;与ETOPO1相比,差异平均值为-33.541 m,标准差为160.769 m。这表明采用重力异常数据,结合船测数据能较高精度地反演海底地形。 相似文献
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根据重力地质法(Gravity Geological Method, GGM),利用6 736个已知水深点数据和卫星测高重力异常反
演了马里亚纳海沟(142°36''~147°18''E,23°~27°N)1''×1''分辨率的海底地形,该计算中的密度差常数为1.20 g/cm3。将反演的地形与实测检核水深数据相比,两者较差标准差为152.9 m,平均误差为(±3.0) m,均方差为153.0 m,优于ETOPO1模型和直接把船测水深控制点格网化后的模型。将重力地质法反演的模型、ETOPO1模型、直接格网模型进行功率谱密度分析,结果显示3种模型在中长波地形能量一致,但对于短波地形,重力地质法模型能量高于其他2个模型,说明重力地质法更能描绘细致的海底地形地貌。选取2条测线与重力地质法模型进行对比研究,结果表明重力地质法在海底地形起伏小的区域优于在海底地形起伏较大区域的反演效果。 相似文献
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通过联合HY-2A、TP、Envisat卫星的高度计数据,分析HY-2A测高数据对中国南海重力异常影响。首先,将HY-2A和TP、Envisat数据进行对比,通过共线处理和交叉点平差前后的不符值RMS统计分析表明,HY-2A数据精度优于TP变轨后及Envisat数据精度;利用逆Venning-Meinesz公式分别计算中国南海海域(0°~23°N,103°E~120°E)15'×15'的重力异常,将反演结果与船测结果对比,HY-2A数据加入反演得到的重力异常精度在±6.13m Gal,其精度要优于没有HY-2A反演得到的结果,并分析反演重力异常与船测重力差值分布规律。结果表明,HY-2A数据对于提高海洋重力异常计算精度具有一定意义。 相似文献
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针对基于测高重力异常反演海底地形理论众多、选取标准无法确定的情况,利用中国南海海域内的测高重力异常和船测水深数据研究比较了重力地质法(GGM)和SmithSandwell (SAS)法两种精度高、计算速度相对较快的海底地形反演理论。其中,GGM方法的密度差异常数Δρ由向下延拓技术确定为2.15 g·cm-3,SAS方法采用移去-恢复技术得到反演波段内重力异常和水深数据。结果表明:测线分布条件一定时,水深多在-1 000 m左右或反演区域岛礁、海山等复杂海底地形较多时选取SAS方法,水深主要在-3 000 m以深的区域或海底地形复杂程度不高时选取GGM方法则能获取更好的效果,其效果最优处与船测水深在检核点处的差值最优平均值能达-0.61 m,标准差可达14.67 m。 相似文献
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联合T/P、ERS1/GM、ERS1/ERM、ERS2/ERM、GEOSAT/ERM、GEOSAT/GM等多源卫星测高数据,基于逆Vening-Meinesz公式和EGM2008模型,采用移去-恢复方法和快速傅里叶变换算法构建了中国西太平洋海域(0°~40°N,105°E~145°E)1'×1'重力异常模型,选取两个不同特征区域航线,将构建的重力异常模型、EGM2008重力异常模型、美国Scripps海洋研究所重力异常与船测重力数据进行比较分析。结果表明,构建的重力异常模型与船测重力总体趋势变化较为一致、与船测重力比较均方根差为4.16m Gal,总体精度与EGM2008模型重力异常、美国Scripps海洋研究所重力异常相当,反演精度和分辨率达到国际领先水平。 相似文献
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本文给出了向种规则形状二度和三度体重力异常的希尔伯特变换式，提出了一种利用希尔伯特变换反演异常体的方法。这种方法充分利用了重力异常信息：利用重力异常△g(x)曲线和它的希尔伯特变换H（x）曲线及△g(x)-H（x）参量图上的某些特征点直接反演异常体形状参数及埋深。方法简单、实用。 相似文献
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Min zhang Hu Jian cheng Li Hui Li Chong Yang Shen Tao yong Jin Le lin Xing 《Marine Geodesy》2013,36(2):176-189
A new one-minute global seafloor topography model was derived from vertical gravity gradient anomalies (VGG), altimetric gravity anomalies, and ship soundings. Ship soundings are used to constrain seafloor topography at wavelengths longer than 200 km and to calibrate the topography to VGG (or gravity) ratios at short wavelengths area by area. VGG ratios are used to predict seafloor topography for wavelength bands of 100–200 km and to suppress the effect of crust isostasy. Gravity anomalies are used to recover seafloor topography at wavelengths shorter than 100 km. The data processing procedure is described in detail in this paper. The accuracy of the model is evaluated using ship soundings and existing models, including General Bathymetric Charts of the Oceans (GEBCO), DTU10, ETOPO1, and SIO V15.1. The results show that, in the discussed regions, the accuracy of the model is better than ETOPO1, GEBCO, and DTU10. Additionally, the model is comparable with V15.1, which is generally believed to have the highest accuracy. In the north-central Pacific Ocean, the accuracy of the model increased by approximately 29.5% compared with the V15.1 model. This indicates that a more accurate seafloor topography model can be formed by combining gravity anomalies, VGG, and ship soundings. 相似文献
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《Marine Geodesy》2012,35(1):63-85
AbstractWe introduce an iterative inversion method to address the problems in high-order seafloor topography inversion using gravity data (gravity anomaly and vertical gravity gradient anomaly), such as the difficulty in computing the equation and the uniqueness of the calculation results. A part of the South China Sea is selected as the experimental area. Considering the coherence and admittance function of gravity topography and vertical gravity gradient topography, the inversion band of the gravity anomaly and vertical gravity gradient anomaly in the study area is 30?km–120?km. Seafloor topography models of different orders are constructed using an iterative method, and the performance of each seafloor topography model is analyzed against ETOPO1 and other seafloor topography models. The experimental results show that as the inversion order increases, the clarity and richness of seafloor topographic expression continuously improve. However, the accuracy of seafloor topography inversion does not improve significantly when the inversion order exceeds a certain value, which is related to the contribution of high-order seafloor topography to gravity information. The results show that the accuracy of BGT4 (inversion model constructed by the gravity anomaly) is slightly poorer than that of BVGGT4 (inversion model constructed by the vertical gravity gradient anomaly) in areas with complex topography, such as multi-seamounts and trenches, and the results are generally better in areas with flat seafloor topography. 相似文献
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We have obtained regression relationships between vertical components of gravity anomalies in tropical cyclone areas and some cyclonic characteristics. These regressions are more pronounced in territories where negative gravity anomalies are prevalent. Numerical experiments are performed for the cyclonic zone of the northwestern Pacific and western Atlantic. In the zone of the western Atlantic, the main focus is on cyclones entering to the terrestrial part of the United States. We conclude that under some conditions, gravity anomalies can affect the characteristics of tropical cyclones. 相似文献
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Inversion modelling of marine gravity anomalies to derive predicted seafloor topography has provided significant advance in delineating deep-ocean bathymetry where the seafloor both conforms to the half-space cooling model of seafloor spreading, and largely sediment-free. Similar modelling for elevated ridges and seamounts, that are formed by processes other than seafloor spreading and/or have proximal sediment sources (e.g., continental margins and volcanic arcs), have significantly higher errors when validated against modern shipborne echo-sounding data. A three-dimensional, five-layer gravity model is emulated for the cases of both synthetic and real seamounts, with varying degrees of sediment burial, to establish the sensitivity of variable sediment cover as a source of error. A simple `Gaussian' seamount with base radius of 30 km, 2000 m of relief, has a maximum 140–160 mGal anomaly, that decreases to 50 mGal with the addition of 1 km of sediment cover with simple `flood' geometry. Complete burial, with a typical sediment density of 2300 kg m–3, results in a 120 mGal difference from a sediment-free seamount model. Increasing sediment density results in an exponential decay of the seamount anomaly. More complex synthetic geometries of varying basement relief and sediment thickness show that the anomaly amplitude remains significant, especially where the latter is >700–800 m thick. For the real case, seamounts of the Three Kings Ridge (northern New Zealand) imaged with seismic reflection data, with varying degrees of sediment cover of up to 1 km, when modelled both with and with-out the inclusion of a sediment layer, typically have rms differences of 30 mGal between observed and modelled gravity anomalies. Significantly, the rms errors are reduced by 50% with the inclusion of a sediment layer that corresponds to a reduction of predicted seafloor topography rms errors of 192–684 m to 78–360 m. 相似文献
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M. E. Artemjev T. M. Babaeva V. O. Mikhailo I. E. Voydetsky 《Marine Geophysical Researches》1984,7(1-2):129-148
All anomalous masses of the Earth are reflected in the free air gravity anomalies and the geoidal undulations. The low viscosity
of the asthenosphere significantly reduces the possibility of existence of density inhomogeneities in the layer. This fact
provides some physical basis for the separation of the gravity field anomalies. It has been shown by power spectrum analysis
of the free air anomalies and gravity field of isostatically compensated model of the lithosphere for the North Atlantic and
adjacent areas of America, Europe and Mediterranean, that the attraction of isostatically compensated model is significant
for any wave length of the field. It causes significant error in the interpretation if long wavelength constituents of the
free air gravity anomalies are considered as a field of deep anomalous masses. The isostatic anomalies und isostatic geoid
are free from the influences of isostatically compensated lithosphere. The characteristic feature of the isostatic anomalies
power spectrum is a pronounced minimum at the wavelength of about 1000 km. The relative homogeneity of the asthenosphere may
explain this minimum. It means that principal density inhomogeneities of the Earth's interior are separated by the asthenospheric
layer. Such a minimum has not been observed at the power spectrum of free air anomalies being masked by corresponding wavelength
of the field of isostatically compensated lithosphere. Isostatic anomalies that reflect the differences between the real structure
of the lithosphere and its isostatically compensated model have wavelengths less than 1000 km. Isostatic anomalies with the
wavelength more than 1000 km reflect the attraction of density inhomogeneities situated under the level of isostatic compensation.
The basic features of power spectrum of isostatic anomalies are the same for oceanic and continental areas. The method based
on Kolmogorov-Wiener filtration which consideres statistical characteristics of the field has been developed to divide the
isostatic gravity anomalies into lithosphere and mantle components. For the North Atlantic and adjacent areas the field of
mantle inhomogeneities has been determined. 相似文献
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To provide easy access to the large number of Seastat and Geosat altimeter observations collected over the last decade, we have plotted these satellite altimeter profiles as overlays to the General Bathymetric Chart of the Oceans (GEBCO). Each of the 32 overlays displays along-track gravity anomalies for either ascending (southeast to northwest) or descending (northeast to southwest) altimeter passes. Where Seasat and Geosat profiles coincide, only the more accurate Geosat profiles were plotted. In poorly charted southern ocean areas, satellite altimeter profiles reveal many previously undetected features of the seafloor. 相似文献
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为充分挖掘海洋重力数据在反演海底地形中的应用潜力,尝试探索利用大地水准面高反演海底地形的技术途径,并以夏威夷—皇帝海山链拐点所在海区作为反演试验区进行验证。首先采用Belikov列推法计算伴随(缔和)勒让德函数,利用EIGEN-6C4地球重力场模型解算获取了分辨率为1'的大地水准面高格网数值模型;然后通过综合分析反演比例函数和转换函数特点、研究海区大地水准面高与海底地形的相干特性以及大地水准面高本身尺度特征,获得了利用大地水准面高反演海底地形的频段范围;最终以试验海区大地水准面高为数据输入,构建了相应的海底地形模型(BNT模型),并与ETOPO1等海深模型进行比对分析。试验结果表明:BNT模型检核差值在一倍均方差范围检核点数量占比70.60%,相比正态分布更加集中;BNT模型检核精度低于ETOPO1等海深模型;海深模型检核精度随着水深增加不断提升,水深小于1 000 m时,海深模型相对误差出现较大发散现象;计算海域ETOPO1模型精度最高,GEBCO模型和DTU10模型检核精度相当。 相似文献