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????????????????????????????????????????????????SymletС?????????о?????????????????????????????????????, ???????????4???5??????????????????????????????????????2???3????????????????????????????????????????????ε????????????????ο??? 相似文献
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????13??T/P???????????????????????????????????????????????????????????????????????????????????Ubari-Murzuq????????????????????????????????????????′????????????????????????С?????Ku???κ?C???ι?????????????????????????????P???????仯?????? 相似文献
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基于卫星加速度恢复地球重力场的去相关滤波法 总被引:3,自引:0,他引:3
基于加速度法恢复地球重力场时,卫星加速度是由卫星轨道数值微分得到,而数值微分会放大高频误差,进而降低了重力场解算结果的精度.针对数值微分导出的加速度误差具有有色噪声的特性,提出利用去相关算法构造白化滤波器对加速度有色噪声进行滤波处理,并根据去相关的基本原理分别构造了基于三点差分和ARMA模型的白化滤波器.采用不同噪声背景的CHAMP卫星模拟轨道数据进行解算,结果表明:基于去相关滤波解算的重力场模型精度均要比等权解算的重力场模型精度高,初步验证了去相关滤波方法的有效性. 相似文献
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���������������Ƚ� 总被引:3,自引:2,他引:1
???Shepard???????????????????????????????Kriging????????????????п???????????????????????????????????????ε?????????????????????÷?Χ??????3????????б???????????1??????????????????????????????????????????????????2?????Kriging?????????????????????????????????????????仯???????????????????????????????????????仯С?????? 相似文献
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GRACE(Gravity Recovery And Climate Experiment)卫星计划为监测陆地水储量变化提供了有效技术手段.本文采用2003至2010年共计8年的GRACE月重力场模型反演中国西南区域陆地水储量变化,与GLDAS(Global Land Data Assimilation System)全球水文模型进行对比分析,其结果在时空分布上均符合较好,同时在2009年秋至2010年春该区域陆地水储量均呈现明显减少,与该时段云贵川三省的干旱事件相一致;比较分析了2009年秋至2010年春GRACE反演陆地水储量变化与TRMM(Tropical Rainfall Measuring Mission)合成数据计算的月降雨量的时空分布,两组结果均与西南干旱事件对应时段与区域十分吻合;对近8年的陆地水储量变化与月降雨量数据进行相关性分析,其结果表明陆地水储量变化与降雨量强相关,即降雨量是导致陆地水储量变化的主要因素;分析该区域地表温度变化,结果显示2009年9月至2010年3月地表温度均比历史同期高,地表温度的升高加剧了陆地水储量的减少. 相似文献
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基于雷达波卫星测高技术,通过数据处理获取华北平原和华东地区的地面沉降数据;优化地球物理参数和环境改正数,利用高精度SRTM模型进行地形坡度改正,通过改进的阈值算法提高测高数据的观测精度。将获取的地面沉降速率与GNSS基准站观测结果进行比较,偏差为-3.4±9.1 mm/a,相关性为0.88。采用阈值法和改进阈值法进行波形重跟踪改正的偏差分别为-3.2±5.5 mm/a和-2.9±4.1 mm/a,相关系数分别为0.94和0.97。实验结果表明,卫星测高可应用于地面沉降监测研究,尤其在缺少GNSS或传统水准监测数据的偏远地区的地面沉降监测中具有重要的研究价值。 相似文献
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In order to improve the processing and interpretation of gravity data, multiscale edge theory in image processing is introduced
into the study of gravity field. Multiscale edges of gravity anomaly are analyzed based on a special wavelet. It shows that
the multiscale edges are the extrema points of the horizontal gravity gradient at different heights, which are related to
the sharp discontinuities of underground sources. The applications of multiscale edge in downward continuation and gravity
inversion are discussed. The simulated examples show that the multiscale edges can be applied to stabilize the downward continuation
operator when the continuation height is low. The multiscale edges also have a convenient application to infer the geometry
of the underground source. Moreover, the gravity inversion algorithm based on the multiscale edges has a good antinoise property.
Supported by the National Natural Science Foundation of China(No.40704003), the National 973 Program of China(No.2007CB714405),
the Open Research Fund from Key Laboratory of Geospace Environment and Geodesy(No.04-01-08). 相似文献
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���Dz�ߵľ������¼�����չ 总被引:1,自引:0,他引:1
?????????????????????????Ka???β?????????????GNSS????????????4?????????????????????????????Щ????????????????????????????????????????????????????Ч??????????????????????????? 相似文献