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121.
在讨论测点高程平移法区域重力地改的精度问题基础上,提出了系统差概念,并推荐一种新的计算方法,即把测点高程平移法和节点高程插值法有机地结合起来实现地改,通过理论模型和实例计算,表明该方法计算精度优于节点高程插值法和测点高程平移法。 相似文献
122.
本文在分析自动脉冲数字测相基本原理的基础之上,推出了不仅与测距频率有关,而且还与填充脉冲频率及低频测相频率有关的新的频率改正公式,并给出新的频率改正公式与传统频率改正公式之间等同的条件,即有锁相环路(或频率跟踪电路)的正常工作来保证。 相似文献
123.
124.
豫西南矽线石物相分析方法研究 总被引:2,自引:2,他引:2
以豫西南地区4个矿区的矿物组合为依据,建立了铝量法测定矽线石含量的物相分析方法。对比了不同方法制备的矽线石及其不同存在条件下溶解率的差异,确定了接近矿区实际的、准确合理的分析结果校正办法。 相似文献
125.
利用ERA-Interim 1979—2018年6—8月的再分析资料,通过相关分析、信息流、合成分析等方法研究了南亚高压强度与其邻近地区垂直速度的相互依赖关系.结果表明:南亚高压在上对流层-下平流层区域具有上冷下暖的热力结构,冷、暖中心分别在70 hPa和250 hPa,以这两层的温度异常建立的温差指数可以反映南亚高压的强度.在不同时间尺度上,南亚高压强度与其邻近地区垂直速度的相互依赖关系是不同的.在月时间尺度上,南亚高压强度通过动力作用影响邻近地区的垂直速度,南亚高压增强(减弱)时,其东部地区的上升运动和西部地区的下沉运动同步增强(减弱);在日时间尺度上,南亚高压中部的垂直速度通过热力强迫影响南亚高压强度,南亚高压中部地区上升运动增强(减弱)时,南亚高压增强(减弱)且位置偏西(偏东). 相似文献
126.
Estimation of abl Parameters Using the Vertical Velocity Measurements of an Acoustic Sounder 总被引:2,自引:0,他引:2
J. A. Kalogiros C. G. Helmis D. N. Asimakopoulos P. G. Papageorgas 《Boundary-Layer Meteorology》1999,91(3):413-449
The friction velocity, the surface heat flux and the height of the Atmospheric Boundary Layer (ABL) are important parameters. In this work, vertical velocity variance (
w
2
) and wind velocity structure parameter (C
v
2
) profiles estimated by acoustic sounder measurements are used, along with similarity relations, to estimate these parameters in the unstable Atmospheric Boundary Layer and the friction velocity in the stable one. The data were collected by two acoustic sounders with different height range and resolution under various atmospheric conditions (stability) and at two experimental sites in different terrain. The C
v
2
profiles are estimated using gate difference of the vertical velocity measurements and the assumption of local isotropy. The vertical velocity data are corrected for the significant effects of noisy measurements and sampling volume averaging on the
w
2
and C
v
2
estimations using original techniques that are presented in this work. The results of the similarity method using acoustic sounder data are compared against estimates of the corresponding atmospheric parameters obtained from direct measurements. The comparison confirms the ability of the method to provide reasonably accurate estimates of these parameters especially in the middle of the day. 相似文献
127.
ABSTRACT In this paper, we propose a method to regenerate Rational Polynomial Coefficients (RPCs) using KOMPSAT-3A imagery and to reduce the geolocation error using minimum ground control points (GCPs). To estimate the new RPCs, the physical sensor model fitted to KOMPSAT-3A imagery was utilized and virtual GCPs over the study area were created. The size of the virtual grid used was 20x20x20. To remove the sensor-related errors in physical sensor model, three different image correction models (image coordinate translation model, shift and drift model, and affine transformation model) were additionally applied. We evaluated our proposed method in two areas within Korea, one in urban (Seoul) and one in rural (Goheung) areas. The results showed that there was a significant improvement after applying the suggested approach in the two areas. The image coordinate translation model is suggested in terms of GCP requirement and expected errors estimated from the error propagation analysis using Gauss–Markov Model (GMM). 相似文献
128.
遥感影像镶嵌时拼接缝的消除方法 总被引:29,自引:0,他引:29
对现有的影像并接缝消除方法的优缺点进行了分析,提出了拼接缝消除的强制改正方法,并用大量的实际图像进行了试验。结果表明:所提出的方法具有较好的拼接缝消除效果,且算法简单,易于实现,可以处理彩色和黑白等多种图像。 相似文献
129.
Wavelet filter analysis of atmospheric pressure effects in the long-period seismic mode band 总被引:2,自引:0,他引:2
The importance of the reduction of atmospheric pressure effects becomes very clear when investigating seismic normal-mode spectra below 1.5 mHz. The usual simple correction method consists in subtracting a term converted from local atmospheric pressure (pressure multiplied by a frequency-independent admittance) from the gravity record in time domain. Thus, estimating an efficient admittance is the key for an improved correction. Band-pass filters derived from dyadic orthogonal wavelet transform, having narrow pass-bands with good frequency response but without Gibbs phenomenon and causing no phase lag, are very helpful to estimate an efficient admittance, which is both time and frequency-dependent. Processing of high quality superconducting gravimeter (SG) records for the great Sumatra earthquake (Mw = 9.3, Dec 26, 2004) with wavelet filters reveal the three very well resolved splitting singlets of overtone 2S1 with a single gravity record after correction with time-dependent and frequency-dependent admittances. We also observe all coupled toroidal modes below 1.5 mHz, except 0T5, 0T7 and 1T1, with good signal-to-noise ratio (SNR); moreover, toroidal modes 1T2 and 1T3 are for the first time unambiguously revealed in vertical components. 相似文献
130.
Chang Li Robert D. van der Hilst M. Nafi Toksöz 《Physics of the Earth and Planetary Interiors》2006,154(2):180-195
We have produced a P-wave model of the upper mantle beneath Southeast (SE) Asia from reprocessed short period International Seismological Centre (ISC) P and pP data, short period P data of the Annual Bulletin of Chinese Earthquakes (ABCE), and long period PP-P data. We used 3D sensitivity kernels to combine the datasets, and mantle structure was parameterized with an irregular grid. In the best-sampled region our data resolve structure on scale lengths less than 150 km. The smearing of crustal anomalies to larger depths is reduced by a crustal correction using an a priori 3D model. Our tomographic inversions reveal high-velocity roots beneath the Archean Ordos Plateau, the Sichuan Basin, and other continental blocks in SE Asia. Beneath the Himalayan Block we detect high seismic velocities, which we associate with subduction of Indian lithospheric mantle. This structure is visible above the 410 km discontinuity and may not connect to the remnant of the Neo-Tethys oceanic slab in the lower mantle. Our images suggest that only the southwestern part of the Tibetan plateau is underlain by Indian lithosphere and, thus, that the upper mantle beneath northeastern Tibet is primarily of Asian origin. Our imaging also reveals a large-scale high-velocity structure in the transition zone beneath the Yangtze Craton, which could have been produced in multiple subduction episodes. The low P-wave velocities beneath the Hainan Island are most prominent in the upper mantle and transition zone; they may represent counter flow from the surrounding subduction zones, and may not be unrelated to processes beneath eastern Tibet. 相似文献