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991.
992.
遗传门限自回归模型在气象时间序列预测中的应用 总被引:5,自引:2,他引:5
提出了建立门限自回归模型(TAR)的一套简便通用的方法。用基于实码的改进遗传算法,可同时优化门限值和自回归系数,解决了TAR建模过程所涉及的大量复杂寻优工作这一难题,为TAR模型在气象预测中的广泛应用提供了有力工具。实例计算的结果说明:通过门限值的控制作用,TAR模型可有效地利用气象时序资料所隐含的时序分段相依性这一重要信息,限制了模型误差,保证了TAR模型预测性能的稳健性,提高了预测精度。该方法具有通用性,在各种气象非线性时序预测中具有广泛的实用价值。 相似文献
993.
遗传算法及其在速度结构与震源联合反演中的应用 总被引:2,自引:0,他引:2
遗传算法是近年来发展较快的一种求解多参数非线性优化问题的有效方法。本文通过对遗传传算法的介绍。对该方法的发展现状及特点进行了分析,在此基础上,对遗传算法进行了改进:通过引入放大系统K。对目标函数进行压缩及扩展来提高遗传算法的搜索机制; 相似文献
994.
The main target of the present study is an objective and automated regionalization of Rayleigh wave dispersion data for the Mediterranean basin, without a priori seismotectonic constraints, and to determine the corresponding regional shear-velocity structures. The database used is formed by almost 200 Rayleigh wavetrains corresponding to 42 regional events, with surface-wave magnitude greater than 4.5, recorded at the MedNet very-broad-band stations in the Mediterranean area. Path-averaged group velocities for the Rayleigh wave fundamental mode are derived for each available epicentre-station trajectory crossing the Mediterranean basin. After this, a principal component analysis and a clustering process are applied to local group velocities, obtained for 13 different periods from 10 to 70 s, in order to classify the Mediterranean basin into several homogeneous regions. The stochastic inversion of the averaged group velocity dispersion curve obtained for each region provides the respective shear-velocity structures, down to a depth of 150–160 km. The characteristics of these areas and their possible correlation with the main seismotectonic features of the Mediterranean region are discussed. The regional models reveal significant lateral changes in the elastic structure, with the main differences concerning particularly the upper 35–40 km. Within this depth range, low shear velocities, varying from 2.8 to 3.9 km s−1, characterize the Eastern Mediterranean, whereas higher velocities, ranging from 3.0 to 4.2 km s−1, are deduced for the Western Mediterranean. These results suggest a thicker crust in the eastern part, but with a greater thickness of sedimentary layers. However, for depths of between 80 and 110 km, lower shear velocities are obtained in the Western part, while higher shear velocities are derived for the Eastern Mediterranean Sea, in the Aegean Sea, Greece, the south of Italy, Sicily and Tunisia. This velocity pattern suggests an averaged thicker lithosphere under the latter areas, as the top of the asthenosphere is detected at a mean depth of 75 km for the remaining regions. This thicker lithosphere can be related to processes associated with the convergence of the Eurasian and African plates and subduction under the Calabrian and Hellenic Arcs. 相似文献
995.
In this paper, we focused on the retrieval of the LAI in an alpine wetland located in western part of China in late August and early July 2011. A two-layer canopy reflectance model (ACRM) was used to establish the relationships between the LAI and the reflectance of near-infrared (NIR) and red (RED) wavebands. The reflectance data were derived from Landsat TM L1T product and the Terra and Aqua MODIS 16-day and 8-day composite reflectance products (MOD/MYD09) at 250 m resolution. Due to the lack of the information about some major input parameters for ACRM, which are sensitive to model outputs in the reflectance of NIR and RED wavebands, the inverse problem was ill-posed. To overcome this problem, a method of increasing the sensitivity of the LAI while reducing the influence of other model free parameters based on the study of free parameters’ sensitivity to the ACRM outputs and the region’s features was studied. The area of interest was divided into two parts using the approximately statistic normalized difference vegetation index (NDVI) value around 0.5. One part was sparse vegetation (0.1 < NDVI < 0.5), which is more sensitive to soil background effects and less sensitive to the canopy biophysical and biochemical variables. The other part was dense vegetation (0.5 ≤ NDVI < 1.0), which is less sensitive to soil background effects and more sensitive to plant canopies and leaf parameters. Then, the relationships of ρnir–LAI and ρred–LAI were established using a look-up table algorithm for the two parts. Furthermore, a regularization technique for fast pixel-wise retrieval was introduced to reduce the elements of LUT sets while maintaining a relatively high accuracy. The results were very promising compared to the field measured LAI values that the correlation (R2) of the measured LAI values and retrieved LAI values reached 0.95, and the root-mean-square deviation (RMSD) was 0.33 for late August, 2011, while the R2 reached 0.82 and RMSD was 0.25 for early July 2011. 相似文献
996.
《The Cartographic journal》2013,50(3):276-285
AbstractTraditionally schematised maps make extensive use of curves. However, automated methods for schematisation are mostly restricted to straight lines. We present a generic framework for topology-preserving curved schematisation that allows a choice of quality measures and curve types. The framework fits a curve to every part of the input. It uses Voronoi diagrams to ensure that curves fitted to disjoint parts do not intersect. The framework then employs a dynamic program to find an optimal schematisation using the fitted curves. Our fully-automated approach does not need critical points or salient features. We illustrate our framework with Bézier curves and circular arcs. 相似文献
997.
张俊东;陈秀万;李颖;罗鹏;万玮;曹艳丰 《东北测绘》2013,(2):59-62,66
基于高精度的PWVGPS与MODIS近红外三通道比值透射率间的关系建立MODIS大气可降水量新反演算法以提高反演精度。利用美国Kansas州和Oklahoma州2009年4月~9月间17期的MODIS数据和对应的SuomiNet网PWVGPS数据进行研究,发现Kaufman和Gao Bo-Cai算法反演的PWVMODIS系统性地偏低于PWVGPS,存在较大的反演误差。以高精度的PWVGPS为标准水汽值,研究PWVGPS与MODIS近红外第19波段的三通道比值透射率间的关系,建立了MODIS大气可降水量新反演算法,并利用研究区数据进行试验验证,结果表明新算法可大幅提高PWVMODIS的反演精度。 相似文献
998.
999.
极区海冰密集度AMSR-E数据反演算法的试验与验证 总被引:4,自引:2,他引:2
海冰密集度是极区海冰监测的重要参数,目前分辨率最高的微波海冰密集度产品为德国Bremen大学发布的针对AMSR-E 89 GHz频段数据利用ASI算法反演的网格数据。为实现中国极区遥感产品从无到有的战略步骤,本文针对AMSR-E 89GHz频段微波数据的ASI算法,进行了插值算法、系点值和天气滤波器一系列试验。针对北极海区,着重对影响反演结果的主要参数——纯冰和纯水的亮温极化差异阈值,即系点值(P1和P0)进行了2009年全年的统计分析。研究表明,2009年北极纯冰和纯水的代表区域P1和P0年平均值分别为10.0 K和46.67 K;2 K以上的系点值差异引起的海冰密集度差别较为显著;同样的系点值差异在不同极化差异P取值范围对海冰密集度的影响也不同。通过统计确定的系点值推算并修正了海冰密集度反演公式,对2009年全年北极海冰密集度进行了反演,并与Bremen大学产品进行了比较。继而对白令海和楚科奇海12个晴空下MODIS可见光样本数据进行反演,以验证AMSR-E冰密集度反演结果,并对误差原因进行了分析。本研究反演结果与MODIS样本比对的误差略小于Bremen大学的反演产品,空间平均误差为3.84%,空间平均绝对误差10.83%。 相似文献
1000.