共查询到18条相似文献，搜索用时 500 毫秒
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水深是反映海底地形地貌的最基础要素,对缺失的水深点进行准确的插值能帮助有效地表达海底地形地貌起伏形态。针对海底地形变化复杂的区域,传统的反距离加权插值法存在只考虑样本水深点与待插值水深点之间的距离,而忽略了样本水深点之间的空间相关性的问题。本文提出了一种顾及特征水深点距离重分配的反距离加权插值算法。该算法首先对离散的水深点构建特征水深线,在特征水深线的基础上,提取特征水深线上的特征点作为特征水深点;然后在所有样本水深点到待插值水深点距离之和不变的约束下,提出距离重分配的量化指标;最后构造出一个顾及特征水深点距离重分配的IDW插值算法模型。实验结果表明,在海底地形变化复杂的区域,顾及特征水深点距离重分配的反距离加权插值算法与传统的IDW、自然邻域插值、样条函数插值算法等相比,能有效提高水深点的插值精准度。 相似文献
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为了客观准确地反映辽东湾海域沉积物中石油类含量的空间分布特征,文中基于GIS的地统计分析模块,对2015年辽东湾海域沉积物石油类调查数据进行探索性数据分析,分别运用反距离权重法、普通克里金法、规则样条函数法和张力样条函数法进行空间插值,采用交叉检验方法对插值精度进行了评估。结果表明:插值精度张力样条函数法规则样条函数法反距离权重法普通克里金法,整体上4种插值方法均能客观地模拟出沉积物石油类含量的空间分布趋势。在局部区域,张力样条函数法插值预测结果更接近真实测量值。辽东湾海域沉积物石油类宜采用张力样条函数法进行空间插值。 相似文献
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空间插值在海洋环境评价中有着广泛的应用,常用的插值方法有:线性插值、最近邻点插值、自然邻点插值、三次多项式插值、反距离权重插值、克里金插值等。盐度是海水重要的环境因子,基于2012年8月份的北海区盐度监测数据,采用空间插值分析表层盐度分布,并通过开展不同插值方法的插值实验,对插值结果进行曲面分析和误差分析,对比各插值方法的特点与适用性。结果显示:基于本次海洋环境监测的站位与盐度数据,克里金插值、自然邻点插值曲面趋势符合较好,而且相对其他插值方法误差也较小,是相对适用于海水盐度的空间插值方法。 相似文献
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以三次Ｈｅｒｍｉｔｅ插值函数和另二类初等形式的函数为基础所构造的一种混合型分段插值函数进行海洋资料整理中的插值和绘线处理。结果更加合理，特别对具有累加或统计性质的数据，不但给出光滑的插值函数及其图形，而且还能给出大部分光滑的导函数图形。本文同时介绍了大有可为方法在不同专业领域中的一些应用实例。 相似文献
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为建立一个高精度、高空间分辨率的逐日气温格点数据集,满足公共气象服务对于精确信息及实时信息的需要,利用2018年6—8月京津冀区域以及临近省区共3 974个国家级及区域气象观测站质控后的逐日气温资料,采用ANUSPLIN软件对逐日气温数据进行空间内插,得到了京津冀区域逐日气温格点数据集(0.01°×0.01°),并分别利用反距离权重插值法、普通克里金插值法、样条函数法对逐日气温数据进行空间插值,采用相关系数(Corr)、平均绝对误差(MAE)、平均相对误差(MRE)等作为评估指标来检验插值精度。结果表明:1) ANUSPLIN软件满足了空间插值对精度及曲面平滑度的要求,能直观体现京津冀区域气温由北向南递增的空间分布特征; 2) 4种插值方法中,基于ANUSPLIN软件的插值结果最优,相关系数平均达0.97,其样本误差在1℃之内占比为90.59%,MAE为0.46℃,MRE为1.81%; 3)插值误差较大的区域位于冀北高原、燕山丘陵及太行山脉一带,高海拔、低站点密度等是造成插值误差的主要原因。基于ANUSPLIN插值方法建立的逐日气温格点数据集具有分辨率高、空间插值误差小的优势,ANUSPLIN对气温的空间分布具有较好的预测能力。 相似文献
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利用插值试验分析采样网格对粒度趋势分析的影响 总被引：10，自引：0，他引：10
利用地理信息系统软件ArcView3．2的空间分析功能，采用三次样条插值方法，对采自山东半岛月湖的表层沉积物的粒度参数进行插值。应用“粒度趋势分析”方法，选取一系列的特征距离值进行试验，从原始数据和插值后数据中提取净输运方向的信息。结果显示，原始的不规则采样点所得粒度趋势对于特征距离的选择很敏感，而插值后的规则格网在不同的特征距离下均表现出比较统一的粒度趋势信息。研究表明，规则格网较不规则格网采样点有许多优势，应用插值方法可有效地提高原始数据的信息含量及其质量。 相似文献
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为充分发挥监测数据的作用,进而科学评价海洋环境和促进生态修复,文章分别采用ArcGIS的普通克里金法、反距离权重法和含障碍的样条函数3种插值方法,对2017年11月镇海湾海水无机氮监测数据进行插值分析,并通过插值结果比对选出最优方案。研究结果表明:通过对照点监测数据的验证,含障碍的样条函数的插值结果相对误差较小,比普通克里金法和反距离权重法更适用于海岸线复杂和岛屿众多的监测区域;根据含障碍的样条函数的插值结果制作镇海湾海水无机氮浓度空间分布图,并应用属性数据计算海水无机氮各类水质面积,与相关公报结论相符;合理采用ArcGIS插值方法对监测数据进行制图和计算,水质评价结果直观、可靠且具有应用价值。 相似文献
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With Shannon sampling rates at the sensors of a linear antenna, it is not always possible to achieve a beam system with complete azimuth coverage. Furthermore, it is not possible to compensate an antenna system platform's own motion in such a way as to be able to build up a beam system fixed in space. Even the method of increasing the sampling rate for the sensors to an impracticably high value would only solve these problems to a limited extent. On the other hand, a solution which is easily put into practice is offered by time interpolation between adjacent sample points of the sensor signals. Therefore we have investigated this method in detail. The beam patterns are formed by special linear combination of the autocorrelation function (ACF) of the sensor signals. This kind of linear combination is applicable to all types of interpolation between adjacent sample points. For one special type of interpolation, namely linear interpolation, an azimuthal level-distribution function which specifies the maximum antenna reception sensitivity for all steering angles is stated for a linear antenna havingN sensors. With this function, it is possible to estimate the influence of the sampling frequency, Signal center frequency, signal bandwidth, and antenna dimensions on the antenna/beamformer performance. 相似文献
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提出并实现了基于遥感技术和多站点潮位插值的淤泥质海岸线推算方案。利用多时相遥感影像提取出人工岸线和瞬时水边线,在控制站点潮汐调和分析的基础上,利用潮汐线性分带插值校正处理,赋予水边线离散点在影像成像时刻的实际潮位,进而根据三角函数相似性原理推算出岸滩的平均坡度和平均大潮高潮点位置,连接形成自然岸线,最终根据自然岸线与人工岸线合成得到海岸线的空间分布。实践应用证明,该方案得到的海岸线与现场测定的平均大潮高潮痕迹点相吻合,可为快速确定淤泥质海岸岸线,监测岸滩资源的空间变化提供方法与数据支撑。 相似文献
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A. V. Grigor'ev 《Physical Oceanography》1993,4(6):471-477
The results of numerical experiments involving data assimilation by a non-linear model for synoptic dynamics of the ocean are given. The results of application of simplified optimal filtration algorithms (with the correlation error function being parametrized for both linear and non-linear variants) and of the optimal interpolation are intercompared. The use of a non-linear equation to predict average values and a linear one to predict dispersion in the filtration algorithm is suggested as most appropriate for the cases, when anisotropy of the correlation function is to be included. In other cases, it is considered worth-while to apply optimal interpolation.Translated by V. Puchkin. 相似文献
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This paper is concerned with the application of active contour methods to unsupervised binary segmentation of high-resolution sonar images. First, texture features are extracted from a sidescan image containing two distinct regions. A region-based active contour model of Chan et al. [J. Vis. Commun. Image represent, vol. 11, pp. 130-141,2000] is then applied to the vector-valued image extracted from the original data. Our implementation includes a new automatic feature selection step used to readjust the weights attached to each feature in the curve evolution equation that drives the segmentation. Results are shown on simulated and real data. The influence of the algorithm parameters and contour initialization are also analyzed. 相似文献
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海温场的递归滤波分析 总被引：1，自引：0，他引：1
递归滤波(RF)是一种属于经验线性插值类的客观分析方法。因其处理边界域和背景场的独特能力以及在计算机处理上的快速便捷优于其他的传统分析方法,适合于分析诸多资料量大(如卫星资料)、不同来源的不均匀资料。本文主要发展这一客观分析方法在海温场分析上的应用。综合利用各种时空分布和精确度均不相同的海温资料,对几个基本参数的取法进行调试并选取适当的值,分析得出细网格的海温场。结果表明,递归滤波方法不仅灵活简便,而且分析出的海温场质量好,基本上可以反映海温的实际情形。对海温场的分析还可为其他从卫星等提取的非常规资料分析提供借鉴。 相似文献
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This article evaluates different spatial interpolation methods for mapping submerged aquatic vegetation (SAV) in the Caloosahatchee Estuary, Florida. Data used for interpolation were collected by the Submersed Aquatic Vegetation Early Warning System (SAVEWS). The system consists of hydro-acoustic equipment, which operates from a slow-moving boat and records bottom depth, seagrass height, and seagrass density. This information is coupled with geographic location coordinates from a Global Positioning System (GPS) and stored together in digital files, representing SAV status at points along transect lines. Adequate spatial interpolation is needed to present the SAV information, including density, height, and water depth, as spatially continuous data for mapping and for comparison between seasons and years. Interpolation methods examined in this study include ordinary kriging with five different semivariance models combined with a variable number of neighboring points, the inverse distance weighted (IDW) method with different parameters, and the triangulated irregular network (TIN) method with linear and quintic options. Interpolation results were compared with survey data at selected calibration transects to examine the suitability of different interpolation methods. Suitability was quantified by the determination coefficient (R2) and the root-mean-square error (RMSE) between interpolated and observed values. The most suitable interpolation method was identified as the one yielding the highest R2 value and/or the lowest RMSE value. For different geographic conditions, seasons, and SAV parameters, different interpolation methods were recommended. This study identified that kriging was more suitable than the IDW or TIN method for spatial interpolation of all SAV parameters measured. It also suggested that transect data with irregular spatial distribution patterns such as SAV parameters are sensitive to interpolation methods. An inappropriate interpolation method such as TIN can lead to erroneous spatial representation of the SAV status. With a functional geographic system and adequate computing power, the evaluation and selection of interpolation methods can be automated and quantitative, leading to a more efficient and accurate decision. 相似文献