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针对海洋表面SAR影像的特点，采用基于灰度共生矩阵的纹理特征方法是提取海面溢油信息的常用方法，但实际海洋表面复杂的信息使得SAR图像上产生类似溢油现象的暗斑区域，这导致在利用纹理特征方法提取溢油信息时存在虚警率，降低了溢油信息的提取精度。基于RADARSAT-2 SAR四极化影像，本文提出基于SAR极化比影像的纹理特征识别方法对海面油膜进行识别提取。结果显示，基于SAR极化比影像的纹理特征识别方法可以有效且准确地提取海面溢油信息，相比于VV极化影像的纹理特征识别方法，溢油监测过程中的虚警率降低了17.96%，溢油监测总体精度达到96.83%。 相似文献
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准确提取海水筏式养殖区信息对于海洋资源管理和环境监测具有重要意义,但是筏式养殖区养殖筏因淹没于水中常出现数据弱信号区域的现象,导致仅凭光学影像提取精度较低。因此,本文以威海荣成湾为研究区域,通过添加通道注意力机制改进U-Net神经网络并结合高分2号光学影像光谱信息以及高分3号雷达影像纹理信息,尝试提高筏式养殖区提取精度。结果表明：（1）无论是对于单一的光学影像还是光学和雷达影像融合影像,添加通道注意力机制的U-Net神经网络预测结果总体精度都会提高,提高幅度在2.21%～4.12%之间。（2）利用改进后的U-Net神经网络处理融合数据,总体精度达到95.75%,相对于仅用高分2号影像的精度高4.3%;(3)对于弱信号区域,利用改进网络以及融合数据提取的总体精度和Kappa系数分别为91.61%和0.827 7。该方法可以对海洋筏式养殖区弱信号区域进行有效提取,能够为海洋养殖面积统计以及海洋环境检测提供技术支持。 相似文献
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20世纪40年代以来多时相中国大陆岸线提取方法及精度评估 总被引：8，自引：2，他引：6
将大陆岸线分为自然岸线、人工岸线2大类以及11个二级类,基于地形图与遥感影像,结合野外考察工作建立详细的技术规范,提取20世纪40年代以来6个时相的中国大陆海岸线;针对提取的结果,应用直接对比法计算实际误差,基于地图学和遥感信息提取的理论计算"理论最大允许误差",二者对比表明:基于多源数据提取多时相岸线的技术方案可行,多时相岸线的实际误差均远远低于"理论最大允许误差",精度较优;基于地形图提取的20世纪40年代和60年代时相岸线,精度总体上低于基于30 m分辨率遥感影像提取的多时相岸线,而且20世纪60年代时相受多源数据融合的影响而精度最低;基于环境与灾害监测预报小卫星CCD数据提取岸线,受影像畸变和几何纠正精度的影响,精度略低于基于Landsat影像提取的结果,但同样基于Landsat影像提取的岸线,新近时相的精度明显优于早期时相。本研究可为岸线变化研究以及海岸带综合管理等提供有力的支持。 相似文献
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针对卫星遥感技术在对滨海湿地互花米草监测时受分辨率、气候条件等多种因素限制存在一定局限性且通过单一的影像数据提取互花米草时精度不稳定的问题,提出了基于无人机点云与影像融合的面向对象互花米草提取方法。以黄河三角洲自然保护区为研究对象,获取了该区域的点云和多光谱影像。先将地面滤波后提取的植被点云与多光谱影像进行特征组合优化,然后对融合影像采用FNEA算法进行多尺度分割后采用基于改进的最近邻算法进行面向对象分类,最终得到的互花米草生产者精度和用户精度分别达到了82.53%和86.43%,较未融合点云的提取精度分别提高了22.34%和7.66%,分类结果的总体精度从89.54%提升至92.61%,且融合点云后影像能够有效区分两种生长状态的互花米草,表明本文提出的方法能够有效提高互花米草的提取精度。 相似文献
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针对单纯依靠光谱特征油膜提取精度低、雷达影像油膜提取易受海况条件及假目标影响的问题,提出了一种结合光
谱特征与纹理特征的多光谱遥感影像油膜信息提取方法。以2011 年6 月蓬莱19-3 油田溢油事故为研究对象,选用HJ-1 星
CCD 遥感数据,利用灰度共生矩阵获取影像纹理特征,采用SVM 模型对结合纹理特征与光谱特征的影像进行分类,提取出
研究区油膜信息,并将分类提取结果与仅依靠光谱特征的SVM 模型分类结果进行了比较。结果表明：引入纹理特征的SVM
模型分类总精度达到90.29 %,比仅依靠光谱特征的分类精度提高了12.41 %;纹理特征的参与降低了原影像噪声对分类结果
的影响,油膜边缘提取更加清晰,油膜中心呈连续面状分布,引入纹理特征的SVM 模型可有效地用于多光谱遥感影像海面
油膜信息提取。 相似文献
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提出基于遥感的影像图和DEM影像图,进行海图地形和DEM等高线数据数字化提取并将提取结果导出到其他GIS系统中的新技术方法。该技术处理速度快,生成的影像图和提取地形数据具有精度高(可达到1 m)的特点。这项新的处理技术可达到提高实际测绘中的劳动效率,降低外业测量人员的野外工作强度,及时更新地理信息、简便地校验测量的质量精度和节省作业经费的目的。 相似文献
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Arne Schnack-Friedrichsen Angela M. Davis Jim D. Bennell Dei G. Huws 《Marine Georesources & Geotechnology》2001,19(4):221-243
The interdependence between the seismo-acoustic properties of a marine sediment and its geotechnical/physical parameters has been known for many years, and it has been postulated that this should allow the extraction of geotechnical information from seismic data. Though in the literature many correlations have been published for the surficial layer, there is a lack of information for greater sediment depths. In this article, a desktop study on a synthetic seafloor model illustrates how the application of published near-surface prediction equations to subsurface sediments (up to several tens of meters burial depth) can lead to spurious predictions. To test this further, acoustic and geotechnical properties were measured on a number of sediment core samples, some of which were subjected to loading in acoustically-equipped consolidation cells (oedometers) to simulate greater burial depth conditions. For low effective pressures (representing small burial depths extending to around 10 meters subsurface), the general applicability of established relationships was confirmed: the prediction of porosity, bulk density, and mean grain size from acoustic velocity and impedance appears generally possible for the investigated sedimentary environments. As effective pressure increases through, the observed relationships deviate more and more from the established ones for the near-surface area. For the samples tested in this study, in some instances increasing pressure even resulted in decreasing velocities. There are several possible explanations for this abnormal behavior, including the presence of gas, overconsolidation, or bimodal grain size distribution. The results indicate that an appropriate depth correction must be introduced into the published prediction equations in order to obtain reliable estimates of physical sediment properties for greater subsurface depths. 相似文献
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Shigehisa Nakamura 《Marine Geodesy》2000,23(1):55-61
Specific properties of the interannual sea level variations and annual tides in the Northwestern Pacific were studied. Several tide stations were monitored. The monthly mean sea level for the year of 1995 was analyzed at each tide station. A seismic event in 1995, some tectonic activity around the subject area, and the Kuroshio (the oceanic western boundary current) may possibly contaminate results which would have occurred from the astronomical annual tide alone. 相似文献
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The effect of different fixation and storage protocols on the flow cytometric (FCM) simultaneous analysis of bacterioplankton and phytoplankton in coastal seawater samples (Mediterranean coastal lagoons) was investigated. FCM measurements (cell number, fluorescence and scatter characteristics) were obtained through DAPI staining. Three fixatives [glutaraldehyde (GA), formaldehyde (FA) and paraformaldehyde (PFA)] and two storage (3 months duration) methods (5 °C and −196 °C) were tested. Two dominant populations were detected in studied samples: bacteria and eukaryotic picophytoplankton. Adding fixatives (2% final concentration) appears necessary to obtain FCM exhaustive counts of all the bacteria and phytoplanktonic cells. This was related to the permeation effect of fixatives which allowed a better DAPI staining of the cells. Maximum fluorescence, i.e. optimal staining of the cells was obtained with FA or PFA, and significant lower fluorescences with GA. Fixed samples stored at 5 °C induced rapid cell loss. Only storage in liquid nitrogen of samples fixed with FA or PFA, allows mid-term (≥4 months) preservation of bacteria or picophytoplankton cell numbers, and limited evolution of DAPI-induced fluorescence and scatter characteristics. 相似文献
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《海洋学报(英文版)》2014,(9):F0003-F0003
<正>Acta Oceanologica Sinica(AOS)is a comprehensive academic journal edited by the Editorial Committee of Acta Oceanologica Sinica and is designed to provide a forum for important research papers of the marine scientific community which reflect the information on a worldwide basis.The journal publishes scholarly papers on marine science and technology,including physics,chemistry,biology, 相似文献
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The relationship between the flux of exotic benthic foraminiferal tests (i.e. tests which are supplied from open-sea sources alone) in a tidal inlet and that of bulk sediment was analysed, which can be expressed as two first-order linear equations. According to this relationship, in order to determine net sediment transport directions in the entrance, the test concentration in surficial sediments of the tidal basin can be compared against a ‘ critical level ’. The critical level is determined for the conditions that no net transport of bulk sediment is present within the entrance. If the observed concentration (averaged over the tidal basin) is higher than the simulated critical level, then the net sediment transport is directed to landward. This method is applied to the analysis of net sand transport at Christchurch Harbour, a tidal inlet system located in southern England. In this investigation, concentrations of exotic foraminiferal tests in the surficial sediments of the tidal basin and ebb tidal delta area were obtained from the analysis of sea-bed sediment samples. A series of probable critical levels were calculated based upon the data sets with regard to: (1) sediment discharge from the rivers; (2) magnitude of sediment discharge within the entrance during the ebb; (3) the test concentration outside the harbour; (4) the thickness of the moving layer; and (5) two parameters associated with dispersive processes. The results show that the concentration in the tidal basin sediment is higher than a number of simulated critical concentrations for representative cases. Consequently, the high level of the concentration of exotic benthic foraminiferal tests within the harbour should be explained as a result of landward net transport of sands within the entrance. 相似文献
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Coastal inundation associated with extreme sea levels is the main factor which leads to the loss of life and property whenever a severe tropical cyclonic storm hits the Indian coasts. The Andhra and Orissa coasts are most vulnerable for coastal inundation due to extreme rise in sea levels associated with tropical cyclones. Loss of life may be minimized if extreme sea levels and associated coastal flooding is predicted well in advance. Keeping this in view, location specific coastal inundation models are developed and applied for the Andhra and Orissa coasts of India. Several numerical experiments are carried out using the data of past severe cyclones that struck these regions. The simulated inland inundation distances are found to be in general agreement with the reported flooding. 相似文献
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Hoi-Soo Jung Kap-Sik Jeong Yong-Shik Chu Sung-Hyun Park Ki-Hyune Kim 《Marine Georesources & Geotechnology》2001,19(3):181-195
Grain size and water content in box-core sediments from the Clarion-Clipperton fracture zone (C-C zone) in the northeast equatorial Pacific were analyzed in detail to understand the downcore variations across a hiatus between Quaternary and Tertiary layers. Grain-size distributions in the topmost core sediments show two modes: a coarse mode (peaked at 50 μm) and a fine mode (at 2-25 μm). The coarse mode disappears gradually with depth accompanied by the dissolution of siliceous fossil tests, whereas the fine mode coarsens due to the formation of authigenic minerals. Water content increases abruptly across a color boundary between an upper pale brown layer and a lower dark brown layer that is the hiatus between Quaternary and Tertiary layers. Abundant smectites and microvoid molds, which are created by the prolonged fossil dissolution in the underlying sediment, are attributed for the abrupt downcore variation of water content. Overall variations in grain size and water content in the topmost core sediments in the western C-C zone are possibly constrained by the dissolution of biogenic siliceous fossils. Variations in geotechnical properties related to these changes must be considered in the design of nodule collectors. 相似文献
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Shigehisa Nakamura 《Marine Geodesy》2001,24(1):27-33
This article concerns an interrelation between the sea levels and the western boundary flow near a tectonic boundary in a local zone in the Northwestern Pacific. In this zone, sea level variations at stations located on the coast facing the Pacific are studied to find the interrelation between variations of the Kurosio flow as an index of the distance of the flow axis off a specific coast. The result is discussed after data processing of the monthly means of the sea levels, and a notice is taken of variations caused by active crustal upheavals during a seismic event, a local earthquake. 相似文献