冰雹云雷达回波自动识别系统   总被引：2，自引：0，他引：2  

段勇  贺敬安  谈曙青 《成都信息工程学院学报》2001,16(2):110-116

利用CAPPI资料对立体风暴进行识别，计算并提供出实用的风暴结构参数，采用矩心踊跃法和矩不变量法相结合对单体风暴和混合性风暴回波进行跟踪；最小二第线性外推预报；根据WSD－88D的冰雹算法，在风暴结构基础上本文建立了Windows98操作平台上冰雹识别系统，经单站1年11次强对流天气过程的资料检验，结果表明：雹云识别精度达82％。系统建立了大量人机对话框以方便用户，增加实用性及推广性。  相似文献   

Extraction and comparison of acoustic backscatter from a calibrated multi- and single-beam sonar     

Melvin  Gary D; Cochrane  Norman A; Li  Yanchao 《ICES Journal of Marine Science》2003,60(3):669-677

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动力定位系统与单波束测深仪在科考船定点作业中的应用     

张彬彬  张道建  张海泉  刘凯  张学贤  卢永平 《海洋通报》2020,39(6):651-656

科考船定点作业时会受到海洋风、涌、浪、流等外界环境因素影响，导致工作效率降低，原位测量精度下降，甚至影响作业安全。动力定位系统 （DP） 具有自动定位功能，能够抵抗外界环境因素的影响，可实现科考船高精度定点控位。 单波束测深仪不仅可以测量水深，也可反映水下设备深度信息，可以起到辅助监控水下设备功能。本文在介绍定点作业施工现状与局限性的基础上，分析 DP 系统与单波束测深仪工作原理，以“向阳红 01”船为载体，在定点作业时开启 DP 系统与单波束测深仪，发现该方法可以提高科考船定点作业工作效率、原位测量精度并保障作业安全，可为其他科考船定点作业提供参考。  相似文献   

多波束数据处理中的UTM直角坐标与经纬度坐标转换技术   总被引：1，自引：0，他引：1  

熊应乾  杜德文  姜莉莉  杨刚  吕海龙  闫仕娟 《海洋科学进展》2006,24(2):246-253

简要介绍了地图投影的一般概念,重点描述了UTM的优点及其与大地坐标之间的相互转换,该转换方法软件化后形成的技术可以为多波束数据后处理商业软件提供坐标转换的补丁技术。最后附上部分经实际检验的Fortran程序供参考。  相似文献   

海底勘查技术的最新发展   总被引：4，自引：0，他引：4  

陈卫民 《海洋技术学报》1996,15(3):25-29

本文将介绍用于探测海底三维地质特征的海底勘查的最新发展。它主要包括海底地形测绘技术，海底形貌观测技术、海底地层声学探测技术等。  相似文献   

Automatic Registration of TOBI Side-Scan Sonar and Multi-Beam Bathymetry Images for Improved Data Fusion   总被引：1，自引：0，他引：1  

Le Bas  T. P.  Mason  D. C. 《Marine Geophysical Researches》1997,19(2):163-176

Deep towed side-scan sonar vehicles such as TOBI acquire high quality imagery of the seafloor with very high spatial resolution but poor locational accuracy. Fusion of the side-scan sonar data with bathymetry data from an independent source is often desirable to reduce ambiguity in geological interpretations, to aid in slant-range correction and to enhance seafloor representation. The main obstacle to fusion is accurate registration of the two datasets.The application of hierarchical chamfer matching to the registration of TOBI side-scan sonar images and multi-beam swath bathymetry is described. This matches low level features such as edges in the TOBI image, with corresponding features in a synthetic TOBI image created by simulating the flight of the TOBI vehicle through the bathymetry. The method is completely automatic, relatively fast and robust, and much easier than manual registration. It allows accurate positioning of the TOBI vehicle, enhancing its usefulness as a research tool. The method is illustrated by automatic registration of TOBI and multi-beam bathymetry data from the Mid-Atlantic Ridge.  相似文献   

Experiments on the discrimination of fish and seabed echoes     

MacLennan  D.N.; Copland  P.J.; Armstrong  E.; Simmonds  E.J. 《ICES Journal of Marine Science》2004,61(2):201-210

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Correction method for full-depth current velocity with lowered acoustic Doppler current profiler (LADCP)   总被引：1，自引：0，他引：1  

Kanae Komaki  Masaki Kawabe 《Journal of Oceanography》2007,63(6):995-1007

A new method is presented to process and correct full-depth current velocity data obtained from a lowered acoustic Doppler current profiler (LADCP). The analysis shows that, except near the surface, the echo intensity of a reflected sound pulse is closely correlated with the magnitude of the difference in vertical shear of velocity between downcast and upcast, indicating an error in velocity shear. The present method features the use of echo intensity for the correction of velocity shear. The correction values are determined as to fit LADCP velocity to shipboard ADCP (SADCP) and LADCP bottom-tracked velocities. The method is as follows. Initially, a profile of velocity relative to the sea surface is obtained by integrating vertical shears of velocity after low-quality data are rejected. Second, the relative velocity is fitted to the velocity at 100–800 dbar measured by SADCP to obtain an “absolute” velocity profile. Third, the velocity shear is corrected using the relationship between the errors in velocity shears and echo intensity, in order to adjust the velocity at sea bottom to the bottom-tracked velocity measured by LADCP. Finally, the velocity profile is obtained from the SADCP-fitted velocity at depths less than 800 dbar and the corrected velocity shear at depths greater than 800 dbar. This method is valid for a full-depth LADCP cast throughout which the echo intensity is relatively high (greater than 75 dB in the present analysis). Although the processed velocity may include errors of 1–2 cm s⁻¹, this method produced qualitatively good current structures in the Northeast Pacific Basin that were consistent with the deep current structures inferred from silicate distribution, and the averaged velocities were significantly different from those calculated by the Visbeck (2002) method.  相似文献   

东海海底地形分区特征和成因研究   总被引：20，自引：0，他引：20  

刘忠臣  陈义兰  丁继胜  张卫红  吴永亭  郭发滨 《海洋科学进展》2003,21(2):160-173

东海一直以其特殊的大地构造地位受到国内外地学界的关注,但作为主要受构造控制的东海海底地形的研究,以往简单趋势性描述居多,专门深入系统的研究尚不多见。不久前完成的高精度、全覆盖多波束海底地形勘测覆盖了东海部分外陆架、大陆坡全部、冲绳海槽和东部岛坡的一部分,取得了海量的测深数据。据此编绘的勘测多波束水深图和结合测区外的传统资料编绘的海底地形图使我们有机会可以重新审视和系统研究东海的海底地形特征。在定量确定了陆架坡折线、陆坡坡脚线和东部槽坡坡脚线的基础上划分出了大陆架、大陆坡、冲绳海槽平原和东部岛坡4大地形区,继之对各区的海底地形特征进行了研究和描述,并在区内选取了有代表性的5条剖面进行了剖析。另外,从地球内营力和外营力两方面分析了影响东海海底地形发育的因素。调查分析表明:整个东海地形分带明显,地形类型多样:大陆架十分宽阔,总体北宽南窄,从大陆向海平缓倾斜,发育了广泛的NW-SE向沙脊群,自大陆向东南呈扇形发散;大陆坡呈NE-SW向条带展布,海底地形陡峻,呈阶梯状下掉,总体北缓南陡,其上峡谷密布,上穿切外陆架,下直达海槽,同时坡麓上海台沟谷伴生发育;冲绳海槽北浅南深,其内在平坦的背景上发育了众多的海山和海丘,其中心又有槽中槽地形;东槽坡地形复杂,发育了  相似文献   

EM120型多波束测深系统及在深海测量中的应用   总被引：1，自引：2，他引：1  

赖仲淄  方兆宝  陈金火 《海洋测绘》2006,26(2):52-54

与传统的单波束回声测深仪相比,多波束测深系统具有水深全覆盖无遗漏扫测,测量范围大、速度快,测深精度和分辨率高,记录数字化和实时自动绘图等优点。介绍了EM120型多波束测深系统深水系统的技术性能,分析了EM120在中沙深海区的测量试验情况及在深海区水深测量中的应用价值,提出了存在问题及其对策。  相似文献