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海洋传感观测服务柔性开发技术研究 总被引：1，自引：0，他引：1
海洋传感观测服务能够实现多个海洋观测系统间的数据共享与集成,支持大范围、多学科的海洋科学研究。在软件开发过程中,由于不同观测系统的数据库异构互异,导致传感器观测服务软件难以复用,开发效率低。本文针对数据库结构的相似性进行分析,提出海洋传感观测服务的柔性开发模型,设计可适配于异构数据库的服务构件。该构件通过配置观测数据在具体数据库的存储结构,实现了数据库结构向服务模式定义的映射;服务构件根据配置信息生成数据库查询语句,实现观测数据的自动提取,避免了数据库异构导致的重复开发的问题。通过将服务构件应用在实际开发中,验证了该模型的有效性与可行性。 相似文献
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海洋环境信息建设是实现"认知海洋"、"透明海洋"、"智能海洋"的基础,从分散海洋环境信息海量数据采集、异构海洋环境信息的高效数据存储、基于节点动态性能的海量海洋环境信息数据处理与分析任务分配、基于人工智能的定向功能的辅助决策等四个方面,探讨了基于Hadoop技术的海洋环境信息分布式架构设计方法,实现将海量、多源、异构、多时空、动态的海洋环境信息进行高效、高质、及时、快速的采集、传输、存储、处理、分析及智能化应用,以全面提升海洋环境自主信息感知获取、融合处理和应急保障能力。 相似文献
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海洋观测预报数据信息是地方经济建设和社会发展重要基础数据之一,由于其数据源与信息源分布于多个不同网络中,且存储与展示形式各异,一直难以被统一集成和很好地应用。从分析海洋观测预报业务数据源与信息源入手,应用目前成熟的网络技术和数据库技术,对海洋观测预报数据信息集成中的若干问题进行深入研究,从而提出并实践了从网络集成、数据集成、知识集成到应用集成的一整套海洋观测预报数据集成的技术框架和方法体系,继而开展基于多源异构数据与信息集成的海洋观测预报服务系统研究,为海洋观测预报数据信息集成的实践过程提供方法支持。 相似文献
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由于物联网(Internet of Thigs,IoT)各领域中应用系统的分散开发和引进,形成了海量的以数据库形式存在的"信息孤岛",传统互联的数据转换系统开发效率及代码重复利用率低下,无法满足新的互联需求。针对以上问题,本文提出了一种面向物联网的异构数据转换模型(IoT-oriented Data Conversion Model,IDCM)。该模型主要由模式匹配器、数据转换器和状态监控器组成。首先,通过引用模式匹配器,实现对异构数据库的自动模式匹配,提高了模式匹配效率。其次,利用数据转换器,调用模式匹配结果,实现动态自适应,提高了代码利用率。然后,通过运行状态监控器的使用,实现了数据转换器统一的集成管理。最后,我们对该模型在家电测试及海洋观测领域的互联项目中进行了实际验证。结果表明,IDCM模型有效、可行,对促进物联网异构数据的转换具有重要的作用。 相似文献
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近年来,在海洋灾害预测、预报等海洋信息产品的开发中,对准确、大量、连续、实时的海洋要素监测数据的依赖性日趋增强。同时,由于海洋数据的复杂性,数据来源的多源性,数据平台异构,数据格式不规范等原因,增大了数据集成的难度,降低了数据使用的效率。文章提出了用XML作为传输媒介,结合Socket网络通信技术,建立实时海洋数据传输网络系统,实现了海洋数据集成与交换格式的统一,屏蔽了影响海洋数据集成和使用效率的因素。文章对XML在海洋信息产品开发中的应用做出了有益的探索和尝试,旨在促进XML在我国海洋信息领域的应用。 相似文献
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海洋数据是国家重要的基础性战略资源,海洋大数据融合应用发展对于实施海洋强国战略意义重大。本文从数据、技术和应用3个角度分析归纳了海洋大数据的内涵、外延和特征,提出了低质性、碎片化和隐匿性3个海洋大数据要解决的关键问题。从海洋大数据资源体系、海洋信息通信网、海洋大数据处理分析、海洋大数据存储管理和共享服务,以及海洋大数据应用研发等方面总结了海洋大数据发展能力现状和趋势,探讨了当前国家海洋大数据中心发展需求,架构海洋大数据国内外总体布局,从数据资源、关键技术、共享服务、开放创新、融合应用和国际合作等6个方面,研究提出海洋大数据重点发展方向,以期为国家、行业和地方海洋大数据发展提供参考。 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