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中国海洋志愿观测船现运行状态及发展 总被引:1,自引:0,他引:1
刘家沂 《海洋通报(英文版)》2009,11(1):90-96
志愿船观测是中国必须履行的国际义务。目前,中国海洋志愿观测船只呈逐年减少趋势,从过去的百余艘船只降至三、四十艘,并且从观测能力上也存在较多问题,比如观测手段比较落后、观测要素单一、观测资料缺乏。从根本上讲,志愿船运行机制缺乏有效的制度化保障,因此难以形成业务化能力,并且不能有效的履行国际义务。本文将对志愿船现运行状态及发展进行论述。 相似文献
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中国海洋环境监测系统-海洋站和志愿船观测系统的建成和使用,为继续完善和发展我国的海洋环境立体监测系统奠定了基础,使我国海洋监测站和志愿船监测业务发生了巨大变化。文章将从技术角度介绍系统的建设情况,论述系统建设产生的效益,并根据作者的理解和多年来从事的相关科研、业务工作所积累的经验,对系统业务化运行提出几点建议。 相似文献
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志愿船观测是我国必须履行的国际义务.目前,我国海洋志愿观测船只呈逐年减少趋势,从过去的百余艘船只降至三、四十艘,并且从观测能力上也存在较多问题,比如观测手段比较落后、观测要素单一、观测资料缺乏.从根本上讲,志愿船运行机制缺乏有效的制度化保障,因此难以形成业务化能力.为解决这一问题,本文对加强我国海洋志愿船观测事业发展提出一些对策建议,仅供参考. 相似文献
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发展志愿船观测获取的宝贵资料对海洋科学研究、海上交通运输安全、国防军事建设等具有非常重要的意义.志愿观测船观测要素、观测数据传输、信息管理、观测技术发展、卫星通信费用等问题一直是志愿船观测存在的几个重要问题,文章就国际志愿船观测(VOS)计划中涉及到的这几个问题的作了论述,以供我国志愿观测船能力建设参考. 相似文献
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刘家沂 《海洋与海岸带开发》2008,(2):18-22
志愿观测船作为船舶监测的组成部分.对建立海洋环境立体监测系统起到了重要的作用。志愿船观测不仅是为了获取本国海上重要天气因素用于气候服务,也是作为WMO和IOC成员国履行国际船舶航行气候服务的成员义务。文章对国际组织的志愿船管理运行和志愿船观测(VOS)计划进行了相关介绍,以利于了解有关情况。 相似文献
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在21世纪,保证经济繁荣和提高生活质量的关键是加强对环境的管理、评价和预报。要做到这一点,就必须对占地球表面71%的大洋的状况进行长期而系统的观测和预报。全球海洋观测系统(GOOS)就是在此背景下由4个国际机构发起与组织实施。发起机构为:政府间海洋学委员会(IOC)、世界气象组织、国际科学联合会理事会和联合国环境规划署。GOOS项目办公室没在巴黎IOC总部、现负责人是英国的C.P.萨默海斯博士(原英国海洋科学研究所所长)。IOC正在联合国教科文组织中为GOOS的负责人谋求一个常设岗位。 相似文献
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水下滑翔机是一种浮力驱动的无人水下自治观探测平台, 具有持续性、鲁棒性、自主性等特点, 是构建海洋观测技术体系重要的水下航行器之一。文章从水下滑翔机发展历程、运行方式和专用传感器展开, 基于国内外海洋学文献综述研究, 重点对水下滑翔机在典型海洋现象观测应用方面进行总结。水下滑翔机的运行稳定性、长时续, 观测高分辨率、低成本的特点, 满足了对海洋中尺度涡、内波、湍流、环流/边界流和锋面的长时间、精细化立体观测要求; 鲁棒性、自主性的特点使其能够适应台风过境、地震、原油泄漏前后等紧急恶劣海洋状况的监测; 运行平稳、低噪声的特点使其成为声学监测与探测的良好平台。对比分析国内外的水下滑翔机(组网)应用状况可以发现, 国内水下滑翔机在传感器、数据处理和组网技术方面都需要进一步完善。最后总结并展望了国内外水下滑翔机面向海洋现象观测的应用。 相似文献
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孔压探杆贯入及潮汐作用下超孔压响应规律研究 总被引:1,自引:0,他引:1
Excess pore water pressure is an important parameter that can be used to analyze certain physical characteristics of sediment. In this paper, the excess pore water pressure of subseafloor sediment and its variation with tidal movement was measured following the installation of a wharf in Qingdao, China by using a fiber Bragg grating(FBG) piezometer. The results indicated that this FBG piezometer is effective in the field. The measured variation of excess pore water pressure after installation is largely explained by the dissipation of excess pore water pressure. The dissipation rate can be used to estimate the horizontal consolidation coefficient, which ranged from1.3×10~(–6) m~2/s to 8.1×10~(–6) m~2/s. The measured values during tidal phases are associated with the variability of tidal pressure on the seafloor and can be used to estimate the compressibility and the permeability of the sediment during tidal movement. The volume compression coefficient estimated from tidal oscillation was approximately2.0×10~(–11) Pa~(–1), which was consistent with the data from the laboratory test. The findings of this paper can provide useful information for in situ investigations of subseafloor sediment. 相似文献
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Sea ice drift is mainly controlled by ocean currents, local wind, and internal ice stress. Information on sea ice motion, especially in situ synchronous observation of an ice velocity, a current velocity, and a wind speed, is of great significance to identify ice drift characteristics. A sea ice substitute, the so-called "modelled ice", which is made by polypropylene material with a density similar to Bohai Sea ice, is used to complete a free drift experiment in the open sea. The trajectories of isolated modelled ice, currents and wind in the Bohai Sea during non-frozen and frozen periods are obtained. The results show that the currents play a major role while the wind plays a minor role in the free drift of isolated modelled ice when the wind is mild in the Bohai Sea. The modelled ice drift is significantly affected by the ocean current and wind based on the ice–current–wind relationship established by a multiple linear regression. The modelled ice velocity calculated by the multiple linear regression is close to that of the in situ observation, the magnitude of the error between the calculated and observed ice velocities is less than12.05%, and the velocity direction error is less than 6.21°. Thus, the ice velocity can be estimated based on the observed current velocity and wind speed when the in situ observed ice velocity is missing. And the modelled ice of same thickness with a smaller density is more sensitive to the current velocity and the wind speed changes. In addition, the modelled ice drift characteristics are shown to be close to those of the real sea ice, which indicates that the modelled ice can be used as a good substitute of real ice for in situ observation of the free ice drift in the open sea, which helps solve time availability, safety and logistics problems related to in situ observation on real ice. 相似文献
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通过构建海域无人机监视监测业务流程形式化模型,为海域无人机监控与管理系统能够自适应可变的业务流程奠定基础。首先对比了各种业务流程建模方法的技术特点和适用场景,然后对海域无人机监视监测业务流程进行分析,提出了一种UML活动图转化为基于Petri网的工作流逻辑偶的方法,最后基于此方法对海域无人机监视监测业务流程进行建模。建模结果表明,该方法能有效地将海域无人机监视监测业务流程的分支、分叉以及汇合等流程逻辑转化为工作流逻辑偶,并且转化的结果满足良序性、良构性以及畅通性。 相似文献
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海洋酸化对马氏珠母贝受精及早期发育的影响 总被引:1,自引:0,他引:1
自2010年7月1日至3日,在pH值为8.1、7.7和7.4条件下研究了海洋酸化对马氏珠母贝(Pinctada martensii Dunker)受精及早期发育的影响。结果显示,海洋酸化对不同pH值下马氏珠母贝的受精率无显著影响。pH8.1、pH 7.7和pH 7.4试验组幼虫的壳长、壳高的值逐渐增大,pH 8.1组幼虫的壳长、壳高的值大于同期其他两组的值,且在实验的第24、36、48小时与其他两组同期幼虫的壳长、壳高的值差异显著,这表明海洋酸化显著影响马氏珠母贝幼虫的生长。实验期间,pH 8.1试验组幼虫的存活率和畸形率没有显著变化,而pH 7.7和pH 7.4组幼虫的存活率显著低于pH 8.1组。pH 7.4组幼虫的畸形率显著高于同期pH 8.1和pH 7.7组幼虫的畸形率,表明在海洋酸化的环境中幼虫的发育受到影响。本文将为海洋酸化的相关研究提供基础数据。 相似文献
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Reconstruction of incomplete oceanographic data sets using empirical orthogonal functions: application to the Adriatic Sea surface temperature 总被引:8,自引:1,他引:8
A method for the reconstruction of missing data based on an EOF decomposition has been applied to a large data set, a test case of Sea Surface Temperature satellite images of the Adriatic Sea. The EOF decomposition is realised with a Lanczos method, which allows optimising computational time for large matrices. The results show that the reconstruction method leads to accurate reconstructions as well as a low cpu time when dealing with realistic cases. The method has been tested with different amounts of missing data, artificially adding clouds ranging from 40% to 80% of data loss, and then compared to the same data set with no missing data. A comparison with in situ data has also been made. These validation studies show that results are robust, even when the amount of missing data is very high. The reconstruction of the data from the Adriatic Sea shows realistic features and a reliable temperature distribution. In addition, the method is compared to an Optimal Interpolation reconstruction. The results obtained with both methods are very similar. The main difference is the computational time, which is reduced nearly 30 times with the method presented here. Once the reconstruction has been performed, the EOF decomposition is analysed to show the method’s reliability, and a cold event on the Albanian coast is studied. The reconstructed data reflect the effect of wind on the Albanian coast, that led to a cold-water episode in this zone for a 6-day period. 相似文献