河豚毒素的微生物起源

河豚毒素（TTX）是一种毒性很强的海洋生物活性物质，为典型的神经Na^＋通道阻断剂。最初从纯科（Tetrodontidae）鱼中发现，故被Tahara命名为Tetrodotoxin（TTX）。TTX的分子结构为氨基全氢喹唑啉化合物，分子式C11H17N3O8，相对分子质量为319，该分子中含有原酸酯结构，几乎所有的碳原子均具不对称取代。它微溶于水和浓酸，极易溶于含醋酸的水溶液，不溶于有机溶剂，纯品为无嗅无色针状固体结晶，易被碱还原。TTX非常稳定，在日光下曝晒20d或在盐水中盐腌30d，其毒性仍不能被全部破坏，只有在高温加热30min以上或在碱性条件下才能被分解。其具有胍基是TTX的活性部位，通过它TTX可特异地结合于神经细胞膜钠通道上，进而抑制Na^＋内流，阻断神经兴奋的传导。     

ActiveX技术在海洋资料自动采集系统研制中的应用

本文结合实例介绍了的 Active X控件的编程技术及其在水文气象数据采集系统研制中的应用     

黄海、渤海水温垂直结构数值预报方法研究 Ⅱ．准三维数值预报模式

本文根据黄渤海海区水温资料建立了无维深度η和无维温度θＴ以及相应的水温垂直剖面的相似函数θＴ＝ｆ（η）。在此基础上，设：上均匀层厚度ｈ＝ｈ（ｘ，ｙ，ｔ）、表层水温ＴＳ＝ＴＳ（ｘ，ｙ，ｔ）、上均匀层以下的温度ＴＺ＝ＹＺ（ＹＺ（ｘ，ｙ，ｚ，）、底层温度ＴＨ＝（ｘ，ｙ，ｔ）、流速分量ｕ＝ｕ（ｘ，ｙ，ｔ）和ｖ＝ｖ（ｘ，ｙ，ｔ）及海面起伏ξ＝ξ（ｘ，ｙ，ｔ），提出了水温垂直结构的准三维数值预报模式。模式的求解是用“ＡＤＩ”和“ＨＮ”法进行。文中引列了预报时效为４ｄ的试报结果，效果是令人满意的。     

海南省临高县调楼乡黄龙港北侧围海工程的自然条件可行性分析

在野外调查的基础上，收集了围填工程海域的气象、水文、地质资料，详细论述了围填区的水动力条件、地质地貌与泥沙运动情况，分析了围填工程对周边设施的影响，得出了围填工程在自然条件下可行的结论。     

单胞藻薄膜袋封闭式培养技术的研究

本文提出了用聚乙烯薄膜透明袋对单胞藻进行封闭式培养技术的研究结果。用该技术培养单胞藻作海产动物幼体的饵料,与目前通用的水泥池开放式培养比较,具有方法简单成本低廉、培养的单胞藻密度高、不易污染、生产周期短等优点。该技术在1988年的扇贝人工育苗生产中,提高了投饵质量和幼虫的成活率。     

Design and Implementation of the Hydrographic Production and Management Information System (HYPAMIS)

With the development of hydrographic work and information techniques, the traditional work mode is not suitable for the Chinese Marine Safety Administration Bureau (CMSAB). Aiming at the separation of charts production and management, a new idea that is the integration of production, management, and quality control is presented. Geographic Information System (GIS), Management Information System (MIS), Office Automation (OA) and Spatial Database Management (SDM) advanced techniques are introduced into the workflows in CMSAB. To realize information sharing, a mixed mode with Browser/Server (B/S) mode and Client/Serve (C/S) mode are adopted. Based on the above ideas and strategies, an integrated system named Hydrographic Production And Management Information System (HYPAMIS) was developed. The whole workflow and three subworkflows including survey management workflow, production workflow, and quality control workflow of are outlined after re-engineering the CMSAB organization. Some design principles and key techniques of the HYPAMIS including the cooperation of GIS and MIS, object-oriented spatial data model and management, data management based on database, and security control are illustrated in detail. Then the implementation of the system is introduced briefly. Finally, performance evaluation of the system and future work is given.     

黄渤海风海流的数值计算

文中根据美国提供的“综合海洋和大气资料集”(COADS)资料,编制了黄渤海区30a(1950～1979)平均的四季(代表月取2月、5月、8月、11月)海面风场,进而通过二维非线性流体动力学方程组揭示了研究海区的平均风海流的气候学特征及其随季节的变化.     

IMPACTS OF ANTARCTIC OSCILLATION ON SUMMER MOISTURE TRANSPORT AND PRECIPITATION IN EASTERN CHINA

1INTRODUCTIONSummer precipitation in China is a phenomenon hap-pening in the south-north oscillation process of the EastAsian summermonsoon, andthe monsoon is in essenceresulted from the joint effects of the planetary scale cir-culation ofthermal convecti…     

Hemispheric-scale climate response to Northern Eurasia land surface characteristics and snow anomalies

This paper presents a synopsis of recently published studies by the co-authors, which show that several land surface characteristics unique to Northern Eurasia are responsible for facilitating a causal relationship between autumn snow anomalies in this region and subsequent hemispheric winter climate patterns. The large size and extratropical location of the contiguous Eurasian land mass results in broad, continental-scale interannual snow cover extent and depth variations throughout autumn and winter, and corresponding diabatic heating anomalies. These surface anomalies occur in the presence of a large region of stationary wave activity, produced in part by the orographic barriers that separate northern/central Eurasia from southern/eastern Eurasia. This co-location of snow-forced anomalies and ambient wave energy is unique to Northern Eurasia, and initiates a teleconnection pathway involving stationary wave–mean flow interaction throughout the troposphere and stratosphere, ultimately resulting in a modulation of the winter Arctic Oscillation (AO). Complementary new results are also presented which show that partial snow cover extent or snow depth only anomalies in Northern Eurasia are insufficient to initiate the teleconnection pathway and produce a winter AO signal. This synopsis provides a useful interpretation of the earlier studies in the specific context of Northern Eurasia regional climate and environmental change.