2000年7-8月台湾海峡南部至珠江口附近海域表层温、盐度分析   总被引：3，自引：3，他引：3  

庄伟  胡建宇  贺志刚  曾淦宁  陈照章 《热带海洋学报》2003,22(4):68-76

根据表层温、盐度的观测结果，结合相关断面的CTD调查资料和同期的卫星遥感海表温度图，分析了2000年7月10日到8月2日台湾海峡南部至珠江口附近海域的一些海洋现象，结果表明：(1)在调查期间，东山至惠来沿岸海域存在明显的低温高盐区，海丰和惠来以南近岸海域的海水也具有相对高盐的性质，说明调查期间在闽南、粤东沿岸普遍存在上升流现象；(2)调查期间在台湾海峡南部至珠江口之间陆架—陆坡区附近的多个断面上观测到了较明显的盐度锋面；(3)珠江口外的盐度锋面的位置随时间而不断变化。  相似文献   

Dynamic Analysis of a Single-Column Platform     

Lian Gan  Ni Kan  Hu Kai  Guo Dawei Prof.  Senior Engineer  Marine Design  Research Institute of China  Shanghai Senior Engineer  Marine Design  Research Institute of China  Shanghai Engineer  Marine Design  Research Institute of China  Shanghai 《中国海洋工程》1991,(4)

In this paper, a single-column structure used as well-head platform is studied. The loads of wave and current exerted on the single-column will be greatly reduced, therefore the cost of the structure will be decreased. The advantages of the single-column structure compared with ordinary jacket structure are explained. A dynamic analysis of this type of structure is made and some problems related to dynamic analysis are solved. In order to check the reliability of computation theory and programme, model tests have been carried out. However, as space is limited, the conclusion of tests will be introduced in another paper. Therefore, this type of structure is applicable for proctical engineering.  相似文献   

Marine disaster prevention and integrated coastal zone management     

许富祥  韦锋余 《海洋预报》2001,18(Z1)

1 MAJN CHARAcrERISTICS OF MARINE DISA5TEROwing to marine natural environment anomaly and imense changr, alI those disastersthat cause Peoples life and propedy loss over the sea aod coast area are called marinedisasters. China is a country with big sea area, of coast line l8000 km length, precinctsea area 3,000,000 km', more than 6500 islands bigger than 500 m2 with coast line of allislands 14000 km length. The Pacific Ocean is ocean with the most frequent marine disasters,further…  相似文献   

北部湾温度锋的季节与年际变化   总被引：1，自引：0，他引：1  

罗琳  王东晓  刘赟  李适宇 《热带海洋学报》2003,22(4):60-67

采用8a(1991—1998)的卫星遥感海水表面温度资料(AVHRR SST)对北部湾温度锋的季节变化与年际变化规律进行了探讨。北部湾海区温度锋的季节态强弱趋势为春季最强，夏季、冬季次之，秋季最弱。在年际时间尺度上，温度锋强度与SST距平(SSTA)存在响应关系，表现在：1)SST正距平对应较弱的锋面产生，负距平对应较强的锋面产生，这种相关性在冬季表现得最为明显；2)锋面的强弱与SSTA绝对值存在正相关关系，即SSTA变化越大，锋面越强。在冬季，温度锋强度与海面风经向分量相关，在偏北风异常情况下，锋面较强；反之，锋面较弱。  相似文献   

南海北部17937岩心四万年来古环境变化的分子有机地球化学记录   总被引：4，自引：0，他引：4  

李丽  王慧  汪品先 《地球科学》2008,33(6):793-799

以分子有机地球化学为手段对南海北部四万年来的古环境古气候研究表明, U₃₇k’-SST表层水温在冰期、间冰期平均范围分别为27℃和24℃, LGM与全新世温差达4.5℃; 以高分子量烷烃所代表的陆源物质输入和长链不饱和酮化合物所代表的海洋初级生产力都呈现冰期高、间冰期低特征, 表明冰期时陆源物质输入的增加和海洋表层生产力的提高; 正构烷烃C₃₁/C₂₇记录了南方大陆的植被由冰期时草本植物占优势向间冰期时木本植物占优势的转变.说明南海在末次冰期以来气候的不稳定性, 和海陆生态系统对气候变化的响应以及分子有机地球化学在古环境古气候研究中的巨大潜力.   相似文献   

南海南部普林虫与“中更新世革命”   总被引：6，自引：2，他引：4  

徐建汪品先  黄宝琦翦知湣 《地球科学》2004,29(1):7-14

对南海南部ODP 1143站2.1 Ma以来沉积物中的浮游有孔虫群进行研究, 发现在冲绳海槽及南海北部普遍被认为是黑潮标志种的Pulleniatina obliquiloculata在中更新世革命(MPR)前后对冰期旋回的响应截然相反; 且在MPR之后的变化与南海北部和冲绳海槽相反, 即冰期时含量高而间冰期时低.交叉频谱分析和相位分析的结果也证实了ODP 1143站P.obliquiloculata与全球冰量变化之间的上述关系.该种在MPR前后冰期旋回的转变, 可能是由于MPR之后南海南部在冰期时切断了与印度洋之间的海水交换, 或者是冰期时海水盐度增加等因素引起的上部水体结构的重大改观所致.   相似文献   

南海ODP1143站上新世至更新世天文年代标尺的建立   总被引：8，自引：3，他引：5  

田军  汪品先  成鑫荣  李前裕 《地球科学》2005,30(1):31-39

基于底栖有孔虫δ18O的精确的年代标尺是古海洋学研究的基础, 特别是长度超过5 Ma, 分辨率小于5 ka的连续δ18O记录在全球大洋深海记录中更是凤毛麟角.在大西洋和东太平洋已经建立起了类似的代表性剖面, 如大西洋ODP659站和东太平洋ODP846站, 但在对全球气候有着重要影响的“西太平洋暖池区”还没有建立起这样的剖面.以南海大洋钻探184航次1143站底栖有孔虫的δ18O为材料, 建立了西太平洋地区跨越5 Ma、分辨率达2~ 3 ka的天文年代标尺.天文调谐的基本原理参照Imbrie et al.(1984), 并将斜率周期上8 ka的相位差和岁差周期上5 ka的相位差从晚更新世扩展到5 Ma; 调谐目标选用Laskar(1990)的斜率和岁差; 调谐方法采用了有别于ODP659站和ODP846站的自动轨道调谐方法(Yu and Ding, 1998).调谐结果显示, 1143站190.77 m、191个冰期、间冰期的深海沉积记录了5.02 Ma的南海古海洋学历史; 1143站布容/松山磁性反转事件的年龄为0.78 Ma, 与前人研究结果一致; 15个识别出的浮游有孔虫生物事件年龄部分与已经发表过的年龄相吻合, 部分为该生物事件在南沙海区的新年龄.由年代标尺推导出的南海沉积特征显示, 2.9 Ma是沉积速率的一个转折点, 在此之前, 平均线性沉积速率只有39.5 m/Ma, 冰期、间冰期平均波动幅度为50 m/Ma; 2.9 Ma以后, 平均线性沉积速率猛然上升到65.4 m/Ma, 冰期、间冰期平均波动幅度为200 m/Ma.此外, 南海的沉积速率还显示出冰期或间冰期中的亚冰阶沉积速率高, 而相邻的间冰期或亚间冰阶的沉积速率低, 这种特点在更新世尤为典型.这可能与全球冰量变化带来的冰期、间冰期差异性风化剥蚀和搬运有关.   相似文献   

Erratum to: An event-by-event assessment of tropical intraseasonal perturbations for general circulation models     

Jean Philippe Duvel  Hugo Bellenger  Gilles Bellon  Marine Remaud 《Climate Dynamics》2013,40(9-10):2575-2575

  相似文献   

High-Resolution Mesoscale Analysis Data from the South China Heavy Rainfall Experiment (SCHeREX): Data Generation and Quality Evaluation          下载免费PDF全文

倪允琪  崔春光  李红莉  彭菊香  邱学兴  张艳霞  许晓林  高梅  接连淑  张文华 《Acta Meteorologica Sinica》2011,(4)

In this study, the observational data acquired in the South China Heavy Rainfall Experiment (SCHeREX) from May to July 2008 and 2009 were integrated and assimilated with the US National Oceanic and Atmospheric Administration’s (NOAA) Local Analysis and Prediction System (LAPS; information available online at http://laps.fsl.noaa.gov). A high-resolution mesoscale analysis dataset was then generated at a spatial resolution of 5 km and a temporal resolution of 3 h in four observational areas: South China, Cent...  相似文献   

Characterisation of rapid infiltration flows and vulnerability in a karst aquifer using a decomposed fluorescence signal of dissolved organic matter     

Marine Quiers  Christelle Batiot-Guilhe  Cristina C. Bicalho  Yves Perrette  Jean-Luc Seidel  Sandra Van Exter 《Environmental Earth Sciences》2014,71(2):553-561

The fluorescent properties of dissolved organic matter (DOM) have been used as natural tracers in various water systems. However, only few studies have focused on groundwater systems, specifically, on karst systems. The aim of this study was to develop the use of the DOM fluorescence signal as a natural tracer, considering the multiple compartments of a karst system. This method was applied to the Lez hydrosystem, which supplies the city of Montpellier with drinking water. The hydrodynamics and hydrochemistry of the spring were monitored beginning March 2006. The DOM fluorescence was measured by the excitation–emission matrix spectroscopy technique. The analysis of the total fluorescence signal confirms the efficiency of this tool to trace rapid infiltration flows. Moreover, the decomposition of the signal into different fluorophores complements the information provided by the total signal. Indeed, the fluorescence emitted by the humic compounds seems to be the ideal tool for identifying rapid infiltration flows. Nevertheless, the fluorescence of protein-like compounds is better correlated with the inflow of faecal bacteria at the outlet. This decomposition of the fluorescence signal is an interesting way to provide information on both the rapid infiltration flow as well as the vulnerability of the karst aquifers.  相似文献