INTERRELATION BETWEEN EAST-ASIAN WINTER MONSOON AND INDIAN/PACIFIC SST WITH THE INTERDECADAL VARIATION

Investigated statistically is the interrelation between East Asian winter monsoon(EAWM)and SST over sensitive areas of the Indian and Pacific Oceans.with focus on the relation of EAWMto strong ENSO signal area.i.e.,the equatorial eastern Pacific(EEP)SST.Evidence suggeststhat the EAWM variation is intimately associated not only with the EEP SST but with theequatorial western Pacific“warm pool”and equatorial Indian/northwestern Pacific Kuroshio SSTas well:the EAWM and ENSO interact strongly with each other on the interannual time scales,exhibiting pronounced interdecadal variation mainly under the joint effect of the monsoon QBO andthe monsoon/SST background field features on an interdecadal basis—when both fields are in thesame phase(anti-phase).strong EAWM contributes to EEP SST rise(drop)in the followingwinter,corresponding to a warm(cold)ENSO cycle;the EAWM QBO causes ENSO cycle to bestrong phase-locked with seasonal variation,making the EEP SST rise lasting from April—May toMay—June of the next year,which plays an important role in maintaining a warm ENSO phase.     

衡阳市湘江水污染特征及其治理

本文探讨了衡阳市湘江水中主要污染物的来源,分布,运移特征及河床沉积物的污染特征,进而评价了其水质并提出治理措施。     

浅源极远震的震相特征与识别方法

介绍了纵波在地球内部的传播过程和浅源极远震的震相特点。由不同震中距的地震反映在三分向地震记录图上的初至震相振幅比的差异,归纳出由地震初动判别地震类型的方法,结合实际工作经验,得出如何判别ＰＫＳ震相、如何由ＰＰ推Ｓ、由ＳＳ反推ＰＰ震相,以及根据地震面波的到时,通过《Ｒｍ－Ｐ》表来验证震中距等几种识别极远震及其震相的方法     

Simplified Method for Calculating Standing Wave Pressure on Vertical Breakwater

Through numerical modeling, a kind of simplified calculating method for standing wave pressure on vertical face breakwater have been put forward. Not only the formulas proposed in this paper are simple in form and very easy in use, but also they possess continuity on the full range of standing wave. And more, the precision requiremennts of calculation can be satisfied to a certain extent in engineering practice.     

Application of long-chain alkenones and U_(37)~k values for paleotemperature estimation in the Arctic Chukchi Sea-Bering Sea area

lwnoowrlowIt is a hot spot in the world to carry out palcoocean and paleo-climate studies by using sur-face sediments. One of the direct effects of the global clirnate changes or short Periedic abnor-mal clirnate events is the variety of sea surface temPerature (wr). Increase or deCrease of theSST wil1 have certainly imPact, the unsaturate ratio (U)v) of long-chain alkenones (LCA)compe Of planktonic algae. The ratio Ulv records the information of SST changes, whichwill be entirely and or…     

The biogeochemistry of carbon cycle in summer of the Prydz Bay, Antarctic Ⅰ:Characteristics of DOC distribution

1　IntroductionAtthepresenttime ,thereiseveryindicationthattheearthbecomingwarmerandwarmer (Liuetal.1 995) ,asoneofthewarmhousegases,CO2 playanimportantroleinthechangingofthetemperatureandenvironmentoftheglobe .TheexchangingofCO2betweentheatmosphereandocean ,maketheoceanbeingthelargepoolofcarbon ,andthechangingofcarboncycleintheoceanwouldbringdistincteffectontheatmosphere .TheSouthernOceanisthewaterbodythathastheenormousenergyandexchangessub stancewithotheroceansintheglobe ,anditsecosystem …     

海上地震勘探GI枪子波数值模拟

GI枪震源已经逐步成为海上地震勘探的主要激发方式。常规气枪只有一个腔室,而GI枪具有G腔和I腔2个腔室,能够较好地压制气泡振荡。基于自由气泡振动理论,分析GI枪的激发机制,在考虑气泡壁的热传导作用和流体粘度对气泡振动影响的基础上,建立了海上勘探GI枪子波数值模型,并对气泡的振动过程和远场地震子波进行了数值模拟。结果表明:当G腔内气体释放所形成的气泡体积达到最大时,I腔内气体的释放有效地抑制了气泡的收缩,气泡壁运动速度明显减小,气泡变得稳定;GI枪激发所产生的子波具有明显的峰值和较小的旁瓣,有利于高分辨率海上地震勘探。     

前言

长江口地处我国经济社会高度发达的东部沿海,与世界其它河口发达地区一样,长江口及邻近海域的生态与环境面临巨大压力和挑战。同时,大河输入、黑潮和东亚季风的相互作用,构成了长江口及邻近海域独特的区域海洋环境,是地球上研究自然变化和人类活动对近海环境演变     

海洋重力资料整理技术与软件实现

针对海洋重力测量成果规范化整理与重力异常计算软件开发问题,重点讨论了重力掉格校正与测线文件获取的可视化方法;引入贝塞尔方法计算船速和航向,并进行厄特渥斯校正.在此基础上,依据海洋重力调查规范,基于图形可视化技术开发了一套具有人机交互功能的海洋重力资料整理软件.     

强潮环境下的海滩剖面沉积特征——以春季广西北海银滩为例

海滩地貌动力状态是海滩过程和陆海相互作用研究中的重要内容,但目前国内对北部湾强潮环境下的砂质海滩地貌与沉积的研究相对较少。对2010年3月采集的北海银滩剖面高程与沉积物变化的资料进行分析,探讨此类海滩响应外在驱动力作用的地貌动力状态特征,结果表明:1)北海银滩地貌结构简单,地貌状态属于消散型类型。2)银滩沉积物类型为砂,并以细砂、中砂为主,沉积物分选性较好;此外,沉积物中砂的百分含量和中值粒径自陆向海逐渐减小,而极细砂的百分含量则逐渐增加。3)北海银滩横向剖面沉积物可区分为后滨、滩面和内滨3个沉积单元。后滨沉积物在风的作用下以跃移质为主;滩面沉积物因波浪形成的冲流作用而具有双向运动的性质;内滨沉积物主要受控于波浪和潮流的联合驱动作用而以跃移质组分为主。