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seasonal circulation
相关语句
  季节环流
     Seasonal circulation in the South China Sea ──a TOPEX/POSEIDON satellite altimetry study
     南海的季节环流──TOPEX/POSEIDON卫星测高应用研究
短句来源
     Partial Analysis and Verification of Upper Layer Seasonal Circulation in South China Sea
     南海上层季节环流局部分析与验证
短句来源
     The mechanisms for the fluid mud formation and variation in the Yellow River mouth area and the seaward dispersion of sediment discharged from the Yellow river are well explained by the seasonal circulation and the tidal current distribution and variation.
     季节环流以及涨落潮的分布和变化很好地解释了黄河口南北浮泥的形成和消长变化以及黄河入海泥沙向海扩散的机理。
短句来源
     Combining with the data of UCM and ADCP,the original verification can be get for the way of numerical calculation,which is used to research upper layer seasonal circulation in South China Sea.
     通过分析并结合UCM-60超声海流计和ADCP走航式测流仪相关实测数据,初步验证了这种研究南海上层季节环流所用的数值计算方法。
短句来源
  “seasonal circulation”译为未确定词的双语例句
     The Seasonal Circulation And Thermohaline Structure In The Japan/East Sea(JES) Are studied numericall using the Princeton Ocean Model (POM) with horizontal resoluttion varying from 11.54 to 18.53 km and 15sigma levels conforming to a relatively realistic bottom topography.
     本文利用Princeton Ocean Model(POM)模式从数值上对季节性环流和温盐结构进行了研究。 所取的水平分辨率从11.54km到18.53km,垂直方向取15σ层。
短句来源
     NUMERICAL SIMULATION OF THE SEASONAL CIRCULATION IN THE HUANGHAI SEA AND EAST CHINA SEA
     东中国海环流及其季节变化的数值模拟
短句来源
     The Seasonal Circulation and Thermohaline Structure in the Japan Sea Are Studied Numericall Using the POM
     POM模式分析日本海环流季节变化
短句来源
     This phenomenon is consistent with t he seasonal circulation pattern change of the current induced by the monsoon.
     这个现象是和受季风影响的东海海流的变化相一致的。
短句来源
  相似匹配句对
     SEASONAL VARIATIONS OF ATMOSPHERIC CIRCULATION AND THE RAINY YEARS
     长江中下游持续性多雨与南、北半球大气环流的季节变化
短句来源
     On the Seasonal Variation of Atmospheric General Circulation and the Monsoon
     大气环流的季节变化和季风
短句来源
     3) circulation.
     3、再循环原则。
短句来源
     Circulation Modernization
     流通现代化
短句来源
     Seasonal dynamics of the concentrations of P in C.
     乔木层和亚乔木层青冈中P浓度季节变化较平稳;
短句来源
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  seasonal circulation
In summer, the increase in the proportion of molecular to atomic species, created by the global seasonal circulation and augmented by the geomagnetic forcing, is effective in controlling the plasma densities at all Universal Times.
      
?In this study a methodology for grouping seasonal circulation types occurring over an area is introduced.
      
A Procedure of Reconstruction of the Climatic Seasonal Circulation in the Black Sea Based on the Assimilation of Hydrological Da
      
Application of boundary layer analysis is thereafter made for one specific phenomenological situation, namely the Northern Adriatic Sea and the problem posed by its wintertime seasonal circulation.
      
The seasonal circulation is mostly driven by monsoon winds, and is related to water exchange between the SCS and the East China Sea through the Taiwan Strait, and between the SCS and the Kuroshio through the Luzon Strait.
      
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In this paper, the two months' integration about a global atmospheric circulation model including many physical climatic processes has been made by the global climatic mean data sets in January. The results show that the seasonal circulation systems and the steady active centres are fairly simulated by this model. And the variation of kinetic and internal energy with time show that the computation tends to be stable, consequently, it is expected that this model can be used to simulate, and be capable of...

In this paper, the two months' integration about a global atmospheric circulation model including many physical climatic processes has been made by the global climatic mean data sets in January. The results show that the seasonal circulation systems and the steady active centres are fairly simulated by this model. And the variation of kinetic and internal energy with time show that the computation tends to be stable, consequently, it is expected that this model can be used to simulate, and be capable of simulating the climate changes on time scale of months to years.

地球上的气候演变,是在一个包括大气、海洋、冰、土壤和植物的多相气候系统中,由许多物理、化学、生物过程相互作用的综合结果。对这些过程相互作用的了解,是基于有能力定量地、以相容的表达式将它们结合起来考虑、这种模试依靠一套方程组的数值积分和构成气候数值模式的经验关系。本文给出了一个全球经纬度网格的大气环流模式(AMS GCM),考虑了各种物理过程,并利用实际资料进行了两个月的积分,初步结果分析,效果是令人鼓舞的。

The mean seasonal circulation in upper layer of the South China Sea (SCS) is studied using TOPEX/ POSEIDON altimetry remote sensing products from 1992 to 1996. The research results reveal that upper layer circulation in the SCS is predominated by seasonal alternating monsoons and its pattern varies seasonally. The winter general circulation appears to be cyclone consisted of two sub-basin cyclonic gyres. The summer circulation is generally anticyclonic, but no systematic current...

The mean seasonal circulation in upper layer of the South China Sea (SCS) is studied using TOPEX/ POSEIDON altimetry remote sensing products from 1992 to 1996. The research results reveal that upper layer circulation in the SCS is predominated by seasonal alternating monsoons and its pattern varies seasonally. The winter general circulation appears to be cyclone consisted of two sub-basin cyclonic gyres. The summer circulation is generally anticyclonic, but no systematic current structure is found in the eastern SCS south of 18°N. The results also indicate that circulation in the SCS is notably westen intensified. A jet is observed, in both winter and summer, off the coast of Vietnam and the outer edge of Sunda shelf. It appears to be the strongest current in the SCS, which flows southword in winter, hut northward in summer. Since the dynamic feature of this jet is mainly geostrophic rather than wind drifting, it is suggested that name it as a jet (the SCS Monson Jet) instead of a drift. In winter, the Sunda shelf blocks the southward flowing jet and a northeastward return current is developed along coasts of Kalimantan and Palawan Ialands. In summer, the northward flowing jet splits off the southeast coast of Hainan Island. The northern branch flows along the China shelf, consisting with the traditional path of the SCS Warm Current. The southern branch flows to the east along 18°N across the basin, turns to northeast, and joints the northern branch again off Shantou. The SCS Warm Current is strengthened there by reunification and a zone of weak flow is observed near the shelf break between these branches. In the sense of multiyear mean, the Kuroshio intrudes into the northeastern SCS only in winter and induces a sub-basin cyclonic gyre in the northern SCS. At this period, the SCS Warm Current only exists in the area east of Shantou. In summer, the predominated current in the northern SCS is northeastward. There is no indication of Kuroshio invasion there. Validation using observations from satellite tracking surface drifting buoy shows that these remote sensing results are in good agreement with surface observation.

应用1992~1996年的TOPEX/POSEIDON卫星高度计遥感资料,研究了 冬、夏季风强盛期多年平均的南海上层环流结构.研究结果表明,南海上层流结构呈 明显的季节变化,在很大程度上受该海区冬、夏交替的季风支配.冬季总环流呈气旋 型,并发育有两个次海盆尺度气旋型环流;夏季总环流大致呈反气旋型、但在南海东 部18°N以南海域未见明显流系发育.研究还表明,南海环流的西向强化趋势明显, 无论冬、夏在中南半岛沿岸和巽他陆架外缘均存在急流,其流向冬、夏相反,是南海上 层环流中最强劲的一支.鉴于该海流的动力特征与海洋动力学中定义的漂流不同, 有相当大的地转成分,建议称为“南海季风急流(South China Sea Monsoon Jet)”.冬 季南下的季风急流在南海南部受巽他陆架阻挡折向东北,沿加里曼丹岛和巴拉望岛 外海有较强东北向流发育.夏季北上的季风急流在海南岛东南分为两支:北支沿陆 架北上,似为传统意义上的南海暖流;南支沿18°N向东横穿南海后折向东北;二者 之间(陆架坡折附近)为弱流区.两分支在汕头外海汇合后,南海暖流流速增强.就 多年平均而言,黑潮只在冬季侵入南海东北部,并在南海北部诱生一个次海盆尺度的...

应用1992~1996年的TOPEX/POSEIDON卫星高度计遥感资料,研究了 冬、夏季风强盛期多年平均的南海上层环流结构.研究结果表明,南海上层流结构呈 明显的季节变化,在很大程度上受该海区冬、夏交替的季风支配.冬季总环流呈气旋 型,并发育有两个次海盆尺度气旋型环流;夏季总环流大致呈反气旋型、但在南海东 部18°N以南海域未见明显流系发育.研究还表明,南海环流的西向强化趋势明显, 无论冬、夏在中南半岛沿岸和巽他陆架外缘均存在急流,其流向冬、夏相反,是南海上 层环流中最强劲的一支.鉴于该海流的动力特征与海洋动力学中定义的漂流不同, 有相当大的地转成分,建议称为“南海季风急流(South China Sea Monsoon Jet)”.冬 季南下的季风急流在南海南部受巽他陆架阻挡折向东北,沿加里曼丹岛和巴拉望岛 外海有较强东北向流发育.夏季北上的季风急流在海南岛东南分为两支:北支沿陆 架北上,似为传统意义上的南海暖流;南支沿18°N向东横穿南海后折向东北;二者 之间(陆架坡折附近)为弱流区.两分支在汕头外海汇合后,南海暖流流速增强.就 多年平均而言,黑潮只在冬季侵入南海东北部,并在南海北部诱生一个次海盆尺度的 气旋型环流,这

Dissolved 10 Be concentration profiles in sea water of the East China Sea and the Okinaw a Trough in autumn 1993and summer 1994have been investigated.The results show that 10 Be concentrations in this area are mainly controlled by surface biological productivity,redissolution o f suspended particulate matter,and the degree of mixing of Changjiang River(the Yangtze River)with the Kuroshio waters.During the sampling periods(summer and autumn ),the East China Sea was well stratified.Generally the ...

Dissolved 10 Be concentration profiles in sea water of the East China Sea and the Okinaw a Trough in autumn 1993and summer 1994have been investigated.The results show that 10 Be concentrations in this area are mainly controlled by surface biological productivity,redissolution o f suspended particulate matter,and the degree of mixing of Changjiang River(the Yangtze River)with the Kuroshio waters.During the sampling periods(summer and autumn ),the East China Sea was well stratified.Generally the 10 Be water depth profiles can be divided into three layers:the surface mixing lay er,the particulate 10 Be regeneration layer and the bottom layer.The 10 Be concentrations in surface water increase gradually towards the kuroshi o and increase sharply at the edge of t he Kuroshio Current.Vertical distrib utions of 10 Be show that in the summer 10 Be is enriched in the bottom waters near the Yangtze River estuary and the cen tral continental shelf.The two enriched areas are separated,probably b y an intrusion of the continental coasta l water.In the autumn,10 Be enrichment in bottom water occurred only in the western part of the continent shelf.This phenomenon is consistent with t he seasonal circulation pattern change of the current induced by the monsoon.The i nfluence of the Kuroshio branch intr usion in the southern East China Sea f rom northeast waters of Taiwan on 10 Be may be more significant than the kuroshio mainstream.Box model results indicate that 10 Be input from the Kuroshio Current is more important than from Yangtze Riv er and from atmospheric precipitation.About 81%of 10 Be input to the East China Sea enters i nto the sediments and 19%of 10 Be flows out of the East China Sea by currents and water exchange.The 10 Be sedimentation flux in the East Chi na Sea is nearly five times of the average global 10 Be production rate.Therefore,the East China Sea may be an important sink for 10 Be.

讨论了中日东海MASFLEX合作计划中调查的东海及冲绳海槽海水中溶解态10Be浓度水平及垂直剖面的结果。在这个海区影响10Be浓度的因素主要有生物生产力、悬浮颗粒物的再溶解,以及长江水与黑潮水的混合程度。在样品采集期间(夏季和秋季),东海水柱呈分层状态。通常10Be的垂直剖面可以分成三层,即表面混合层、10Be释放层和底层。表层水10Be的浓度从长江口到黑潮逐渐增大,在黑潮的边缘则剧烈增大。10Be的垂直分布表明,在夏季10Be富集在长江口附近和大陆架中部的底层水中,这两个富集海区是分开的,很可能是由大陆沿岸水所隔开。在秋季,10Be在底层水中的富集仅仅出现在东海大陆架的西部。这个现象是和受季风影响的东海海流的变化相一致的。黑潮分支在台湾东北外海向东海南部侵入对10Be的影响要比黑潮主干流本身更加重要显著。由箱式模型所得到的10Be质量平衡计算结果表明,来自黑潮的10Be输入要比长江及大气沉降的输入更为重要。输入东海的10Be大约81%进入到沉积物中,而19%的10Be则通过海流和水交换流出东海。在东海的10Be沉积通量是10Be全球平均大气生产率的5倍左右,因而东海是10Be的一个重要汇集地。

 
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