赤道潜流,equatorial undercurrent
1)equatorial undercurrent赤道潜流
1.A Study on a Model of Origin of Pacific Equatorial Undercurrent太平洋赤道潜流起源的模式研究
2.Variations ofequatorial undercurrent and its relationship with ENSO cycle赤道潜流变化及其与ENSO的关系
3.Variable properties of theequatorial undercurrent in the Pacific and its anomalous warm water eastward propagation;在年际变化中,赤道潜流变化特征非常明显,尤其是在El Nino事件发生过程中,赤道潜流出现明显的加强现象。
英文短句/例句
1.Variations of equatorial undercurrent and its relationship with ENSO cycle赤道潜流变化及其与ENSO的关系
2.hydrodynamics of equatorial ocean赤道海洋流体动力学
3.The equator. Used with the.赤道赤道。和the连用
4.Eisenia foetida for Enhancing Subsurface Flow Constructed Wetlands赤子爱胜蚓强化潜流人工湿地效能的研究
5.Many rivers carry silt toward the equator.许多河流带着泥沙流向赤道。
6.quasi-biennial oscillation (QBO)赤道地区平流层风的准两年振荡
7.Researches on Interannual and Inter-decadal Variability of Cross-Equatorial Flow;越赤道气流的年际、年代际变化研究
8.After a latent period of 2-3 days, outgrowth was observed across the posterior capsule.经过2-3天的潜伏期,LECs开始从囊袋赤道部长出,并在后囊上延伸。
9.The Circulation Configuration of Strong/Weak Cross-Equatorial Flow to the North of Australia澳洲北部强/弱越赤道气流对应的环流配置
10.Advances of the study of the North Equatorial Current bifurcation and the northern circulation of the South China Sea北赤道流分叉点及南海北部环流的研究进展
11.Equatorial Customs Union赤道关税同盟(赤道税盟)
12.Researching an Implicit Rule of US Mainstream Media Coverage;探析美国主流媒体涉华报道的潜规则
13.EARLY MEI - YU OVER THE JIANG - HUAI AREA IN 1991 AND ITS RELATION WITH THE ABNORMALITY OF THE CROSS EQUATORIAL CURRENT1991年江淮早梅及其与过赤道气流异常的关系
14.AN ANALYSIS ON THE CHARACTERISTICS OF THE STRONG WESTERLY WIND BELT AT THE LOWER LEVEL AT THE UPLIFTED AREA OF WALKER CIRCULATION沃克环流上升区赤道低空强西风带的分析
15.Study on Formation Causes of Strong and Weak Cross-equatorial Flow to the North of Australia;澳洲北部越赤道气流强弱变化的成因研究
16.QBO of Stratosphere Water Gas in Equator;赤道地区平流层水汽准两年周期振荡特征
17.Interannual Variation of Summer Cross-Equatorial Flow in Lower Troposphere of Eastern Hemisphere东半球夏季低空越赤道气流的年际变化
18.A westward moving airstream will, therefore, move equatorwards as it passes over the barrier.因此,向西流动的气流在通过壁垒时,将向赤道方向运动。
相关短句/例句
Cromwell current太平洋赤道潜流
3)equatorial currents赤道流系
4)North Equatorial Current北赤道流
1.Surface Current Speed and Bifurcation of theNorth Equatorial Current in the Pacific Ocean;太平洋北赤道流表层流速及分叉点位置
2.Advances of the study of theNorth Equatorial Current bifurcation and the northern circulation of the South China Sea北赤道流分叉点及南海北部环流的研究进展
3.The China Pioneer Area of Eastern Pacific Ocean is to the north of the equatorial high nutrients area, across the the boundary of theNorth Equatorial Current and North Equatorial Countercurrent.中国多金属结核开辟区位于东北太平洋夏威夷东南海域,北赤道流和北赤道逆流的交界处,其南侧是赤道太平洋上升流区,为我们深入了解营养盐动力学提供了绝佳的机会。
5)South Equatorial Current (SEC)南赤道流
6)equatorial current赤道流
延伸阅读
赤道潜流赤道潜流equatorialundercurrent赤道附近海域次表层中的海流。处于赤道流之下,中层水之上。与表层南北赤道流的流向相反,自西向东流动,流速较表层的赤道流大。所在的次表层是一个温跃层。1952年首次由T.克伦威尔在太平洋发现,命名为克伦威尔海流。以后在大西洋和印度洋都发现了这种潜流。就太平洋而言,赤道附近海域从海面至深度为50~100米的表层,是温度均匀的暖水层,其下至深度约300米处为温跃层,即赤道潜流所在的次表层。赤道潜流的厚度约200米,流幅(宽度)约300千米,约介于南纬2°至北纬2°之间;流轴大致与温跃层一致,最大流速达1.5米/秒,流量约为4.0×107米3/秒,流长约为1.4万千米,几乎横跨了太平洋。大西洋赤道潜流与此相近。印度洋面主要受季风控制,在赤道处的风主要是经向的,随季节更替而改变方向。故每年11月~次年的3月吹北风,5~9月吹南风,都不能产生赤道潜流;只有在3~4月才有印度洋的赤道潜流。