环流系统的英文

• circulating system
• circulating-current system

• 环流:    circulation; circulating cur ...
• 系统:    system
• 无环流系统:    non-circulating-current system
• 深层环流系统:    thermohaline circulation
• 温差环流系统:    thermosiphon; thermosyphon

例句与用法

1. ( 3 ) the polar eddy , the west circumfluence on 500hpa medium latitudinal region ands subtropic circumfluence are the key systems of tpnes floods precipitation and , the wet years have abundant vapor , moreover , the omga is positive in all atmosphere
   ( 3 )极涡、中高纬西风环流系统和副热带系统是影响青藏高原东北侧区汛期降水的大尺度环流背景关键系统。同时，多雨年的主要流场特点是有利于水汽输送，且整层大气始终表现为上升运动。
2. Then by using of statistics and numerical simulation analysis , research abnormality of the main circulation system at following summer in east asia , and the influence of the abnormality on the rainfall and temperature in summer in china , when sst over the kuroshio area during winter show cold or warm anomaly
   再分别通过统计和数值模拟的方法，系统的分析了冬季黑潮海温冷暖异常时，后期夏季东亚地区高低空的主要环流系统的异常，以及这些异常又如何进一步影响了我国夏季的降水和气温。
3. Its interannual variation ' s main period is about 4 ~ 5a and the 7 ~ 8a ' s period exist too ; the interdecadal variation ' s main period of the australian high is about 15a . the interannual variation of australian high ( aah ) has correct correlation with antarctic oscillation and enso , and the enso ' s 4a period has the most important influence on the aah . ( 2 ) when the ah becomes stronger , the members of the whole aamcs are stronger following it . that is to say , in the years that the ah is stronger ( compared to the weak years of ah ) and on the horizontal circulation , the members of aamcs , including the ah , the cross - equator flow ( cef ) between 100 and 160 e , the south china sea south - west monsoom ( ssm ) , the south sea monsoon rough , the tropical easily flow , subtropical high ( sh ) , the mei - yu front , the mid - latitude effect , become stronger , and their positions are more southward ; in the meridional - right circulation , there are five circulations including classic monsoon meridional - cirle circulation and hadley circulation that become stronger in the strong years of ah than in the weak years of ah
   本文采用ncep ncar再分析月平均的全球海平面气压场、高度场、海表温度场、高云量和cmap全球降水资料，以及中国160站逐月降水资料，分析了1948 2002年期间澳大利亚高压(以下简称澳高)的年际和年代际变化以及澳高年际变化对亚澳季风环流系统的影响，结果显示： ( 1 )澳高存在明显的年际和年代际变化，澳高年际变化以4 5年的周期变化为主，同时兼有7 8年左右的周期，而澳高的年代际变化则以15年左右的周期变化为主：澳高年际变化同时与南极涛动和enso有正相关，并且enso的4年左右的周期变化对澳高年际变化影响最大。
4. When the wpi - soi correlation is weak and the west pacific sst warmer ( colder ) , a anomalous anticyclonic ( cyclonic ) circulation is found in the lower troposphere over northern equatorial western pacific . this anomalous circulation is not in favor of maintaining a significant correlation between the west pacific sst and enso
   Wpi - soi相关关系微弱时，在西太平洋赤道北侧的对流层低层存在高(低)海温?反气旋(气旋)异常环流系统，不利于维持enso与西太平洋海温变化间的紧密联系。
5. The distribution pattern can be attributed to ( 1 ) pollution sources located mostly in the eastern coast area ; ( 2 ) the current circulation systems in jiaozhou bay which hindered diffusion of pahs from east towards west ; ( 3 ) sediment grain size and composition factors had an influence on the horizontal distribution
   造成这种东-西差异分布格局的原因有( 1 )绝大部分污染源集中在胶州湾东岸； ( 2 )胶州湾的环流系统和潮流系统使东部的污染物很难向西部扩散； ( 3 )沉积物粒度及有机质含量对pahs含量分布有一定的影响。