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Home > chinese-english > "walker circulation" in English

English translation for "walker circulation"

沃克环流
沃克流


Related Translations:
baby walker:  婴儿学步车婴儿学走路的扶车
clint walker:  克林特沃克
jimmy walker:  华克沃克
spirit walker:  灵魂行者
stalk walker:  工作区
walkers ferry:  沃克斯费里
lee walker:  沃克
dawson walker:  杜逊获加
antoine walker:  沃克
wheeled walker:  带轮子的中器带轮子的助
Example Sentences:
1.Equatorial zonal circulation ; walker circulation
赤道纬向环流walker环流
2.These phenomena are relevant to the anomaly low sst in tropic eastern pacific ( la nina ) and the strengthen of walker circulation
这些现象又与东太平洋海温的明显偏低( lani ( ? ) a )和沃克环流的加强密切相关。
3.The eastward shift in the walker circulation and western wind anomolis are the possible reasons of the change of relationships between summer cross equator flows and enso
赤道太平洋西风异常及walker环流上升支的东移使得夏季越赤道气流与enso的关系产生了明显的年代际变化。
4.On the surface of msta , there exists true dipole mode in the indian ocean , that ' s to say that if the temperature anomaly in the western indian ocean is positive , it is much likely that there is negative anomaly in the eastern indian ocean . dipole mode also exists in the pacific as that in the indian ocean . by virtue of the walker circulation and the similar circulation above the indian ocean , it is showed that the air - sea interaction events in the tropical pacific and the indian ocean develop with each other at the same time
由于在次表层海温距平极值面上,热带西、东印度洋的海温距平呈真正意义的偶极子模态,即当西印度洋海温距平为正(负)时,东印度洋海温距平为负(正) ,偶极子模态的海温距平分布在热带太平洋同样存在,两大洋海温距平的偶极子模态间有密切的联系,结合walker环流和印度洋上空的类似walker环流,进而指出热带印度洋和太平洋海气相互作用事件是协调发展的。
5.During the years of strong monsoon , the convective activities happening in tropical india ocean and tropical west pacific and walker circulation are much stronger than that during the years of weak index , but the convective activities happening in tropical east pacific are weaker than those during the years of weak monsoon
春季热带对流活动对山东夏季降水异常的贡献比夏季更显著。强季风年与山东夏涝年相联系,热带印度洋一菲律宾群岛、南海一热带西太平洋对流活动偏强,热带东太平洋地区对流活动偏弱, walker环流加强。
6.When the spatial pattern is uniform in the whole area , there is a better relations between the wp ssta and walker circulation , hadley circulation , enso and the summer rainfall of the upper and middle reaches of the yangtze river , while the spatial pattern is of the north - south asymmetry , there is a better relation between the wp ssta and hadley circulation and the summer rainfall of the middle and lower reaches of the yangtze river
暖池区ssta不同分布型与东亚大气环流和中国夏季降水关系不同, ssta的一致性分布与hadley 、 walker环流、 enso循环及长江中上游地区降水关系较好,而ssta南北反对称分布与hadley环流和长江中下游地区降水关系较好。
7.Results show that there are two main spatial patterns of the wp ssta : one is uniform in the whole area , the other is of the north - south asymmetry . when the spatial pattern is uniform in the whole area , in the warm years , there is a anticyclone circulation existing over the warm pool and westerly in the subtropical region and easterly in the tropical region have been greatly strengthened at 850hpa , while a anticyclone circulation over the india region at 200hpa , the walker circulation has been strengthened , the summer rainfall may be above normal in the upper and middle reaches of the yangtze river , vice versa
当ssta为一致性分布时,暖异常年, 850hpa暖池区上空为一反气旋偏差环流,副热带地区西风和低纬度地区东风得到加强,长江中上游地区盛行偏南风气流; 200hpa南亚上空为一反气旋偏差环流,长江中上游地区为北风; walker环流加强,副热带高压偏强,经向垂直环流在25 35 n附近为上升气流,长江中上游地区降水偏多,是lanina事件的多发年,对应的soi指数偏高,冷异常年则相反。
8.Based on the analysis mentioned above , a conceptual diagram explaining the physical process is put forward : stronger ( weaker ) convective activities in tropical areas stronger upward ( downward ) vertical anomaly stream in tropical areas more ( less ) moisture transports from " key regions " to shandong stronger ( weaker ) hadley and walker circulation stronger ( weaker ) east asian summer monsoon eap ( negative eap ) in 500hpa upward ( downward ) vertical anomaly stream rise in shandong subtropical high abnormally located northward ( southward ) more ( less ) rain in shandong province
弱季风年与山东夏旱年则相反。通过分析山东夏季降水与东亚夏季风以及大气环流异常的物理过程,得出了如下物理概念模型:热带印度洋以及南海-热带西太平洋地区对流加强(减弱)吟热带地区垂直上升(下沉)气流增强峥热带印度洋和南海一西太平洋地区水汽输送通量增加。
9.During 1950 ~ 1976 / 1977 , the walker circulation over the tropical pacific and the vertical zonal monsoon circulation over the tropical indian ocean coupled at the oceanic continent , the same period when el nino occurs , the anomaly of the west wind over the tropical pacific can correlate with the departure of east wind over the tropical indian ocean through the two coupled vertical zonal circulation . but after 1976 / 1977 , the updraft of the walker circulation moved eastward . locating at the north of australia . therefore the two vertical zonal circulation could n ' t coupled , and the anomaly of west wind and the departure of east wind could n ' t geared . in the result . the signal of enso decreased in indian ocean after 1976 / 1977
1951 1976 1977年,热带太平洋的walker环流和热带印度洋的纬向季风环流在海洋性大陆附近耦合,当elnino事件发生时,太平洋的西风异常可以通过这两个纬向的垂直环流与印度洋的东风异常联系起来,而1976 1977年以后,由于西太平洋walker环流上升支东移到澳大利亚北部,热带两洋的纬向垂直环流无法耦合,热带太平洋elnino事件中的西风异常与热带印度洋的东风异常联系减弱,所以1976 1977年以后, enso在热带印度洋的信号减弱了。
Similar Words:
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