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monsoon circulation中文是什么意思

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用"monsoon circulation"造句"monsoon circulation"怎么读"monsoon circulation" in a sentence

中文翻译手机手机版

  • 季风环流

例句与用法

  • Eawm - related air - sea - land interaction and the asian summer monsoon circulation
    相关的海陆气相互作用及亚洲夏季风
  • Furthermore , comparisons are made between the monsoon circulation index proposed in this paper and other monsoon indices for their representation of climate anomalies in china
    此外，还将该环流指数与目前常用的4种东亚夏季风指数进行了对比分析。
  • With 1958 ~ 1997 ncep / ncar reanalysis data and 1961 ~ 1995 summer ( jja ) rainfall and temperature records of 160 stations in china , a new east asian subtropical summer monsoon circulation index is defined , in which the barotropic and baroclinic components of the circulation are included
    摘要采用大气环流正、斜压分解方法，从东亚副热带夏季风为正、斜压混合型季风观点出发，定义并计算了1958 - 1997年东亚副热带夏季风环流指数。
  • In drought or flood years over the yangtze river basin , the features of the establishment , progression and decrease of moisture transport is significantly different , meanwhile the differences of the moisture transport by the monsoon circulation between mid and low latitudes in the northern hemisphere , and by the subtropical high are obvious , so are their convergence , especially over south china sea , the tropical west pacific , the yangtze river basin , north china and north - east in china
    ( 4 )长江流域旱涝年亚澳季风区夏季风水汽输送的建立、推进、减弱的阶段性特征显著不同，对应的中低纬季风环流、副高环流等季风系统水汽输送、汇合也有显著差别，尤其是在南海、热带西太平洋、长江流域、华北和东北等地区。
  • The summer rainfall anomaly of north china is closely related to indian low , west pacific subtropical high , westerly troughs and ridges in mid - latitude , south asia high , subtropical monsoon circulation and cold air activity on the corresponding period , and similar circulation pattern also appears in the preceding spring
    结果表明： ( 1 )华北夏季降水异常与同期印度低压、西太平洋副高、中纬度西风槽脊、南亚高压、副热带季风环流和冷空气活动的异常都密切相关。华北夏季降水异常年春季的环流特征与夏季类似。
  • ( 4 ) in summer , tropic west pacific ssta decadal change infect precipitation decadal change in south and north of changjiang river maybe by : positive ssta in tropic west pacific weaken the summer monsoon circulation , lead more precipitation in south of changjiang river and less precipitation in north of it , vice versa ; middle north pacific ssta decadal change infect precipitation decadal change in mid - down valley of changjiang river maybe by : when ssta is negative in middle north pacific , the height field in tropic rises obviously , the subtropical high strengthens and extends westward , the northern limit retreats southward , leads upper trough retreats northward and move eastward , meiyu front moves northward , then leads more precipitation in mid - down valley of changjiang river , vice versa ; middle northwest pacific - low latitude mid - east pacific infects precipitation in north china possibly by change the activity of northeast china cyclone
    （ 4 ）热带西太平洋ssta年代际变化影响夏季中国长江南北降水年代际变化的可能机制是热带西太平洋海表温度正（负）异常减弱（加强）东亚夏季风环流，从而使江南降水增加（减少） ，江北降水减少（增加） ；夏季中部北太平洋ssta年代际变化影响中国长江中下游地区夏季降水年代际变化的可能机制是中部北太平洋海表温度负异常，将导致热带地区高度场普遍增高，副高加强西伸，副高北界南退，致使高空槽北缩东移，梅雨锋西移北进，中国长江游中游、中卜游降水增多，反之亦反；夏季中高纬西北太平洋一低纬中东太平洋反向距平分布结构影响中国东北降水的可能机制是低纬中东太平洋海表温为负异常。
  • The responses of asian monsoon circulation to the heat source annual anomalies over the bay of bengal and philippines in summer and the annual relationships between the heat sources over the bay of bengal and philippines and the precipitation of china in summer are studied emphatically , with the results as follows : ( 1 ) the coverage and intensity of atmospheric heat source are the largest and strongest in summer and then turn smaller and weaker in autumn and winter , and in turn begin to become larger and stronger in spring again
    着重讨论了夏季孟加拉湾和菲律宾热源年际异常时，亚洲季风环流系统的响应，及其与中国夏季降水的年际关系。结果表明： ( 1 )夏季大气热源的范围最大，强度最强，以后以秋、冬季依次变小变弱，春季又开始变大变强。夏季亚洲季风区有三个强的大气热源中心，其中以孟加拉湾热源最强，菲律宾热源和印度半岛西部热源次之。
  • 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。
  • Using the daily and monthly ncep / ncar reanalysis data from 1951 to 2000 and monthly precipitation of 160 stations in china in summer from 1951 to 2000 , the climatic distribution of heat source are computed . the responses of the asian monsoon circulation to the annual anomaly of the heat source over the bay of bengal in summer and the annual relationship between the heat source and the precipitation of china in summer are analyzed
    摘要利用1951 - 2000年ncep / ncar再分析逐日及月平均资料和我国160个测站1951 - 2000年月降水量资料，计算了夏季大气热源气候分布，分析了夏季孟加拉湾地区热源年际异常及亚洲季风环流系统的响应，以及夏季孟加拉湾地区热源与中国夏季降水的年际关系。
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