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negative anomaly in Chinese

Pronunciation:
How to pronounce "negative anomaly""negative anomaly" in a sentence
TranslationMobile
  • 负异常
Examples
  • During flood years , the center of negative anomaly is around ural mountains , the center of positive anomaly is around high - latitude of east asia and another negative and positive center are over okhotsk sea and the north - west pacific , respectively
    通过对夏季旱涝等级指数的morlet型和mexicanhat型小波变换分析,发现山东夏季旱涝指数主要存在着2 5年和7年左右的周期振荡。
  • 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。
  • Research manifests that : ( 1 ) allocation in the year of precipitation is very uneven , and yearly precipitation is different in great scope , negative anomaly of precipitation appear concentratly in the 1990s , the precipitation in the 1990s decreased in different degree ; ( 2 ) close positive correlation exists between runoff and precipitation , runoff is abundant in the year with prolific precipitation , and generally in the year with scarce rain the volume of runoff is not enough ; ( 3 ) there is 20 % margin in their changes amplitude , this mainly resulted from high frequent human activities
    结果表明: ( 1 )流域内降水年内分配极其不均;年际变化剧烈,进入90年代后降水负距平集中出现, 20世纪90年代降水较多年均值有较大程度的减少; ( 2 )流域内河川径流与降水之间存在密切的正相关关系,降水量多的年份,河川径流丰富,反之较枯; ( 3 )河川径流积极响应降水的变化,然而河川径流变化幅度却比降水变化幅度大20 % ,这个偏差主要是由于频繁的人类活动的干扰造成的。
  • The precipitation character of the middle part of viet nam and its relation to the atmospheric circle . the autumn precipitation of the middle part of viet nam has obvious variations in inter - annual and inter - decade scale with clearly quasi 6a , 10a , 15a period ; in heavy rainfall years , there are a positive anomaly over the north - west pacific and a negative anomaly over japan ; while in deficient rainfall years , the anomaly distribution is on the contrary ; 4 . the precipitation character of the south part of viet nam and its relation to the atmospheric circle . the research finds that the rainfall of the south part of vietnam usually concentrates in the autumn every year and a clear difference of atmosphere condition exists between that of flood and drought years
    越南中部降水变化特征及其与大气环流和海温的关系越南中部秋季降水具有明显的年际、年代际变化特征,具有明显的准6a 、 10a 、 15a左右的周期;越南中部多雨年, 500hpa高度距平场在热带西北太平洋为正距平,日本附近上空为负距平;而少雨年则相反;越南中部多雨年,热带中东太平洋海温异常偏高,西太平洋海温异常偏低;少雨年则相反;越南中部多雨年,登陆越南的台风频数偏多;而少雨年则相反。
  • There is a north - north - east negative anomaly belt of aerial magnetism in the middle - east part of the basin , which could be displayed by the aerial magnetism of commutative field , upwardly continuation , lvt in earthquakes , the experimentation of granite liquation ( demagnetization ) , the distribution of neozoic era volcanic rock , earthquake , hot spring and ground feature . the anomaly shows the blocking in east - west direction , and it is also associated with intense activity of deep heat interaction and the development of the crust - mantle mixed layer in the north qiangtang
    从区域航磁、向上延拓、地震低速层、花岗岩熔融(退磁)实验、新生代火山岩的分布、地震、温泉、地貌等发现,盆地中东部存在一北北东向航磁负异常带,既显示出东西分块,也与北羌塘深部热力作用强烈活动、发育“壳幔混合层”有联系。
  • The research showed that : from january to march , the acreage average ozone gross gathered , which was synchronized with the increase of the frequency of strong ssw event . furthermore , the change tendency of ozone gross in the atmosphere break forward and backward 1990 . after the1990s , ozone gross in the atmosphere appeared negative anomaly in the mid and high latitude of north hemisphere from january to march , which was consistent with the obvious descent of appearance frequency of strong ssw event after the 1990s
    分析表明: 1至3月,臭氧总量的面积平均逐渐增高,这与强ssw事件频数1至3月增高同步;此外,大气臭氧总量趋势变化以1990年前后存在明显的突变, 90年代以后,北半球中高纬1 ? 3月间大气臭氧总量处于负异常阶段,这和90年代以来强ssw事件发生频数明显下降相吻合。
  • Numerical studies suggest that long scale and slow - changed oscillations in the zonal wind stress rebuild by pop anal ysis make the intention of el nino / la nina events deeply . it also enlarges their range . but , positive and negative anomaly center is toward west than actual conditions
    数值试验的结果表明,由pop重建的纬向风应力中缓慢变化的大尺度振荡成分加深了elnino lanina事件的强度,加大了它们的空间分布范围,但正负距平中心的位置比观测风应力模拟的情况偏西。
  • The positive and negative anomaly centers at 500hpa level formed the anomaly " wave train " from lower latitude to higher latitude over east asia . the teleconnection pattern called east asia - pacific pattern ( eap ) plays important roles in the summer rainfall in shandong area . study shows that weaker okhotsk sea high , northward location of subtropical high and stronger indian low , are likely to lead to more rain in shandong province in summer
    分析对比旱涝年不同层次高度场以及高低层散度场,结果发现,在春夏季旱涝年,高度场几个主要的距平中心以及115 130 e区域高( 200hpa )低( 925hpa )层散度场基本呈现出反位相分布特征,北半球夏季存在的东亚-太平洋遥相关型( eap型)对山东夏季降水产生重要影响。
  • 3 in the years of cold spring , the inner mongolia high and the aliushen low are strengthened with the low index of the east asia trough and the negative anomaly center of temperature over northeast china from surface to tropopause while the contrary conditions occur in the years of warm spring
    3 、东北地区出现春季低温的主要环流特征是:内蒙古高压,阿留申低压的强度加强;阿流申低压指数以及东亚大槽强度指数减弱,东北地区从地面到对流层顶处在温度负距平中心内,东北地区春季高温时则出现与上面相反的变化形式。
  • Among the felsic rocks , samples from the zhangjiakou formation ( fm . ) are characterized by moderately to strongly eu anomalies , and variable negative anomaly of sr , ti and p , whereas samples from the donglingtai fm . exhibit enriched lree and flat hree patterns with nb / ta fractionation and high zr / sm ratios
    在中酸性火山岩系列中,张家口组火山岩表现出中等-强烈的eu负异常和不同程度的sr 、 ti 、 p负异常;东岭台组火山岩表现出富集lree和平坦的hree的稀土配分模式, nb ta分馏,高zr sm比值。
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What is the meaning of negative anomaly in Chinese and how to say negative anomaly in Chinese? negative anomaly Chinese meaning, negative anomaly的中文negative anomaly的中文negative anomaly的中文,translation, pronunciation, synonyms and example sentences are provided by ichacha.net.