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nwc中文是什么意思

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用"nwc"造句"nwc"怎么读"nwc" in a sentence

中文翻译手机手机版

  • 全国摔跤联合会
  • 营运资本

例句与用法

  • Secondly , the mean seasonal climate characteristics of atmosphere water vapor and its transport flux over nwc respectively in january , april , july and october during the past 50 years was discussed
    其次分析了50年来1 、 4 、 7 、 10各月份西北地区大气水分和水汽平均输送的季节性气候特征。
  • ( 4 ) the intensity of the vertical movement of the air over the east of nwc , from the 1990s " , it tended to weaker , which is regarded as a dynamic background condition
    ( 4 )西北地区东部垂直运动的强弱具有一定的年代际变化, 90年代以来,强度趋于减弱,成为该区90年代降水减少的一个动力背景。
  • That is to say , the so - called drought trend in the east of nwc , is not only point to the evolution of precipitation on the ground in the long term , but also to the vapor content in the whole troposphere
    这是上世纪九十年代中后期天水重大干旱事件发生的一个背景条件。这说明,所谓西北地区东部干旱化的趋势,不仅表现在地面降水量的长期演变方面,而且表现在对流层整层水汽含量方面。
  • Using monthly mean rainfall and temperature data in north - west of china ( nwc ) , the characteristics of rainfall anomaly at rainy season in nwc and the inter - annual varieties of drought / flood are diagnosed by means of eof , reof and wavelet analysis et al . and the ncep / ncar monthly reanalyzed data are employed to analyse the evolution character of water vapor flux and it ' s divergence flux , 500hpa height and u , v wind field . results show that ( a ) the space distribution of rainfall anomaly can be separated into seven climate sensitive areas , the first and the third region have the same rought / flood trend
    本文使用西北(区) 168个站1961 2000年6 9月(主汛期)月平均降水、温度资料,运用eof 、 reof 、小波分析等方法诊断了主汛期月降水异常和旱涝的年代际变化;同时利用ncep ncar月平均资料,分析了强(弱)季风年西北空中水汽通量及其散度场、 500hpa高度场、 u 、 v风场的演变特征,结果表明: ( a )西北汛期降水可分为七个气候异常区,第一、三异常区旱涝趋势相同。
  • ( 3 ) the mean features of vapor water in the atmosphere in the east of nwc between during the great drought affair and dry years are contrasted and shows that , the precipitable water in the whole troposphere is evidently reduced , and the vapor transport is also weakened , the degree of convergence of water vapor is lessened
    ( 3 )对比西北地区东部重大干旱事件期间和典型湿年大气水分平均特征发现:干年西北地区东部全区整层大气可降水量明显少于湿年,且水汽输送减弱,水汽辐合程度也有所减小。
  • ( d ) in the weak monsoon year , nwc lies in the northwest airflow region , west and south wind , as well as moisture transportation are remarkably reduced . except part of the first field , there is vapour flux divergenceon in nwc ( e ) in the strong monsoon years , the height field is low on the west and high on the east , west and south wind , and it ' s vapor flux transportation , are evidently boosted up . there is vapour flux conflurnce in the he first and sixth region
    ( d )弱夏季风年,西北区高度场西高东低,处于脊前西北气流的控制之下,西风和南风明显减小,水汽通量输送也大大减少,除一区的甘肃河东大部( 30 35 n , 101 105 e )存在水汽通量辐合外,其它地区为水汽通量辐散(弱的辐合) 。 ( e )强夏季风年,西北区高度场东高西低,西风和南风明显增强,水汽通量输送同样显著增强,一、三区存在大范围的水汽通量辐合。
  • Lastly , the precipitable water ( pv ) and vapor transport flux during the great drought affair in the east of nwc in 1990s " have been analyzed and compared with what during wet years . the reason that resulted to that drought affair was studied from the point of water vapor in the atmosphere
    再次,对上世纪90年代西北地区重大干旱事件期间大气可降水量、水汽输送等进行了分析,并与典型湿年进行对比,从大气水分特征的角度探讨了这次重大干旱事件的可能形成原因。
  • It is not practical to supply full wavelength converter in a network because of some problem such as long price and complex techniques . so no wavelength converter ( nwc ) and spare wavelength converter ( swc ) are considered in our following chapter . chapter 3 : prototype of ilp model of static rwa issue is proposed here
    由于光迹是较新的一种设计方案,现有的光迹模型只是最基本最简单的模型,还是很粗糙的,并且还没有涉及波长一致性约束,因此,本章在改进了光迹模型描述的基础上,增加了考虑到波长一致性条件时光迹及其保护模型的描述,建模和仿真。
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