nwc meaning in Chinese
全国摔跤联合会
营运资本
Examples
- 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。