vapor flux meaning in Chinese
气体焊剂
水气通量
水汽通量
Examples
- The results show that before the summer monsoon onset , the air - sea heat exchange near xisha area is weak , the vapor flux is small and the main trend is that the ocean is being heated ; while after its onset , the air - sea heat exchange is balanced roughly
结果表明：季风爆发前，西沙海气界面热量交换较弱，水汽通量较小，以海洋获得热量为主；季风爆发后，海气界面热量交换接近平衡。 - Special analysis is made to see the impact of different boundary layer parameterization schemes on some factors which affect the heavy rainfall such as vertical velocity , divergence , vorticity , divergence of water vapor flux , se field and so on
结果表明：复杂地形条件下，特别是降水有明显日变化的地区，边界层的作用是十分重要的，这在暴雨时的纬向垂直环流结构中表现地非常明显。 - 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。 - Climatological characteristics , which can provide some drought or flood years with large - scale background , are investigated for large - scale water vapor transport over asian - australian monsoon region based on vertically integrated water vapor flux by pentad from 1980 to 1997 . at the same time , the differences of moisture transport over the yangtze river basin between drought and flood and the moisture budgets over eastern china from april to september are examined . major results are as follows : i
使用1980 ? 1997年垂直积分的整层水汽输送通量资料，从气候平均的角度分析了亚澳季风区大尺度水汽输送演变和偏南风水汽输送在东亚地区推进的气候特征，为研究异常年份旱涝事件的产生提供了相应的大尺度背景；同时还讨论了长江流域旱涝年水汽输送的差异以及4 - 9月我国东部各区域的水分收支情况。 - The most obvious feature of the first leading term of eof applied to the climatic vertically integrated water vapor flux over asian - australian monsoon region shows a planetary - scale southwesterly moisture transport , starting from south hemisphere , passing over asian monsoon region and flowing into north pacific , which indicates the interaction between the northern and southern hemisphere as well as between mid and low latitudes in the northern hemisphere
( 3 )亚澳季风区气候平均状态下4 - 9月份的水汽通量的eof矢量展开的第一特征向量最显著的特征是存在一条行星尺度的强西南风水汽输送带，它源于南半球低纬地区，经过亚洲季风区，进入北太平洋地区，集中反映了南北半球和中低纬各支水汽输送气流的相互作用。