water vapor flux 中文意思是什麼
water vapor flux
解釋
水氣通量-
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年垂直積分的整層水汽輸送通量資料，從氣候平均的角度分析了亞澳季風區大尺度水汽輸送演變和偏南風水汽輸送在東亞地區推進的氣候特徵，為研究異常年份旱澇事件的產生提供了相應的大尺度背景；同時還討論了長江流域旱澇年水汽輸送的差異以及4 - 9月我國東部各區域的水分收支情況。 -
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（區） 168個站1961 2000年6 9月（主汛期）月平均降水、溫度資料，運用eof 、 reof 、小波分析等方法診斷了主汛期月降水異常和旱澇的年代際變化；同時利用ncep ncar月平均資料，分析了強（弱）季風年西北空中水汽通量及其散度場、 500hpa高度場、 u 、 v風場的演變特徵，結果表明： （ a ）西北汛期降水可分為七個氣候異常區，第一、三異常區旱澇趨勢相同。 -
When the southwesterly ( northeasterly ) moisture flux over southern china and its vicinity increased, then more ( less ) water vapor was transported from the low latitudes to the atmosphere over southern china, which resulted in strong ( weak ) atmospheric moisture sinks over the above - regions in southern china
華南中東部以及廣西北音隊湖南西部貴州東部地區水汽匯的強度異常與東亞上空水汽輸送異常導致上述地區垂直積分的水汽通量輻合的異常密切相關，當中國南方上空有西南（東北）風水汽通量距平，即西南風水汽輸送增強（減弱）時，則上述地區上空的水汽匯偏強（偏弱） 。 -
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
結果表明：復雜地形條件下，特別是降水有明顯日變化的地區，邊界層的作用是十分重要的，這在暴雨時的緯向垂直環流結構中表現地非常明顯。 -
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 ）亞澳季風區氣候平均狀態下4 - 9月份的水汽通量的eof矢量展開的第一特徵向量最顯著的特徵是存在一條行星尺度的強西南風水汽輸送帶，它源於南半球低緯地區，經過亞洲季風區，進入北太平洋地區，集中反映了南北半球和中低緯各支水汽輸送氣流的相互作用。 -
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年來1 、 4 、 7 、 10各月份西北地區大氣水分和水汽平均輸送的季節性氣候特徵。 -
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，對上世紀90年代西北地區重大幹旱事件期間大氣可降水量、水汽輸送等進行了分析，並與典型濕年進行對比，從大氣水分特徵的角度探討了這次重大幹旱事件的可能形成原因。 -
The real land surface is of multiple scales heterogeneity, which controls the exchanges of air - land momentum, heat flux, water vapor and other green house gases
真實的自然陸面具有多重尺度的非均勻性，這種陸面特徵決定了地-氣之間動量、熱量、水汽和其它溫室氣體交換的強弱。
分享友人