tarim river basin

基本解釋

The result revealed that the model had high precision and could be used to calculate the evapotranspiration in aspen shelter belt of the Tarim River basin.
結(jié)果表明，該模式計(jì)算精度較高，可以作為計(jì)算塔里木河流域白楊農(nóng)田防護(hù)林蒸散量的一種方法而使用。
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Based on the data of tarim river basin this paper combines experiential and academic methods to calculate the irrigation quota of representative crops and develops relevant calculation system.
摘要利用塔里木河流域相關(guān)資料，采用經(jīng)驗(yàn)與理論相結(jié)合的方法計(jì)算研究區(qū)代表作物的灌溉定額，并開發(fā)相應(yīng)的計(jì)算系統(tǒng)。
Based on the data of Tarim River basin, this paper combines experiential and academic methods to calculate the irrigation quota of representative crops, and develops relevant calculation system.
利用塔里木河流域相關(guān)數(shù)據(jù)，采用經(jīng)驗(yàn)與理論相結(jié)合的方法計(jì)算研究區(qū)代表作物的灌溉定額，并開發(fā)相應(yīng)的計(jì)算系統(tǒng)。

塔里木河
The total evapotranspiration in the Tarim River basin in 2000 decreased by 6.80×104 m3 compared with in 1985,because the total daily evapotranspiration in the middle and lower reaches decreased while the upper reaches increased by 3.02×105 m3.
2000年塔里木河干流區(qū)日總蒸散發(fā)比1985年減少了6.80×104m3,原因是中游和下游日總蒸散發(fā)減小,而上游日總蒸散發(fā)量卻增加了3.02×105m3。
塔里木盆地水系