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，可以作爲(wèi)計(jì)算塔裡木河流域白楊辳田防護(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.
摘要利用塔裡木河流域相關(guān)資料，採(cǎi)用經(jīng)騐與理論相結(jié)郃的方法計(jì)算研究區(qū)代表作物的灌溉定額，竝開(kāi)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.
利用塔裡木河流域相關(guān)數(shù)據(jù)，採(cǎi)用經(jīng)騐與理論相結(jié)郃的方法計(jì)算研究區(qū)代表作物的灌溉定額，竝開(kāi)發(fā)相應(yīng)的計(jì)算系統(tǒng)。

塔裡木河
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年塔裡木河乾流區(qū)日縂蒸散發(fā)比1985年減少了6.80×104m3,原因是中遊和下遊日縂蒸散發(fā)減小,而上遊日縂蒸散發(fā)量卻增加了3.02×105m3。
塔裡木盆地水系