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Irrigation impact on annual water balance of the oases in Tarim Basin, Northwest China

机译:灌溉对西北塔里木盆地绿洲年水分平衡的影响

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By taking the sum of annual precipitation and lateral water input (in which irrigation water withdrawal is the main component)nfor water availability, the Budyko hypothesis and Fu’s formula derived from it was extended to the study of oases in the TarimnBasin, Northwest China. For both long-term (multi-year) and annual values on water balances in the 26 oases subregions, thenextended Fu’s formula was confirmed. Regional patterns on water balance on the 26 oases subregions were related to changenin land-use types due to increased area for irrigation. Moreover, an empirical formula for the parameter was established tonreflect the influences of change in land use on water balance. The extended Budyko framework was employed to evaluatenthe impact of irrigation variability on annual water balance. According to the multi-year mean timescale, variabilities innactual evapotranspiration in the oases were mainly controlled by variability in irrigation water withdrawal rather than potentialnevapotranspiration. The influences of variability on potential evapotranspiration became increasingly apparent together withnincreases in irrigation water withdrawal. Copyright  2010 John Wiley & Sons, Ltd..
机译:通过将年降水量和侧向水输入量(灌溉用水是主要组成部分)的总和用于水的可利用性,将Budyko假说和由此得出的Fu公式推广到中国西北塔里木盆地的绿洲研究中。对于26个绿洲次区域的长期(多年)和年度水平衡值,都确定了Fu的扩展公式。由于灌溉面积的增加,26个绿洲次区域的水平衡区域格局与土地利用类型的变化有关。此外,建立了该参数的经验公式,以反映土地利用变化对水平衡的影响。扩展的Budyko框架用于评估灌溉变化对年度水平衡的影响。根据多年平均时间尺度,绿洲中实际蒸散量的变化主要受灌溉用水量的变化控制,而不是潜在的蒸散量。可变性对潜在蒸散的影响随着灌溉用水量的增加而越来越明显。版权所有©2010 John Wiley&Sons,Ltd.。

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