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Two Challenges for U.S. Irrigation Due to Climate Change: Increasing Irrigated Area in Wet States and Increasing Irrigation Rates in Dry States

机译:由于气候变化美国灌溉面临的两个挑战:潮湿国家的灌溉面积增加和干旱国家的灌溉速率增加

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摘要

Agricultural irrigation practices will likely be affected by climate change. In this paper, we use a statistical model relating observed water use by U.S. producers to the moisture deficit, and then use this statistical model to project climate changes impact on both the fraction of agricultural land irrigated and the irrigation rate (m3ha−1). Data on water withdrawals for US states (1985–2005) show that both quantities are highly positively correlated with moisture deficit (precipitation – PET). If current trends hold, climate change would increase agricultural demand for irrigation in 2090 by 4.5–21.9 million ha (B1 scenario demand: 4.5–8.7 million ha, A2 scenario demand: 9.1–21.9 million ha). Much of this new irrigated area would occur in states that currently have a wet climate and a small fraction of their agricultural land currently irrigated, posing a challenge to policymakers in states with less experience with strict regulation of agriculture water use. Moreover, most of this expansion will occur in states where current agricultural production has relatively low market value per hectare, which may make installation of irrigation uneconomical without significant changes in crops or practices by producers. Without significant increases in irrigation efficiency, climate change would also increase the average irrigation rate from 7,963 to 8,400–10,415 m3ha−1 (B1 rate: 8,400–9,145 m3ha−1, A2 rate: 9,380–10,415 m3ha−1). The irrigation rate will increase the most in states that already have dry climates and large irrigation rates, posing a challenge for water supply systems in these states. Accounting for both the increase in irrigated area and irrigation rate, total withdrawals might increase by 47.7–283.4 billion m3 (B1 withdrawal: 47.7–106.0 billion m3, A2 withdrawal: 117.4–283.4 billion m3). Increases in irrigation water-use efficiency, particularly by reducing the prevalence of surface irrigation, could eliminate the increase in total irrigation withdrawals in many states.
机译:农业灌溉方式可能会受到气候变化的影响。在本文中,我们使用统计模型,将美国生产者观察到的用水量与水分赤字相关联,然后使用该统计模型来预测气候变化对农田灌溉比例和灌溉率的影响(m 3 ha −1 )。美国各州(1985–2005年)的取水数据表明,这两个数量均与水分亏缺(降水– PET)高度正相关。如果保持目前的趋势,气候变化将使2090年的农业灌溉需求增加4.5-2190万公顷(B1情景需求:4.5-870万公顷,A2情景需求:9.1-2190万公顷)。这种新的灌溉区大部分将发生在气候潮湿的州,而其农业用地的一小部分正在灌溉,这给缺乏严格控制农业用水经验的州的决策者带来了挑战。此外,这种扩张的大部分将发生在当前农业生产每公顷市场价值相对较低的州,这可能使灌溉设施的安装不经济,而生产者的作物或作法没有重大变化。如果没有显着提高灌溉效率,气候变化还将使平均灌溉率从7,963增加到8,400–10,415 m 3 ha -1 (B1比率:8,400–9,145 m < sup> 3 ha -1 ,A2速率:9,380–10,415 m 3 ha -1 )。在已经有干旱气候和大灌溉率的州,灌溉率将增加最多,这对这些州的供水系统构成了挑战。考虑到灌溉面积和灌溉速率的增加,总取水量可能会增加47.7–2834亿m 3 (B1取水量:477–1060亿m 3 ,A2取水量:117.4–2834亿m 3 )。提高灌溉用水效率,特别是通过减少地表灌溉的发生率,可以消除许多州灌溉总取水量的增加。

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