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Dominant control of agriculture and irrigation on urban heat island in India

机译:印度城市热岛上对农业和灌溉的主要控制

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摘要

As is true in many regions, India experiences surface Urban Heat Island (UHI) effect that is well understood, but the causes of the more recently discovered Urban Cool Island (UCI) effect remain poorly constrained. This raises questions about our fundamental understanding of the drivers of rural-urban environmental gradients and hinders development of effective strategies for mitigation and adaptation to projected heat stress increases in rapidly urbanizing India. Here we show that more than 60% of Indian urban areas are observed to experience a day-time UCI. We use satellite observations and the Community Land Model (CLM) to identify the impact of irrigation and prove for the first time that UCI is caused by lack of vegetation and moisture in non-urban areas relative to cities. In contrast, urban areas in extensively irrigated landscapes generally experience the expected positive UHI effect. At night, UHI warming intensifies, occurring across a majority (90%) of India’s urban areas. The magnitude of rural-urban temperature contrasts is largely controlled by agriculture and moisture availability from irrigation, but further analysis of model results indicate an important role for atmospheric aerosols. Thus both land-use decisions and aerosols are important factors governing, modulating, and even reversing the expected urban-rural temperature gradients.
机译:正如许多地区的情况一样,印度经历了表面的城市热岛效应(UHI),这一点已广为人知,但最近发现的城市酷热岛(UCI)效应的起因仍然受限制。这引起了人们对我们对城乡环境梯度驱动因素的基本理解的疑问,并阻碍了在迅速城市化的印度缓解和适应预计的热应力增加的有效策略的发展。在这里,我们显示观察到超过60%的印度城市地区经历了白天的UCI。我们使用卫星观测和社区土地模型(CLM)来识别灌溉的影响,并首次证明UCI是由于相对于城市而言,非城市地区缺乏植被和水分造成的。相反,大面积灌溉的城市地区通常会遇到预期的UHI积极影响。到了晚上,印度大部分地区(90%)的UHI变暖加剧。城乡温度差异的大小主要由农业和灌溉的水分供应控制,但是对模型结果的进一步分析表明,大气气溶胶具有重要作用。因此,土地利用决策和气溶胶都是控制,调节甚至逆转预期的城乡温度梯度的重要因素。

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