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本文引用的文献

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2
Pakistan: High-rise buildings worsened heatwave.
Nature. 2015 Aug 6;524(7563):35. doi: 10.1038/524035e.
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Limitations to Thermoregulation and Acclimatization Challenge Human Adaptation to Global Warming.体温调节和适应能力的局限对人类适应全球变暖构成挑战。
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World population stabilization unlikely this century.本世纪世界人口不太可能稳定下来。
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Strong contributions of local background climate to urban heat islands.局地背景气候对城市热岛的强烈贡献。
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Development and implementation of South Asia's first heat-health action plan in Ahmedabad (Gujarat, India).印度古吉拉特邦艾哈迈达巴德市制定并实施南亚首个热健康行动计划。
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Heat-related mortality in India: excess all-cause mortality associated with the 2010 Ahmedabad heat wave.印度与高温相关的死亡率:2010年艾哈迈达巴德热浪引发的全因死亡率上升
PLoS One. 2014 Mar 14;9(3):e91831. doi: 10.1371/journal.pone.0091831. eCollection 2014.
8
Heat waves and health outcomes in Alabama (USA): the importance of heat wave definition.美国阿拉巴马州的热浪与健康结果:热浪定义的重要性
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9
Perception of climate change.气候变化感知。
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Rapid estimation of excess mortality: nowcasting during the heatwave alert in England and Wales in June 2011.快速估算超额死亡率:2011 年 6 月英格兰和威尔士热浪警报期间的实时预测。
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城市热岛与未来气候变化——对德里热的影响。

Urban Heat Island and Future Climate Change-Implications for Delhi's Heat.

机构信息

National Institute of Urban Affairs (NIUA), Delhi, India.

Vlaamse instelling voor technologisch onderzoek (VITO), Mol, Belgium.

出版信息

J Urban Health. 2019 Apr;96(2):235-251. doi: 10.1007/s11524-018-0322-y.

DOI:10.1007/s11524-018-0322-y
PMID:30353483
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC6458210/
Abstract

UrbClim, the urban climate model, is used for short- and long-term projections of climate for Delhi. The projections are performed for RCP8.5 using an ensemble of 11 GCM model outputs. Various heat stress indices were employed to understand the role of urban heat island (UHI) in influencing the present and future urban climate of the city. UHI intensity based on 5% warmest nights (TNp95) was 4.1 °C and exhibits negligible change over time. However, the impact of UHI on other heat stress indices is very strong. Combined hot days and tropical nights (CHT) that influenced 58-70% of the reference time frame are expected to rise to 68-77% in near-future and to 91-97% in far-future time periods. For reference time period, urban areas experience 2.3 more number of heat wave days (NHWD) than rural areas per summer season. This difference increases to 7.1 in short-term and 13.8 in long-term projections. Similar to this trend, frequency of heat waves (FHW) for urban areas is also expected to increase from 0.8 each summer season in reference time frame to 2.1 and 5.1 in short- and long-term projections. The urban-rural difference for duration of heat waves (DHW) appears to increase from 1.7 days in past to 2.3 and 2.2 days in future, illustrating that DHW for cities will be higher than non-urban areas at least by 2 days. The intensity of heat wave (IHW) for urban land uses increases from 40 °C in reference time frame to 45 °C in short-term projection to 49 °C in far future. These values for non-urban land use were 33 °C during the baseline time period and are expected to increase to 42 °C and 46 °C in near- and far-future time frames. The results clearly indicate the contribution of UHI effects in intensifying the impacts of extreme heat and heat stress in the city.

摘要

UrbClim 是一种城市气候模型,用于对德里的短期和长期气候进行预测。该预测是针对 RCP8.5 使用 11 个 GCM 模型输出的集合进行的。使用各种热应激指数来了解城市热岛 (UHI) 在影响城市当前和未来气候方面的作用。基于 5%最温暖夜晚的 UHI 强度 (TNp95) 为 4.1°C,并且随着时间的推移变化不大。然而,UHI 对其他热应激指数的影响非常大。在参考时间段内影响 58-70%的综合炎热日和热带夜晚 (CHT) 预计将在近期上升到 68-77%,在远期上升到 91-97%。对于参考时间段,城市地区每夏季经历的热浪日 (NHWD) 比农村地区多 2.3 天。这一差异在短期和长期预测中分别增加到 7.1 和 13.8。类似的趋势是,城市地区的热浪频率 (FHW) 也预计将从参考时间段每夏季的 0.8 次增加到 2.1 和 5.1 次。城市与农村之间热浪持续时间的差异 (DHW) 似乎从过去的 1.7 天增加到未来的 2.3 和 2.2 天,表明城市的 DHW 将比非城市地区至少高 2 天。城市土地利用的热浪强度 (IHW) 从参考时间段的 40°C 增加到短期预测的 45°C,再到远期的 49°C。非城市土地利用的相应值在基准时间段为 33°C,预计在近期和远期分别增加到 42°C 和 46°C。这些结果清楚地表明了城市热岛效应在加剧城市极端高温和热应激影响方面的贡献。