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探索快速发展城市中的城市增长-气候变化-洪水风险关系。

Exploring urban growth-climate change-flood risk nexus in fast growing cities.

机构信息

Division of Sustainable Development, College of Science and Engineering, Hamad Bin Khalifa University, Qatar Foundation, Doha, Qatar.

出版信息

Sci Rep. 2022 Jul 18;12(1):12265. doi: 10.1038/s41598-022-16475-x.

DOI:10.1038/s41598-022-16475-x
PMID:35851608
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC9293981/
Abstract

This study looks at the nexus between urban growth, climate change, and flood risk in Doha, Qatar, a hot-spot, climate change region that has experienced unprecedented urban growth during the last four decades. To this end, this study overviews the main stages of Doha's urban growth and influencing climatic factors during this period. A physically-based hydrological model was then built to simulate surface runoff and quantify flood risk. Finally, the Pearson correlation was used to verify the potential nexus between flood risk, climate change, and urban growth. Surveying showed that, between 1984 and 2020, urban areas grew by 777%, and bare lands decreased by 54.7%. In addition, Doha witnessed various climatic changes with a notable increase in air temperature (+ 8.7%), a decrease in surface wind speed (- 19.5%), and a decrease in potential evapotranspiration losses (- 33.5%). Growth in urban areas and the perturbation of climatic parameters caused runoff to increase by 422%, suggesting that urban growth contributed more than climatic parameters. Pearson correlation coefficient between flood risk and urban growth was strong (0.83) and significant at p < 0.05. Flood risk has a strong significant positive (negative) correlation with air temperature (wind speed) and a moderate positive (negative) correlation with precipitation (potential evapotranspiration). These results pave the way to integrate flood risk reduction measures in local urban development and climate change adaptation plans.

摘要

本研究探讨了卡塔尔多哈市城市增长、气候变化和洪水风险之间的关系,多哈是气候变化热点地区,在过去四十年经历了前所未有的城市增长。为此,本研究概述了多哈城市增长的主要阶段及其在此期间的主要气候影响因素。然后,建立了一个基于物理的水文模型来模拟地表径流并量化洪水风险。最后,使用皮尔逊相关系数验证了洪水风险、气候变化和城市增长之间的潜在关系。调查显示,1984 年至 2020 年间,城市面积增长了 777%,裸地减少了 54.7%。此外,多哈还经历了各种气候变化,空气温度显著上升(+8.7%),地表风速显著下降(-19.5%),潜在蒸散损失减少(-33.5%)。城市地区的增长和气候参数的干扰导致径流量增加了 422%,这表明城市增长的影响大于气候参数。洪水风险与城市增长之间的皮尔逊相关系数很强(0.83),在 p < 0.05 时显著。洪水风险与空气温度(风速)呈强显著正(负)相关,与降水(潜在蒸散)呈中度正(负)相关。这些结果为在当地城市发展和气候变化适应计划中纳入洪水风险降低措施铺平了道路。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5090/9293981/8df6b2039be9/41598_2022_16475_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5090/9293981/ec1c83f5aa6b/41598_2022_16475_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5090/9293981/26e14bbb9c3c/41598_2022_16475_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5090/9293981/2b22e6b724f5/41598_2022_16475_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5090/9293981/28eebfcc0446/41598_2022_16475_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5090/9293981/1aef83285d43/41598_2022_16475_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5090/9293981/8df6b2039be9/41598_2022_16475_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5090/9293981/ec1c83f5aa6b/41598_2022_16475_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5090/9293981/26e14bbb9c3c/41598_2022_16475_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5090/9293981/2b22e6b724f5/41598_2022_16475_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5090/9293981/28eebfcc0446/41598_2022_16475_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5090/9293981/1aef83285d43/41598_2022_16475_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/5090/9293981/8df6b2039be9/41598_2022_16475_Fig6_HTML.jpg

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