关键词: Climate change Evapotranspiration Urban agglomeration Urbanization

来  源:   DOI:10.1016/j.scitotenv.2024.175399

Abstract:
Evaluating the differences in evapotranspiration between urban and surrounding non-urban areas (i.e., ∆ET) has critical implications for urban ecological planning and water resources management. However, it is unclear how the magnitude of changes in ∆ET caused by urbanization varies under different climatic conditions in China. Here, using the remotely ET estimates at 1 km spatial resolution, we firstly estimated the magnitude of changes in ∆ET and then quantified the main driving factors influencing variations in ∆ET of 7 national-level urban agglomerations (UAs) across China during 2003-2020. Results showed that all annual ETurban values were smaller than ETnon-urban of 7 UAs, and the absolute ∆ET values of cities in South China were generally higher than those in North China. There is an apparent effect of urbanization on ∆ET increase in Guanzhong Plain City Group, Central Plain UA and Guangdong-Hong Kong-Macao Greater Bay Area (GHKMGBA), while ∆ET decrease in Chengdu-Chongqing City Group and Yangtze River Delta (YRDUA) were primarily due to the climate change. The suppressing effects of temperature and NDVI on ∆ET decrease in YRDUA were enhanced, and the promoting effect of GDP on ∆ET increase in GHKMGBA was weakened. Considering nonstationary features, urbanization appears to heighten extreme ∆ET by 0.83 %, 4.83 % and 10.39 % under 5-year, 20-year, and 50-year return periods over all the 7 UAs, respectively. Collectively, our findings confirm that urbanization is a significant factor that leads to ∆ET increase, and the factors affecting the response of urban water circulation system need to be deeply decomposed.
摘要:
评估城市和周围非城市地区的蒸散量差异(即,ΔET)对城市生态规划和水资源管理具有至关重要的意义。然而,目前尚不清楚在中国不同的气候条件下,城市化引起的ΔET变化的幅度如何变化。这里,使用1公里空间分辨率的远程ET估计,我们首先估计了ΔET的变化幅度,然后量化了2003-2020年中国7个国家级城市群(UAs)影响ΔET变化的主要驱动因素。结果表明,所有年度ETnurban值均小于ETnon-urban的7个UA,华南地区城市的ΔET绝对值普遍高于华北地区。城市化对关中平原城市群ET增长有明显影响,中原UA和粤港澳大湾区(GHKMGBA),而成渝城市群和长江三角洲(YRDUA)的ET下降主要是由于气候变化。温度和NDVI对YRDUAET降低的抑制作用增强,GDP对GHKMGBAΔET增长的促进作用减弱。考虑到非平稳特征,城市化似乎使极端ΔET提高了0.83%,5年期以下4.83%和10.39%,20年,以及所有7个UA的50年回报期,分别。总的来说,我们的研究结果证实,城市化是导致ΔET增加的重要因素,影响城市水循环系统响应的因素需要深入分解。
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