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阿尔伯塔省人口最多的两个城市的城市热岛效应及其影响因素。

Urban Warming of the Two Most Populated Cities in the Canadian Province of Alberta, and Its Influencing Factors.

机构信息

Department of Geomatics Engineering, Schulich School of Engineering, University of Calgary, 2500 University Dr. NW, Calgary, AB T2N 1N4, Canada.

Spatial Sciences Discipline, School of Earth and Planetary Sciences, Curtin University, Bentley, WA 6102, Australia.

出版信息

Sensors (Basel). 2022 Apr 9;22(8):2894. doi: 10.3390/s22082894.

Abstract

Continuous urban expansion transforms the natural land cover into impervious surfaces across the world. It increases the city's thermal intensity that impacts the local climate, thus, warming the urban environment. Surface urban heat island (SUHI) is an indicator of quantifying such local urban warming. In this study, we quantified SUHI for the two most populated cities in Alberta, Canada, i.e., the city of Calgary and the city of Edmonton. We used the moderate resolution imaging spectroradiometer (MODIS) acquired land surface temperature (LST) to estimate the day and nighttime SUHI and its trends during 2001-2020. We also performed a correlation analysis between SUHI and selected seven influencing factors, such as urban expansion, population, precipitation, and four large-scale atmospheric oscillations, i.e., Sea Surface Temperature (SST), Pacific North America (PNA), Pacific Decadal Oscillation (PDO), and Arctic Oscillation (AO). Our results indicated a continuous increase in the annual day and nighttime SUHI values from 2001 to 2020 in both cities, with a higher magnitude found for Calgary. Moreover, the highest value of daytime SUHI was observed in July for both cities. While significant warming trends of SUHI were noticed in the annual daytime for the cities, only Calgary showed it in the annual nighttime. The monthly significant warming trends of SUHI showed an increasing pattern during daytime in June, July, August, and September in Calgary, and March and September in Edmonton. Here, only Calgary showed the nighttime significant warming trends in March, May, and August. Further, our correlation analysis indicated that population and built-up expansion were the main factors that influenced the SUHI in the cities during the study period. Moreover, SST indicated an acceptable relationship with SUHI in Edmonton only, while PDO, PNA, and AO did not show any relation in either of the two cities. We conclude that population, built-up size, and landscape pattern could better explain the variations of the SUHI intensity and trends. These findings may help to develop the adaptation and mitigating strategies in fighting the impact of SUHI and ensure a sustainable city environment.

摘要

持续的城市扩张将自然土地覆盖物转变为世界各地的不透水面。这增加了城市的热强度,影响了当地气候,从而使城市环境变暖。地表城市热岛 (SUHI) 是量化这种局部城市变暖的指标。在这项研究中,我们量化了加拿大阿尔伯塔省人口最多的两个城市,即卡尔加里市和埃德蒙顿市的 SUHI。我们使用中等分辨率成像光谱仪 (MODIS) 获得的地表温度 (LST) 来估计白天和夜间的 SUHI 及其在 2001-2020 年期间的趋势。我们还对 SUHI 与七个选定影响因素(如城市扩张、人口、降水和四个大气大规模振荡,即海表温度 (SST)、北美太平洋 (PNA)、太平洋年代际振荡 (PDO) 和北极涛动 (AO))之间进行了相关性分析。我们的结果表明,这两个城市的年白天和夜间 SUHI 值从 2001 年到 2020 年持续增加,卡尔加里的增幅更大。此外,这两个城市的白天 SUHI 值最高值出现在 7 月。虽然这两个城市的年白天 SUHI 都有显著的变暖趋势,但只有卡尔加里的年夜间 SUHI 显示出这种趋势。SUHI 的月度显著变暖趋势在 6 月、7 月、8 月和 9 月在卡尔加里呈增加模式,在 3 月和 9 月在埃德蒙顿呈增加模式。在这里,只有卡尔加里在 3 月、5 月和 8 月显示出夜间显著变暖趋势。此外,我们的相关性分析表明,人口和建成区扩张是研究期间影响这两个城市 SUHI 的主要因素。此外,SST 仅与埃德蒙顿的 SUHI 呈可接受的关系,而 PDO、PNA 和 AO 在这两个城市中均无关系。我们的结论是,人口、建成区规模和景观格局可以更好地解释 SUHI 强度和趋势的变化。这些发现可能有助于制定应对 SUHI 影响的适应和缓解策略,并确保城市环境的可持续性。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/25c6/9032056/2d5499a6e0c2/sensors-22-02894-g001.jpg

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