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高温热浪对大连市城市热岛变化特征影响分析

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高温热浪(heat wave,HW)事件频发加剧城市热岛(urban heat island,UHI)的负面影响,因此探究HW时期不同生长季UHI变化特征的差异对居民应对城市热胁迫具有重要意义.本文基于大连市主城区2018年和2019年生长季前中后期Landsat 8数据,对比分析热浪与非热浪(non-heat wave,NHW)期间 UHI 的差异,结合归一化植被指数(normalized difference vegetation index,NDVI)和归一化建筑指数(normalized difference build-up index,NDBI)进一步定量探讨地表覆被类型与城市热岛效应的关系.结果表明:①相比非热浪年,热浪年在生长季内均表现出明显的增温趋势,生长季中期地表温度(land surface temperature,LST)标准差降低了 0.3 ℃,说明2019年LST离散程度减小,LST变化趋于稳定.②HW对UHI的影响总体呈现出较为明显的促进作用.时间上,HW对应生长季中期热岛强度较NHW显著增强,较强热岛和弱热岛面积占比从非热浪年的12.8%和17.7%增长至热浪年的27.3%和21.2%;空间上,中心城区热岛强度最强,呈现由中心城区向周围扩散的趋势.③HW和NHW生长季内UHI与NDVI、NDBI存在明显相关关系(P<0.05).UHI与NDVI呈负相关关系,与NDBI呈正相关关系.生长季前期和后期,UHI主要受到NDVI和NDBI的共同影响,而在生长季中期,2018年UHI不仅受到NDVI和NDBI的影响,还受到高温热浪的影响.研究结果可为城市居民缓解城市热胁迫提供有效的科学支持和理论依据.
Analysis of the impact of high temperature heat wave on the characteristics of urban heat island change in Dalian City
Heat wave(HW)events frequently exacerbate the negative impacts of urban heat island(UHI),it is of great significance to investigate the differences in UHI variations during different growing seasons in the HW period for residents to cope with urban heat stress.Based on Landsat 8 data from the early,middle and late stages of the growing seasons of the 2018 and 2019 in the main city of Dalian,the differences in urban heat island(UHI)variations between heat wave and non-heat wave(NHW)periods are compared and analyzed in this study.By incorporating the normalized difference vegetation index(NDVI)and normalized difference built-up index(NDBI),the relationship between land surface cover types and urban heat island effects is further quantitatively explored.The results show that ① Compared to the non-heat wave years,the heat wave years all showed a significant warming trend throughout the growing season,and the standard deviation of LST decreased by 0.3 ℃ in the middle of the growing season,indicating that the LST dispersion decreased and the LST variation stabilized in 2019.(2)The effect of HW on UHI generally shows a more obvious promoting effect.Temporally,the heat island intensity in the middle of the growing season corresponding to HW is significantly stronger than NHW,and the area share of stronger heat island and weak heat island increases from 12.8%and 17.7%in non-heat wave years to 27.3%and 21.2%in heat wave years.Spatially,the heat island intensity is strongest in the central city,showing a trend of spreading from the central city to the surrounding area.(3)UHI is significantly correlated with NDVI and NDBI during the growing season for HW and NHW(P<0.05).UHI is negatively correlated with NDVI,it is also positively correlated with NDBI.In the early and late growing season,UHI is mainly influenced by both NDVI and NDBI together,while in the middle of the growing season in 2018,UHI is influenced not only by NDVI and NDBI,but also by high temperature heat waves.The findings of this study can provide effective scientific support and theoretical basis for urban residents to mitigate urban heat stress.

Urban heat islandHeat waveSurface temperatureLandsat

曹葛、金翠、张泽宇、候明璇

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辽宁师范大学地理科学学院,辽宁 大连 116029

城市热岛 热浪 地表温度 Landsat

辽宁省教育厅科学研究一般项目国家自然科学青年基金

LJKM2022141441801340

2024

河北省科学院学报
河北省科学院

河北省科学院学报

影响因子:0.176
ISSN:1001-9383
年,卷(期):2024.41(1)
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