Urban Heat Load in a Small Mediterranean City in Recent, Extreme and Future Climate Conditions—A Case Study for the City of Dubrovnik

IF 2.8 3区 地球科学 Q2 METEOROLOGY & ATMOSPHERIC SCIENCES International Journal of Climatology Pub Date : 2024-12-19 DOI:10.1002/joc.8728
Marijana Boras, Ivana Herceg-Bulić, Matej Žgela
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Abstract

This article examines the urban heat load (UHL) of Dubrovnik, a small Mediterranean city located in the complex terrain of the eastern Adriatic coast. In the study, the characteristics of the UHL are investigated in three special scenarios that mimic the different climate conditions: the recent climate (1981–2010), the hypothetical extreme climate (consisting of the 10 years with the hottest summers in the period 1961–2021) and the future climate (2041–2070) according to the RCP4.5 scenario. The UHL is quantified in terms of climate indices with fixed thresholds, defined as the annual number of days on which the daily minimum or maximum temperature exceeds certain thresholds. The analysis was carried out using the microscale urban climate model MUKLIMO_3. In addition, the potential benefits of certain measures to reduce UHL were investigated. In relation to the recent climate, the results show an increase in the amplitude of UHL under extreme and future climate conditions, with the UHL being strongest under the projected future climate conditions. In all three scenarios, the UHL is the highest in the built-up parts of the city. However, a strong increase in UHL is obtained in the green parts of the domain indicating a possible reduction in the cooling capacity of green areas under warmer climate conditions. Applied land use/land cover (LULC) changes of the model area, which include changes in the albedo of roofs, the proportion of low vegetation, impervious surfaces and built-up areas, have some influence on the reduction of UHL, but their effect is quite weak and mostly local. The greatest effect on reducing diurnal UHL is achieved by changing albedo, while the most effective reduction in nocturnal UHL is achieved by a combination of changes in albedo, the proportion of low vegetation, impervious surfaces and built-up areas. Considering the relatively weak cooling effect of the LULC modifications and the potential reduction in vegetation efficiency under warmer climate conditions as well as the expected increase in heatwaves, it is likely that Dubrovnik will suffer from extremely high UHL in the future.

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地中海小城市在近期、极端和未来气候条件下的城市热负荷——以杜布罗夫尼克市为例
杜布罗夫尼克是一座地中海小城,位于亚得里亚海东部海岸的复杂地形中,本文研究了杜布罗夫尼克的城市热负荷(UHL)。在这项研究中,对三种模拟不同气候条件的特殊情景下的 UHL 特性进行了调查:近期气候(1981-2010 年)、假设极端气候(由 1961-2021 年期间夏季最热的 10 年组成)以及根据 RCP4.5 情景的未来气候(2041-2070 年)。UHL 以具有固定阈值的气候指数进行量化,定义为日最低气温或最高气温超过特定阈值的年天数。该分析是利用微尺度城市气候模型 MUKLIMO_3 进行的。此外,还调查了减少 UHL 的某些措施的潜在效益。与近期气候相比,结果表明在极端气候和未来气候条件下,UHL 的振幅会增大,而在预测的未来气候条件下,UHL 的振幅最大。在所有三种情况下,城市建成区的 UHL 都是最高的。然而,在该区域的绿地中,UHL 出现了大幅增加,这表明在气候变暖的条件下,绿地的冷却能力可能会降低。模型区域中应用的土地利用/土地覆盖(LULC)变化,包括屋顶反照率、低植被比例、不透水表面和建筑区的变化,对减少 UHL 有一定影响,但其影响相当微弱,而且大多是局部的。改变反照率对减少昼间 UHL 的影响最大,而减少夜间 UHL 最有效的方法是综合改变反照率、低植被比例、不透水表面和建筑密集区。考虑到土地利用、土地利用变化和植被变化的降温效果相对较弱,在气候变暖的条件下植被效率可能会降低,以及热浪预计会增加,杜布罗夫尼克未来很可能会遭受极高的 UHL。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
International Journal of Climatology
International Journal of Climatology 地学-气象与大气科学
CiteScore
7.50
自引率
7.70%
发文量
417
审稿时长
4 months
期刊介绍: The International Journal of Climatology aims to span the well established but rapidly growing field of climatology, through the publication of research papers, short communications, major reviews of progress and reviews of new books and reports in the area of climate science. The Journal’s main role is to stimulate and report research in climatology, from the expansive fields of the atmospheric, biophysical, engineering and social sciences. Coverage includes: Climate system science; Local to global scale climate observations and modelling; Seasonal to interannual climate prediction; Climatic variability and climate change; Synoptic, dynamic and urban climatology, hydroclimatology, human bioclimatology, ecoclimatology, dendroclimatology, palaeoclimatology, marine climatology and atmosphere-ocean interactions; Application of climatological knowledge to environmental assessment and management and economic production; Climate and society interactions
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