Temporal Variability of an Urban Heat Island in Yekaterinburg

A. A. Gornostaeva, D. Demezhko, B. D. Khatskevich
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Abstract

The article deals with the analysis of temporal variability of the urban heat island (UHI) in the field of surface air temperatures in Yekaterinburg using the data on meteorological observations on weather stations “Yekaterinburg” and “Verkhnee Dubrovo”. The UHI intensity variations have been analyzed for the periods from annual/interannual to diurnal. The sustainable effect of the urban heat island is manifested in all seasons. Annual cycles of monthly averaged UHI values demonstrates “W”-shaped form with maxima of about 1.0 ºС in February/March and in three summer months. Summer maximum is generally determined by maximal diurnal (night) UHI values. The maximum in February/March is related to the increased minimum daily values. From the 50s of the 20th century “W”-shaped annual curve of the UHI intensity remained unchanged under the increase in mean annual UHI values while growing at a rate of 1.31 ºС/100 years to the beginning of the 80s. At the same time, summer maximum increased at a faster rate in comparison with the winter one. Since the beginning of the 80s, the mean annual UHI intensity has stabilized at the level of 0.8 ºС. In a diurnal cycle, the maximal UHI intensity (to 2.4 ºС) is observed in May-July after the sunset. Maximal daily UHI intensity values in summer months are associated with a slower cooling of the city in high-rise building area. The local afternoon maximum (up to 0.8 ºС) caused by the insolation maximum under low albedo value of the urban coverage occurs also from May to July. In the autumn-winter period and at the beginning of spring, the daily amplitude of the UHI intensity decreases due to a decrease in the maximum of UHI and a slight increase in the minimum one. The increase in the minimum UHI values is facilitated by cloudiness, snow cover, calm wind conditions, an increase in the concentration of aerosol and water vapor near the surface and anthropogenic heat emissions. The study results can be used in fundamental and applied climatology, in the development of urban policy.
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叶卡捷琳堡城市热岛的时间变率
本文利用“Yekaterinburg”和“Verkhnee Dubrovo”气象站的气象观测资料,分析了叶卡捷琳堡地表气温场的城市热岛(UHI)的时间变率。从年/年际到日,分析了热岛强度的变化。城市热岛的持续效应在各个季节都表现出来。月平均热岛指数的年周期呈“W”形,2月/ 3月和夏季三个月的最大值约为1.0ºС。夏季最大值通常由最大日(夜)热岛热岛值决定。2月/ 3月的最大值与每日最低值的增加有关。20世纪50年代至80年代初,热岛强度的年“W”型曲线在年平均热岛值的增加下保持不变,以1.31ºС/100年的速率增长。与此同时,夏季极大值的增加速度要快于冬季极大值。80年代以来,年平均热岛强度稳定在0.8ºС水平。在日循环中,最大热岛强度(至2.4ºС)出现在日落后的5 - 7月。夏季最大日热岛强度值与高层建筑区域城市降温速度较慢有关。城市覆盖低反照率下的日照最大值引起的局地午后最大值(0.8ºС)也出现在5 ~ 7月。秋冬期和春初,热岛强度日幅值减小,最大热岛强度减小,最小热岛强度略有增大。云量、积雪、无风条件、近地表气溶胶和水汽浓度的增加以及人为热排放促进了最低热岛值的增加。研究结果可用于基础气候学和应用气候学,以及城市政策的制定。
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