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Characterizing the Hourly Variation of Urban Heat Islands in a Snowy Climate City during Summer

机译:表征白雪皑皑气候城市夏季城市热岛的小时变化

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摘要

Temporal variation of urban heat island (UHI) intensity is one of the most important themes in UHI studies. However, fine-scale temporal variability of UHI with explicit spatial information is sparse in the literature. Based on the hourly air temperature from 195 meteorological stations during August 2015 in Changchun, China, hourly spatiotemporal patterns of UHI were mapped to explore the temporal variability and the effects of land use on the thermal environment using time series analysis, air temperature profiling, and spatial analysis. The results showed that: (1) high air temperature does not indicate strong UHI intensity. The nighttime UHI intensity (1.51 °C) was much stronger than that in the daytime (0.49 °C). (2) The urban area was the hottest during most of the day except the period from late morning to around 13:00 when there was about a 40% possibility for an “inverse UHI intensity” to appear. Paddy land was the coolest in the daytime, while woodland had the lowest temperature during the nighttime. (3) The rural area had higher warming and cooling rates than the urban area after sunrise and sunset. It appeared that 23 °C was the threshold at which the thermal characteristics of different land use types changed significantly.
机译:城市热岛(UHI)强度的时间变化是UHI研究中最重要的主题之一。但是,文献中稀疏的具有明确的空间信息的UHI的时间尺度细小变化。基于2015年8月中国长春市195个气象站的每小时气温,绘制了UHI的时空时空分布图,以利用时间序列分析,气温廓线和空间分析。结果表明:(1)气温高并不表明UHI强。夜间UHI强度(1.51°C)比白天(0.49°C)强得多。 (2)除从清晨到13:00左右这段时间外,市区大部分时间最热,那里大约有40%的可能性出现“逆UHI强度”。白天的稻田最凉爽,而夜间的林地温度最低。 (3)日出和日落后,农村地区的升温和降温速率均高于城市地区。似乎23°C是不同土地利用类型的热特性发生显着变化的阈值。

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