Abstract

Rapid urbanization leads to changes in urban micro meteorology, such as the urban heat island effect and rain island effect, which eventually brings about urban waterlogging and other problems. In this study, the data of precipitation, temperatures and impervious surfaces with long series and high resolution are used to study the rain island effect in Jinan City, China. MK-Sen’s slope estimator, Pettitt test and Pearson correlation analysis are used to quantitatively analyze the impact of urban expansion on extreme climate indices. The results show that Jinan City has experienced rapid urbanization since the 1978 economic reform, and the impervious surface areas have increased from 311.68 km2 (3.04%) in 1978 to 2389.50 km2 (23.33%) in 2017. Urban expansion has a significant impact on temperature, with large variations in extreme temperature indices over the intensive construction area relative to the sparse construction area. The extreme temperature indices have a significant correlation with impervious surfaces. Jinan City shows a certain degree of rain island effect, which seems to be spatially correlated with the urban heat island effect. The frequency of short-duration precipitation events significantly increases and the intensity of precipitation events generally increases. The magnitude and frequency of extreme precipitation indices in the intensive construction area significantly increase when compared to that in the sparse construction area, and they have a significant correlation with impervious surfaces. There is a tendency that Jinan City’s rainfall center moves towards to the intensive construction area.

Highlights

  • Urbanization is commonly pursued by all countries to achieve social and economic modernization

  • The results show that the distribution of extreme precipitation is related to the urbanization process in Jinan City

  • Their results indicate that the changes in extreme precipitation in urban areas are related to urban expansion

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Summary

Introduction

Urbanization is commonly pursued by all countries to achieve social and economic modernization. In 2018, 55% of the world’s population was recorded to live in urban areas, a proportion that is expected to increase to 68% by 2050, and it is expected that the growth of the world’s urban population will be highly concentrated in a few countries, such as. Urbanization inevitably leads to variations in near-surface material and energy balance and affects local atmospheric circulations [3]. The analysis of regional climate change caused by urban expansion has been the subject of numerous studies in the past decade [4,5]. The impact of urbanization on regional climate is due to variations in atmospheric thermal, dynamic and chemical components [6,7].

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