Differentiated Effects of Urbanization on Precipitation in South China

In this paper, precipitation data from the Tropical Rainfall Measuring Mission (TRMM), together with atmospheric reanalysis data, are employed to identify warm-season precipitation (1998–2014) changes and their association with rapid urbanization in south China. Three urban clusters (Chenyu, Yangtze...

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Main Authors: Lingli Fan, Guangya Zhang, Jianjun Xu
Format: Article
Language:English
Published: MDPI AG 2021-05-01
Series:Water
Subjects:
Online Access:https://www.mdpi.com/2073-4441/13/10/1386
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spelling doaj-61de06fdcdc440d1a3c394cb3f34a8232021-06-01T00:11:30ZengMDPI AGWater2073-44412021-05-01131386138610.3390/w13101386Differentiated Effects of Urbanization on Precipitation in South ChinaLingli Fan0Guangya Zhang1Jianjun Xu2College of Ocean and Meteorology, South China Sea Institute of Marine Meteorology, Guangdong Ocean University, Zhanjiang 524088, ChinaEducation Information Center, Guangdong Ocean University, Zhanjiang 524088, ChinaCollege of Ocean and Meteorology, South China Sea Institute of Marine Meteorology, Guangdong Ocean University, Zhanjiang 524088, ChinaIn this paper, precipitation data from the Tropical Rainfall Measuring Mission (TRMM), together with atmospheric reanalysis data, are employed to identify warm-season precipitation (1998–2014) changes and their association with rapid urbanization in south China. Three urban clusters (Chenyu, Yangtze Delta, and Fujian Guangdong coast) are focused. The results reveal that, for the inland Chengyu urban cluster, a lack of precipitation trend is likely due to insignificant trends in convective available potential energy (CAPE) and total column water vapor (TCWV). They are likely resulted from a reduced local moisture recycling in urban areas, balanced by an increased evapotranspiration of rural areas, together with a stable advection of water vapor input. For the Yangtze River Delta urban cluster, a negative trend in precipitation is associated with a slightly decreased CAPE and an increased TCWV, but is very likely related to urbanization induced an increased planetary boundary layer (PBL) and reduced land surface evaporation. For the Fujian Guangdong coast urban cluster, a marked positive precipitation trend is well explained by positive trends in CAPE and TCWV. The increased precipitation likely benefits from enhanced moisture recycling due to improved vegetation cover in rural areas, and enhanced advection moisture inputs due to urbanization along the coast. These results suggest urbanization effects on precipitation vary with regional conditions. In the coastal area, urbanization enhances sea breezes, which may benefit precipitation if sea breezes go along with the prevailing moisture. In inland area, urbanization likely leads to a warmer-dryer climate if large-scale land cover keeps stationary.https://www.mdpi.com/2073-4441/13/10/1386urbanizationwarm season precipitationregional differentiationsouth China
collection DOAJ
language English
format Article
sources DOAJ
author Lingli Fan
Guangya Zhang
Jianjun Xu
spellingShingle Lingli Fan
Guangya Zhang
Jianjun Xu
Differentiated Effects of Urbanization on Precipitation in South China
Water
urbanization
warm season precipitation
regional differentiation
south China
author_facet Lingli Fan
Guangya Zhang
Jianjun Xu
author_sort Lingli Fan
title Differentiated Effects of Urbanization on Precipitation in South China
title_short Differentiated Effects of Urbanization on Precipitation in South China
title_full Differentiated Effects of Urbanization on Precipitation in South China
title_fullStr Differentiated Effects of Urbanization on Precipitation in South China
title_full_unstemmed Differentiated Effects of Urbanization on Precipitation in South China
title_sort differentiated effects of urbanization on precipitation in south china
publisher MDPI AG
series Water
issn 2073-4441
publishDate 2021-05-01
description In this paper, precipitation data from the Tropical Rainfall Measuring Mission (TRMM), together with atmospheric reanalysis data, are employed to identify warm-season precipitation (1998–2014) changes and their association with rapid urbanization in south China. Three urban clusters (Chenyu, Yangtze Delta, and Fujian Guangdong coast) are focused. The results reveal that, for the inland Chengyu urban cluster, a lack of precipitation trend is likely due to insignificant trends in convective available potential energy (CAPE) and total column water vapor (TCWV). They are likely resulted from a reduced local moisture recycling in urban areas, balanced by an increased evapotranspiration of rural areas, together with a stable advection of water vapor input. For the Yangtze River Delta urban cluster, a negative trend in precipitation is associated with a slightly decreased CAPE and an increased TCWV, but is very likely related to urbanization induced an increased planetary boundary layer (PBL) and reduced land surface evaporation. For the Fujian Guangdong coast urban cluster, a marked positive precipitation trend is well explained by positive trends in CAPE and TCWV. The increased precipitation likely benefits from enhanced moisture recycling due to improved vegetation cover in rural areas, and enhanced advection moisture inputs due to urbanization along the coast. These results suggest urbanization effects on precipitation vary with regional conditions. In the coastal area, urbanization enhances sea breezes, which may benefit precipitation if sea breezes go along with the prevailing moisture. In inland area, urbanization likely leads to a warmer-dryer climate if large-scale land cover keeps stationary.
topic urbanization
warm season precipitation
regional differentiation
south China
url https://www.mdpi.com/2073-4441/13/10/1386
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AT guangyazhang differentiatedeffectsofurbanizationonprecipitationinsouthchina
AT jianjunxu differentiatedeffectsofurbanizationonprecipitationinsouthchina
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