Timing of rainfall occurrence altered by urban sprawl

被引:30
|
作者
Niyogi, Dev [1 ,2 ,3 ]
Osuri, Krishna K. [4 ]
Busireddy, N. K. R. [1 ,4 ]
Nadimpalli, Raghu [5 ]
机构
[1] Purdue Univ, Dept Earth Atmosphere & Planetary Sci, Dept Agron, W Lafayette, IN 47907 USA
[2] Univ Texas Austin, Dept Geol Sci, Jackson Sch Geosci, Austin, TX USA
[3] Univ Texas Austin, Dept Civil Architecture & Environm Engn, Austin, TX USA
[4] Natl Inst Technol Rourkela, Dept Earth & Atmospher Sci, Rourkela 769008, Odisha, India
[5] IIT, Sch Earth Ocean & Climate Sci, Bhubaneswar 752050, Odisha, India
关键词
Urbanization; Anthropogenic heat; WRF model; Rainfall modification; Timing of rainfall; Diurnal rainfall pattern; CANOPY MODEL; HEAT-ISLAND; IMPACT; SIMULATION;
D O I
10.1016/j.uclim.2020.100643
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The impact of urban changes from 1989 to 2015 on urban rainstorms is assessed for the rapidly expanding Indian city of Hyderabad. A typical event that occurred during 12-14 June 2015 is simulated, and the possible association between altered urban-sprawl and shifts in the rainfall timing and patterns are analyzed. The simulation results revealed that the consideration of urban footprint changes was necessary to correctly simulate the heavy rainfall in the high-resolution Weather Research and Forecasting (WRF) model. With the urban expansion and associated anthropogenic heating (AH), the rainfall was more distributed, and its occurrence delayed by similar to 1-2 h. The results suggest that urbanization can affect rainfall both in terms of the timing as well as the location with respect to the urbanized area. The urban downwind region received an increased rainfall, and this spatial shift was more pronounced with increasing urbanization - from being over the urban area to over rural-urban boundary downwind of the city. The analysis of hydrometeors indicated that rain and cloud quantity decreased with an increasing AH in the urban area. Study results highlight the possibility that the change in the rainfall timing is another climatological signature of urban modification of rainfall.
引用
收藏
页数:13
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