Paul Supantha, Ghosh Subimal, Mathew Micky, Devanand Anjana, Karmakar Subhankar, Niyogi Dev
Interdisciplinary Program in Climate Studies, Indian Institute of Technology Bombay, Mumbai, 400076, India.
Department of Civil Engineering, Indian Institute of Technology Bombay, Mumbai, 400076, India.
Sci Rep. 2018 Mar 2;8(1):3918. doi: 10.1038/s41598-018-22322-9.
While satellite data provides a strong robust signature of urban feedback on extreme precipitation; urbanization signal is often not so prominent with station level data. To investigate this, we select the case study of Mumbai, India and perform a high resolution (1 km) numerical study with Weather Research and Forecasting (WRF) model for eight extreme rainfall days during 2014-2015. The WRF model is coupled with two different urban schemes, the Single Layer Urban Canopy Model (WRF-SUCM), Multi-Layer Urban Canopy Model (WRF-MUCM). The differences between the WRF-MUCM and WRF-SUCM indicate the importance of the structure and characteristics of urban canopy on modifications in precipitation. The WRF-MUCM simulations resemble the observed distributed rainfall. WRF-MUCM also produces intensified rainfall as compared to the WRF-SUCM and WRF-NoUCM (without UCM). The intensification in rainfall is however prominent at few pockets of urban regions, that is seen in increased spatial variability. We find that the correlation of precipitation across stations within the city falls below statistical significance at a distance greater than 10 km. Urban signature on extreme precipitation will be reflected on station rainfall only when the stations are located inside the urban pockets having intensified precipitation, which needs to be considered in future analysis.
虽然卫星数据提供了城市对极端降水反馈的强大有力特征;但城市化信号在站点级数据中往往不那么突出。为了对此进行研究,我们选取印度孟买的案例进行研究,并使用天气研究与预报(WRF)模型对2014 - 2015年期间的八个极端降雨日进行了高分辨率(1公里)的数值研究。WRF模型与两种不同的城市方案相结合,即单层城市冠层模型(WRF - SUCM)、多层城市冠层模型(WRF - MUCM)。WRF - MUCM和WRF - SUCM之间的差异表明了城市冠层的结构和特征对降水变化的重要性。WRF - MUCM模拟结果与观测到的分布式降雨相似。与WRF - SUCM和WRF - NoUCM(无城市冠层模型)相比,WRF - MUCM也产生了更强的降雨。然而,降雨增强在城市区域的少数区域较为突出,表现为空间变异性增加。我们发现,当距离大于10公里时,城市内各站点降水的相关性低于统计显著性。极端降水的城市特征只有在站点位于降水增强的城市区域内时才会反映在站点降雨上,这在未来的分析中需要加以考虑。