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城市水文过程对气象环境影响的模拟分析 被引量:1
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作者 李立 刘寿东 +2 位作者 王咏薇 任侠 王恪非 《气象科学》 北大核心 2019年第2期247-255,共9页
采用引入城市水文过程的WRF/SLUCM方案,以北京2010年7月4—6日高温热浪天气为背景,模拟了绿地灌溉、绿洲效应和人为潜热等水文过程对城市气象环境的影响。结果表明:(1)绿地灌溉、绿洲效应和人为潜热等水文过程可导致北京城区13 ∶00(7月... 采用引入城市水文过程的WRF/SLUCM方案,以北京2010年7月4—6日高温热浪天气为背景,模拟了绿地灌溉、绿洲效应和人为潜热等水文过程对城市气象环境的影响。结果表明:(1)绿地灌溉、绿洲效应和人为潜热等水文过程可导致北京城区13 ∶00(7月4—6日小时平均,下同)潜热通量升高最多约100 W·m^-2 ,02 ∶00升高最多约15 W·m^-2;感热通量13 ∶00降低最多约80 W·m ^-2;02 ∶00降低最多约5 W·m^-2 。(2)城市水文过程可导致城区13 ∶00相对湿度增加最多约4%,02 ∶00约6%;地表气温13 ∶00降低最多约1.2 ℃,02 ∶00约0.4 ℃。(3)城市水文过程对北京城市热岛强度的减弱效果白天明显好于夜间,且在10 ∶00—14 ∶00出现了强度约0.8 ℃的冷岛效应。(4)水文过程会导致北京城区500 m高度以下白天大气温度最多降低0.5 ℃,相对湿度最多增加3%,但夜间影响较小。由于热对流运动的减弱,城区边界层高度降低约200 m;城区1 km高度以上水平风速增大,低层风速减小。 展开更多
关键词 WRF/SLUCM方案 城市水文过程 气象要素 边界层结构
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Numerical evaluation of enhanced green infrastructures for mitigating urban heat in a desert urban setting 被引量:3
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作者 Afifa Mohammed Ansar Khan Mattheos Santamouris 《Building Simulation》 SCIE EI CSCD 2023年第9期1691-1712,共22页
The cities of desert climates are anticipated to recognize a synergy of urban heat island(UHI)and severe heat waves during summertime.To improve the urban thermal environment,the present study aims quantitatively expl... The cities of desert climates are anticipated to recognize a synergy of urban heat island(UHI)and severe heat waves during summertime.To improve the urban thermal environment,the present study aims quantitatively explore a strategically designed network of vegetation patches called green infrastructure(GI)in subtropical desert cities such as Dubai.To achieve a more comfortable temperature environment,we built and simulated four GI situations with higher GI fractions,GI25,GI50,GI75,and GI100.Using a mesoscale urban model,the mosaic approach is utilized to test potential thermal improvement and urban climate impact,and a portion of each urban grid cell in the model domain is altered with various species of urban vegetation patches by 25%,50%,75%,and 100%.The daily peak reduction in ambient temperature at 17:00LT is similar to 0.0168℃ per unit of GI increase when compared to the untreated scenario;however,the maximum anticipated daytime summer temperature decline for GI25,GI50,GI75,and GI100 is 0.6℃,1.1℃,1.4℃,and 1.7℃,respectively.The associated reduction in nighttime ambient temperature per unit increase in the GI is 0.0432℃,with a maximum temperature drop of around 2.4℃ for the GI100 scenario.Increased GI reduces the height of the planetary boundary layer(PBL)by up to 468 m,which might lead to greater pollution concentrations.While GI-based cooling has a significant influence on delayed sea breeze and humidity,it may raise the risk of heat discomfort in the indoor building environment.This study adds to our understanding of the potential for GI mitigation as well as the seasonal impact of developing GIs on the desert urban boundary layer. 展开更多
关键词 green infrastructure heat mitigation urban heat wrf-slucm Dubai city
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