Changes in apparent temperature and PM2.5 around the Beijing–Tianjin megalopolis under greenhouse gas and stratospheric aerosol intervention scenarios

Jun Wang, John C. Moore, Liyun Zhao
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Abstract

Abstract. Apparent temperature (AP) and ground-level aerosol pollution (PM2.5) are important factors in human health, particularly in rapidly growing urban centers in the developing world. We quantify how changes in apparent temperature – that is, a combination of 2 m air temperature, relative humidity, surface wind speed, and PM2.5 concentrations – that depend on the same meteorological factors along with future industrial emission policy may impact people in the greater Beijing region. Four Earth system model (ESM) simulations of the modest greenhouse emissions RCP4.5 (Representative Concentration Pathway), the “business-as-usual” RCP8.5, and the stratospheric aerosol intervention G4 geoengineering scenarios are downscaled using both a 10 km resolution dynamic model (Weather Research and Forecasting, WRF) and a statistical approach (Inter-Sectoral Impact Model Intercomparison Project – ISIMIP). We use multiple linear regression models to simulate changes in PM2.5 and the contributions meteorological factors make in controlling seasonal AP and PM2.5. WRF produces warmer winters and cooler summers than ISIMIP both now and in the future. These differences mean that estimates of numbers of days with extreme apparent temperatures vary systematically with downscaling method, as well as between climate models and scenarios. Air temperature changes dominate differences in apparent temperatures between future scenarios even more than they do at present because the reductions in humidity expected under solar geoengineering are overwhelmed by rising vapor pressure due to rising temperatures and the lower wind speeds expected in the region in all future scenarios. Compared with the 2010s, the PM2.5 concentration is projected to decrease by 5.4 µg m−3 in the Beijing–Tianjin province under the G4 scenario during the 2060s from the WRF downscaling but decrease by 7.6 µg m−3 using ISIMIP. The relative risk of five diseases decreases by 1.1 %–6.7 % in G4, RCP4.5, and RCP8.5 using ISIMIP but has a smaller decrease (0.7 %–5.2 %) using WRF. Temperature and humidity differences between scenarios change the relative risk of disease from PM2.5 such that G4 results in 1 %–3 % higher health risks than RCP4.5. Urban centers see larger rises in extreme apparent temperatures than rural surroundings due to differences in land surface type, and since these are also the most densely populated, health impacts will be dominated by the larger rises in apparent temperatures in these urban areas.
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温室气体和平流层气溶胶干预情景下京津特大城市周边视温和PM2.5变化
摘要视温(AP)和地面气溶胶污染(PM2.5)是影响人类健康的重要因素,特别是在发展中国家快速发展的城市中心。我们量化了视温度的变化——即2米气温、相对湿度、地面风速和PM2.5浓度的组合——取决于相同的气象因素,以及未来的工业排放政策,可能会对大北京地区的人们产生怎样的影响。四个地球系统模式(ESM)模拟了中等温室气体排放RCP4.5(代表性浓度路径)、“一切照旧”RCP8.5和平流层气溶胶干预G4地球工程情景,使用10公里分辨率动态模式(天气研究与预报,WRF)和统计方法(部门间影响模式比较项目- ISIMIP)进行了缩小。利用多元线性回归模型模拟了PM2.5的变化,以及气象因子对季节AP和PM2.5的控制作用。无论是现在还是将来,WRF都比ISIMIP产生更温暖的冬季和更凉爽的夏季。这些差异意味着极端视温日数的估计值随着降尺度方法以及气候模式和情景的不同而有系统地变化。气温变化对未来情景之间表观温度差异的主导作用甚至比目前更大,因为在太阳地球工程下预期的湿度减少被该地区在所有未来情景中由于温度上升和预期风速降低而导致的蒸汽压上升所抵消。与2010年代相比,在G4情景下,2060年代北京-天津地区的PM2.5浓度因WRF降尺度而减少5.4µg m−3,而根据ISIMIP则减少7.6µg m−3。在使用ISIMIP的G4、RCP4.5和RCP8.5中,五种疾病的相对风险降低了1.1% - 6.7%,但使用WRF的降低幅度较小(0.7% - 5.2%)。不同情景之间的温度和湿度差异改变了PM2.5造成的相对疾病风险,因此G4造成的健康风险比RCP4.5高1% - 3%。由于地表类型的差异,城市中心的极端表观温度比农村环境的上升幅度更大,而且由于这些城市也是人口最密集的地区,因此对健康的影响将主要是这些城市地区表观温度的较大上升。
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