{"title":"冬末南风下台湾北部的 PM2.5 事件","authors":"","doi":"10.1016/j.atmosres.2024.107686","DOIUrl":null,"url":null,"abstract":"<div><p>When northern Taiwan is influenced locally, PM<sub>2.5</sub> events occur in specific conditions. If it is also affected by long-range transport from mainland China in the northwest, the probability of these PM<sub>2.5</sub> events increases. The current study applies WRF/CMAQ to study such case but focus on the local. From April 7 to 9, 2019, the Pacific high pressure extended westward, causing the prevailing weak southerly wind near Taiwan. The intensity of the Pacific high pressure weakened, and the wind speed near Taiwan also weakened. Therefore, the PM<sub>2.5</sub> concentration in Taiwan increased. In northern Taiwan, the hourly PM<sub>2.5</sub> concentration will inevitably increase to approximately 70 μg m<sup>−3</sup>. The ISAM of the CMAQ model demonstrates that local contributions to daily PM<sub>2.5</sub> concentrations at the four representative monitoring stations in northern Taiwan are 3.5 to 16.2 μg m<sup>−3</sup>, greater than those from central, southern, and eastern Taiwan, from 1.8 to 6.7 μg m<sup>−3</sup>. We use the integrated process rate (IPR) and integrated reaction rate (IRR) of CMAQ to explore the formation mechanisms of PM<sub>2.5</sub>. The main causes of the increase in PM<sub>2.5</sub> concentration are horizontal advection (HADV), aerosol processes (AERO), emissions (EMIS), and a small amount of cloud processes and aqueous chemistry (CLDS). The main source of NO<sub>3</sub><sup>−</sup> is the reaction between OH and NO<sub>2</sub> during the day and the reaction between N<sub>2</sub>O<sub>5</sub> and water vapor at night. The gaseous HNO<sub>3</sub> concentration reaches a peak near noon or soon after. The aerosol ANO<sub>3</sub> concentration is high in the early morning. We also use the Sulfur Tracking Method (STM) of CMAQ to explore the sources of SO<sub>4</sub><sup>2−</sup>. Mainly it is from the local reaction of SO<sub>2</sub> and H<sub>2</sub>O<sub>2</sub>. Finally, we apply AERO7 in CMAQ to explore the main sources of carbon components. The organic carbon (OC) concentration is much greater than the element carbon (EC) concentration, which indicates a strong local photochemical effect in northern Taiwan. OC mainly comes from low-volatility/semivolatile oxidized combustion OC, followed by low-volatility/semivolatile POA. Similar weather conditions occur in autumn, winter, and spring. When the weak southerly wind was around Taiwan, PM<sub>2.5</sub> in northern Taiwan was noticed.</p></div>","PeriodicalId":8600,"journal":{"name":"Atmospheric Research","volume":null,"pages":null},"PeriodicalIF":4.5000,"publicationDate":"2024-09-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"PM2.5 episodes in northern Taiwan under southerly winds in late winter\",\"authors\":\"\",\"doi\":\"10.1016/j.atmosres.2024.107686\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>When northern Taiwan is influenced locally, PM<sub>2.5</sub> events occur in specific conditions. If it is also affected by long-range transport from mainland China in the northwest, the probability of these PM<sub>2.5</sub> events increases. The current study applies WRF/CMAQ to study such case but focus on the local. From April 7 to 9, 2019, the Pacific high pressure extended westward, causing the prevailing weak southerly wind near Taiwan. The intensity of the Pacific high pressure weakened, and the wind speed near Taiwan also weakened. Therefore, the PM<sub>2.5</sub> concentration in Taiwan increased. In northern Taiwan, the hourly PM<sub>2.5</sub> concentration will inevitably increase to approximately 70 μg m<sup>−3</sup>. The ISAM of the CMAQ model demonstrates that local contributions to daily PM<sub>2.5</sub> concentrations at the four representative monitoring stations in northern Taiwan are 3.5 to 16.2 μg m<sup>−3</sup>, greater than those from central, southern, and eastern Taiwan, from 1.8 to 6.7 μg m<sup>−3</sup>. We use the integrated process rate (IPR) and integrated reaction rate (IRR) of CMAQ to explore the formation mechanisms of PM<sub>2.5</sub>. The main causes of the increase in PM<sub>2.5</sub> concentration are horizontal advection (HADV), aerosol processes (AERO), emissions (EMIS), and a small amount of cloud processes and aqueous chemistry (CLDS). The main source of NO<sub>3</sub><sup>−</sup> is the reaction between OH and NO<sub>2</sub> during the day and the reaction between N<sub>2</sub>O<sub>5</sub> and water vapor at night. The gaseous HNO<sub>3</sub> concentration reaches a peak near noon or soon after. The aerosol ANO<sub>3</sub> concentration is high in the early morning. We also use the Sulfur Tracking Method (STM) of CMAQ to explore the sources of SO<sub>4</sub><sup>2−</sup>. Mainly it is from the local reaction of SO<sub>2</sub> and H<sub>2</sub>O<sub>2</sub>. Finally, we apply AERO7 in CMAQ to explore the main sources of carbon components. The organic carbon (OC) concentration is much greater than the element carbon (EC) concentration, which indicates a strong local photochemical effect in northern Taiwan. OC mainly comes from low-volatility/semivolatile oxidized combustion OC, followed by low-volatility/semivolatile POA. Similar weather conditions occur in autumn, winter, and spring. When the weak southerly wind was around Taiwan, PM<sub>2.5</sub> in northern Taiwan was noticed.</p></div>\",\"PeriodicalId\":8600,\"journal\":{\"name\":\"Atmospheric Research\",\"volume\":null,\"pages\":null},\"PeriodicalIF\":4.5000,\"publicationDate\":\"2024-09-10\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Atmospheric Research\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S016980952400468X\",\"RegionNum\":2,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"METEOROLOGY & ATMOSPHERIC SCIENCES\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Atmospheric Research","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S016980952400468X","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"METEOROLOGY & ATMOSPHERIC SCIENCES","Score":null,"Total":0}
PM2.5 episodes in northern Taiwan under southerly winds in late winter
When northern Taiwan is influenced locally, PM2.5 events occur in specific conditions. If it is also affected by long-range transport from mainland China in the northwest, the probability of these PM2.5 events increases. The current study applies WRF/CMAQ to study such case but focus on the local. From April 7 to 9, 2019, the Pacific high pressure extended westward, causing the prevailing weak southerly wind near Taiwan. The intensity of the Pacific high pressure weakened, and the wind speed near Taiwan also weakened. Therefore, the PM2.5 concentration in Taiwan increased. In northern Taiwan, the hourly PM2.5 concentration will inevitably increase to approximately 70 μg m−3. The ISAM of the CMAQ model demonstrates that local contributions to daily PM2.5 concentrations at the four representative monitoring stations in northern Taiwan are 3.5 to 16.2 μg m−3, greater than those from central, southern, and eastern Taiwan, from 1.8 to 6.7 μg m−3. We use the integrated process rate (IPR) and integrated reaction rate (IRR) of CMAQ to explore the formation mechanisms of PM2.5. The main causes of the increase in PM2.5 concentration are horizontal advection (HADV), aerosol processes (AERO), emissions (EMIS), and a small amount of cloud processes and aqueous chemistry (CLDS). The main source of NO3− is the reaction between OH and NO2 during the day and the reaction between N2O5 and water vapor at night. The gaseous HNO3 concentration reaches a peak near noon or soon after. The aerosol ANO3 concentration is high in the early morning. We also use the Sulfur Tracking Method (STM) of CMAQ to explore the sources of SO42−. Mainly it is from the local reaction of SO2 and H2O2. Finally, we apply AERO7 in CMAQ to explore the main sources of carbon components. The organic carbon (OC) concentration is much greater than the element carbon (EC) concentration, which indicates a strong local photochemical effect in northern Taiwan. OC mainly comes from low-volatility/semivolatile oxidized combustion OC, followed by low-volatility/semivolatile POA. Similar weather conditions occur in autumn, winter, and spring. When the weak southerly wind was around Taiwan, PM2.5 in northern Taiwan was noticed.
期刊介绍:
The journal publishes scientific papers (research papers, review articles, letters and notes) dealing with the part of the atmosphere where meteorological events occur. Attention is given to all processes extending from the earth surface to the tropopause, but special emphasis continues to be devoted to the physics of clouds, mesoscale meteorology and air pollution, i.e. atmospheric aerosols; microphysical processes; cloud dynamics and thermodynamics; numerical simulation, climatology, climate change and weather modification.