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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Future prediction of surface ozone over east Asia using Models-3 Community Multiscale Air Quality Modeling System and Regional Emission Inventory in Asia
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Future prediction of surface ozone over east Asia using Models-3 Community Multiscale Air Quality Modeling System and Regional Emission Inventory in Asia

机译:未来的预测表面臭氧在东亚使用Models-3社区多尺度空气质量建模系统和区域排放清单在亚洲

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Present and future tropospheric ozone (O3) concentrations over east Asia have been simulated by the Models-3 Community Multiscale Air Quality Modeling System (CMAQ) coupled with the Regional Emission Inventory in Asia (REAS) to predict surface O3 variations caused by future anthropogenic emissions changes. For future prediction, REAS provides three emission scenarios for China (the reference (REF), the policy succeed case (PSC), and the policy failure case (PFC) scenarios) and one emission scenario (the REF scenario) for the other countries. Simulated O3 concentration in summer was relatively high (70–80 ppbv in June and 65–75 ppbv in August) over the North China Plain in 2000. The projected REF emissions for 2020 (2020REF) enhance the monthly averaged O3 to 75–90 ppbv in June and 75–85 ppbv in August. The projected PSC emissions for 2020 (2020PFC), including a slight NOx reduction of –0.2 Tg (–2%) and a large NMVOC increase of 14.3 Tg (97%) for total Chinese emissions during 2000–2020, cause the monthly and annually averaged O3 concentrations to decrease by less than 2 ppbv in northeastern and central China. Over the North China Plain, the projected PFC emissions for 2020 (2020PFC) cause significant increases, more than 20 ppbv in the monthly averaged O3, and the O3 will be 85–105 ppbv in June and 80–95 ppbv in August for 2020. The 2020PFC also affect O3 increases in early summer in South Korea (14–18 ppbv increase for monthly average) and Japan (2–14 ppbv increase for monthly average) during 2000–2020 despite the slight NOx increase of 0.4 Tg (25%) in South Korea and the slight NOx reduction of –0.2 Tg (–10%) in Japan during 2000–2020. The pollutant in these regions seems to be transport from upwind source regions. These experiments show that over central eastern China at midday in June, the O3 concentration is largely affected by NOx emission increases but is insensitive to NMVOC emission increases.
机译:现在和未来对流层臭氧(O3)浓度在东亚已经模拟Models-3社会的多尺度空气质量建模系统(CMAQ)加上区域在亚洲(rea)预测排放清单表面O3变化引起的未来人为排放的变化。预测,意图提供三个发射场景(参考(REF),中国政策的成功案例(PSC),政策失败案例(PFC)场景)和一个发射的场景其他国家(REF场景)。模拟O3浓度在夏天相对较高(70 - 80和65 - 75年6月ppbv8月ppbv)在华北平原2000. 2020 (ref)提高每月的平均O3ppbv 75 - 90和75 - 85年6月8月ppbv。2020年预计PSC排放(2020 pfc),包括一个轻微的氮氧化物减少-0.2 Tg (-2%)和一个大NMVOC增加14.3 Tg (97%)中国排放总量在2000 - 2020年的原因每月和每年平均O3小于2 ppbv浓度降低中国东北部和中部。2020年中国平原,预计PFC排放2020 (pfc)导致显著增加,超过每月平均20 ppbv O3, O3将85 - 105和80 - 95年6月ppbv ppbv2020年8月。增加在今年夏天早些时候,韩国(14 - 18ppbv每月平均增加)和日本(2 - 14 ppbv增加的月平均)2000 - 2020年尽管轻微氧化氮增加0.4Tg在韩国(25%)和轻微的氮氧化物减少-0.2 Tg在日本(-10%)2000 - 2020。从逆风运输来源地区。实验表明,在中国东部的中心今年6月,中午O3浓度很大程度上影响NOx排放增加,但对NMVOC排放增加。

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