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Influence of Northeast Monsoon cold surges on air quality in Southeast Asia

机译:东北季风寒冷浪涌对东南亚空气质量的影响

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摘要

Ozone (O3) is an important ground-level pollutant. O3 levels and emissions of O3 precursors have increased significantly over recent decades in East Asia and export of this O3 eastward across the Pacific Ocean is well documented. Here we show that East Asian O3 is also transported southward to tropical Southeast (SE) Asia during the Northeast Monsoon (NEM) season (defined as November to February), and that this transport pathway is especially strong during ‘cold surges’. Our analysis employs reanalysis data and measurements from surface sites in Peninsular Malaysia, both covering 2003–2012, along with trajectory calculations. Using a cold surge index (northerly winds at 925 hPa averaged over 105–110°E, 5°N) to define sub-seasonal strengthening of the NEM winds, we find the largest changes in a region covering much of the Indochinese Peninsula and surrounding seas. Here, the levels of O3 and another key pollutant, carbon monoxide, calculated by the Monitoring Atmospheric Composition and Climate (MACC) Reanalysis are on average elevated by, respectively, >40% (∼15 ppb) and >60% (∼80 ppb) during cold surges. Further, in the broader region of SE Asia local afternoon exceedances of the World Health Organization's air quality guideline for O3 (100 μg m−3, or ∼50 ppb, averaged over 8 h) largely occur during these cold surges. Day-to-day variations in available O3 observations at surface sites on the east coast of Peninsular Malaysia and in corresponding parts of the MACC Reanalysis are similar, and are clearly linked to cold surges. However, observed O3 levels are typically ∼10–20 ppb lower than the MACC Reanalysis. We show that these observations are also subject to influence from local urban pollution. In agreement with past work, we find year-to-year variations in cold surge activity related to the El Nino-Southern Oscillation (ENSO), but this does not appear to be the dominant influence of ENSO on atmospheric composition in this region. Overall, our study indicates that the influence of East Asian pollution on air quality in SE Asia during the NEM could be at least as large as the corresponding, well-studied spring-time influence on North America. Both an enhanced regional observational capability and chemical modelling studies will be required to fully untangle the importance of this long-range influence relative to local processes.
机译:臭氧(O3)是一个重要的地面污染物。 O3前体的O3水平和排放量在东亚最近几十年内显着增加,并在太平洋向东出口o3 o3被录取得很好。在这里,我们认为东亚O3也在东北季风(NEM)季节(NEM)季节向南到热带东南(SE)亚洲(定义为11月至2月),并且在“冷涌”中,这条交通途径特别强劲。我们的分析采用半岛马来西亚的表面位点的再分析数据和测量,以及覆盖2003-2012,以及轨迹计算。使用冷喘振指数(925 HPA的北风平均超过105-110°E,5°N)以定义亚季节性加强NEM风,我们在覆盖着大部分吲哚靛蓝半岛和周围地区的地区发现最大的变化海域。这里,通过监测大气组合物和气候(MACC)再分析计算的O3和另一个关键污染物,一氧化碳的水平分别升高,分别为> 40%(〜15ppb)和> 60%(〜80ppb )在寒冷的潮水期间。此外,在SE亚洲的更广泛的地区,世界卫生组织O3(100μgM-3或〜50ppb的空气质量指南的超大,在这些冷浪涌期间,在很大程度上发生。半岛马来西亚东海岸和Macc重新分析的相应部分的地表网站上可用O3观测的日常变异相似,并且与寒冷的浪涌显然。然而,观察到的O3水平通常比Macc再分析低10-20ppb。我们表明,这些观察也受到当地城市污染的影响。在过去的工作方面,我们在与El Nino-Southern振荡(ENSO)相关的寒冷浪涌活动中的年度变化,但这似乎并未成为该地区大气组合物的主导影响。总体而言,我们的研究表明,在NEM期间,East亚洲污染对SE亚洲空气质量的影响可能至少与北美的相应悠久的春天时间影响一样大。将需要增强的区域观察能力和化学建模研究,以完全解开这种远程影响力相对于当地过程的重要性。

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