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Quantifying urban/industrial emissions of greenhouse and ozone-depleting gases based on atmospheric observations.

机译:根据大气观测值量化温室气体和臭氧消耗气体的城市/工业排放。

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Background and pollution trends and cycles of fourteen trace gases over the Northeastern U.S. are inferred from continuous atmospheric observations at the Harvard Forest research station located in Petersham, Massachusetts. This site receives background 'clean' air from the northwest (Canada) and 'dirty' polluted air from the southwest (New York City--Washington, D.C. corridor). Mixing ratios of gases regulated by the Montreal Protocol or other policies (CO, PCE, CFC11, CFC12, CFC113, CH 3CCl3, CCl4, and Halon-1211) and of those not subject to restrictions (H2, CH4, CHCl3, TCE, N2O, and SF6) were measured over the three-year period, 1996 to 1998, every 24 minutes by a fully automated gas chromatographic instrument with electron capture detectors. Evidence for polar vortex venting is found consistently in the month of June of the background seasonal cycles. The ratio of CO and PCE enhancements borne on southwesterly winds are in excellent agreement with county-level EPA and sales-based inventories for the New York City--Washington, D.C. region. From this firm footing, we use CO and PCE as reference compounds to determine the urban/industrial source strengths for the other species. A broad historical and geographic study of emissions reveals that the international treaty has by and large been a success. Locally, despite the passing of the 1996 Montreal Protocol ban, only emissions of CFC12 and CH3CCl3 are abating. Though source strengths are waning, the sources are not spent and continued releases to the atmosphere may be expected for some years to come. For CH3CCl3, whose rate of decline is central to our understanding of atmospheric processes, we estimate that absolute concentrations may persist until around the year 2010. The long-term high frequency time series of hydrogen provided here represents the first such data set of its kind. The H2 diurnal cycle is established and explained in terms of its sources and sinks. The ratio of H2 to CO in pollution plumes is found to be a seasonal and unchanged since early automobile exhaust studies of the 1960s, despite the many restrictions placed on car emissions and fuels since that time. Based on this result, a spatial inventory of H2 emissions from fossil fuel combustion is developed at the county level for the entire Northeastern U.S.
机译:根据位于马萨诸塞州彼得舍姆的哈佛森林研究站的连续大气观测,可以推断出美国东北部十四种微量气体的背景,污染趋势和循环。该站点从西北(加拿大)接收背景``清洁''空气,从西南(纽约市-华盛顿特区走廊)接收``脏''污染空气。受《蒙特利尔议定书》或其他政策(CO,PCE,CFC11,CFC12,CFC113,CH 3CCl3,CCl4和Halon-1211)管制的气体和不受限制的气体(H2,CH4,CHCl3,TCE,N2O)的混合比,和SF6)在1996年至1998年的三年期间内,通过带有电子捕获检测器的全自动气相色谱仪每24分钟进行一次测量。在背景季节周期的六月月份中一致地发现了极涡旋通风的证据。西南风带动的CO和PCE增强比例与县级EPA和纽约市-华盛顿特区基于销售的清单非常吻合。从这个坚实的基础上,我们使用CO和PCE作为参考化合物来确定其他物种的城市/工业来源强度。广泛的排放历史和地理研究表明,国际条约总体上是成功的。在当地,尽管通过了1996年《蒙特利尔议定书》禁令,但只有CFC12和CH3CCl3的排放有所减少。尽管放射源的强度在减弱,但放射源并未消耗,并且有望在未来几年内继续释放到大气中。对于CH3CCl3(其下降速率是我们对大气过程的理解的中心),我们估计绝对浓度可能会持续到2010年左右。此处提供的氢的长期高频时间序列代表了此类数据中的第一个。 H2的昼夜周期是根据其来源和汇来确定和解释的。自从1960年代早期进行汽车尾气研究以来,发现污染烟气中H2与CO的比率是季节性的并且没有变化,尽管自那时以来对汽车排放物和燃料施加了许多限制。根据此结果,在整个美国东北部的县一级,开发了化石燃料燃烧产生的H2排放的空间清单。

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