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The response of surface ozone to climate change over the Eastern United States

机译:美国东部地表臭氧对气候变化的响应

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We investigate the response of surface ozone (O3) to future climate change in the eastern United States by performing simulations corresponding to present (1990s) and future (2050s) climates using an integrated model of global climate, tropospheric gas-phase chemistry, and aerosols. A future climate has been imposed using ocean boundary conditions corresponding to the IPCC SRES A2 scenario for the 2050s decade. Present-day anthropogenic emissions and CO2/CH4 mixing ratios have been used in both simulations while climate-sensitive emissions were allowed to vary with the simulated climate. The severity and frequency of O3 episodes in the eastern U.S. increased due to future climate change, primarily as a result of increased O3 chemical production. The 95th percentile O3 mixing ratio increased by 5 ppbv and the largest frequency increase occured in the 80–90 ppbv range; the US EPA's current 8-h ozone primary standard is 80 ppbv. The increased O3 chemical production is due to increases in: 1) natural isoprene emissions; 2) hydroperoxy radical concentrations resulting from increased water vapor concentrations; and, 3) NOx concentrations resulting from reduced PAN. The most substantial and statistically significant (p<0.05) increases in episode frequency occurred over the southeast and midatlantic U.S., largely as a result of 20% higher annual-average natural isoprene emissions. These results suggest a lengthening of the O3 season over the eastern U.S. in a future climate to include late spring and early fall months. Increased chemical production and shorter average lifetime are two consistent features of the seasonal response of surface O3, with increased dry deposition loss rates contributing most to the reduced lifetime in all seasons except summer. Significant interannual variability is observed in the frequency of O3 episodes and we find that it is necessary to utilize 5 years or more of simulation data in order to separate the effects of interannual variability and climate change on O3 episodes in the eastern United States.
机译:我们通过使用全球气候综合模型进行对应于当前(1990年代)和未来(2050年代)气候的模拟,调查了美国东部地表臭氧(O 3 )对未来气候变化的响应,对流层气相化学和气溶胶。利用与2050年代十年IPCC SRES A2情景相对应的海洋边界条件强加了未来的气候。在两个模拟中都使用了当今的人为排放量和CO 2 / CH 4 混合比,同时允许对气候敏感的排放量随模拟气候而变化。美国东部O 3 发作的严重性和发生频率由于未来的气候变化而增加,这主要是由于O 3 化学品产量增加所致。第95个百分位数的O 3 混合比增加了5 ppbv,最大的频率增加发生在80–90 ppbv的范围内。美国EPA当前的8小时臭氧主要标准是80 ppbv。 O 3 化学品产量的增加归因于:1)天然异戊二烯排放; 2)水蒸气浓度增加引起的氢过氧自由基浓度; 3)PAN减少导致NO x 浓度升高。在美国东南部和中大西洋地区,发生频率的增幅最大,且具有统计意义( p <0.05),主要原因是年平均天然异戊二烯排放量增加了20%。这些结果表明,在未来的气候中(包括春末和初秋月份),美国东部的O 3 季节延长。化学产量的增加和平均寿命的缩短是表面O 3 的季节性响应的两个一致特征,干沉降损失率的增加在除夏季外的所有季节中对寿命的缩短起了最大的作用。在O 3 发生的频率中观察到明显的年际变化,我们发现有必要利用5年或更长时间的模拟数据来区分年际变化和气候变化对O <美国东部的sub> 3 集。

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