Astitha Marina, Kioutsioukis Ioannis, Fisseha Ghezae Araya, Bianconi Roberto, Bieser Johannes, Christensen Jesper H, Cooper Owen R, Galmarini Stefano, Hogrefe Christian, Im Ulas, Johnson Bryan, Liu Peng, Nopmongcol Uarporn, Petropavlovskikh Irina, Solazzo Efisio, Tarasick David W, Yarwood Greg
University of Connecticut, Civil and Environmental Engineering, Storrs, CT 06269-3037, USA.
University of Patras, Physics Department, 26504 Rio, Greece.
Atmos Chem Phys. 2018;18(19):13925-13945. doi: 10.5194/acp-18-13925-2018. Epub 2018 Oct 2.
This study evaluates simulated vertical ozone profiles produced in the framework of the third phase of the Air Quality Model Evaluation International Initiative (AQMEII3) against ozonesonde observations in North America for the year 2010. Four research groups from the United States (US) and Europe have provided modeled ozone vertical profiles to conduct this analysis. Because some of the modeling systems differ in their meteorological drivers, wind speed and temperature are also included in the analysis. In addition to the seasonal ozone profile evaluation for 2010, we also analyze chemically inert tracers designed to track the influence of lateral boundary conditions on simulated ozone profiles within the modeling domain. Finally, cases of stratospheric ozone intrusions during May-June 2010 are investigated by analyzing ozonesonde measurements and the corresponding model simulations at Intercontinental Chemical Transport Experiment Ozonesonde Network Study (IONS) experiment sites in the western United States. The evaluation of the seasonal ozone profiles reveals that, at a majority of the stations, ozone mixing ratios are underestimated in the 1-6 km range. The seasonal change noted in the errors follows the one seen in the variance of ozone mixing ratios, with the majority of the models exhibiting less variability than the observations. The analysis of chemically inert tracers highlights the importance of lateral boundary conditions up to 250 hPa for the lower-tropospheric ozone mixing ratios (0-2 km). Finally, for the stratospheric intrusions, the models are generally able to reproduce the location and timing of most intrusions but underestimate the magnitude of the maximum mixing ratios in the 2-6 km range and overestimate ozone up to the first kilometer possibly due to marine air influences that are not accurately described by the models. The choice of meteorological driver appears to be a greater predictor of model skill in this altitude range than the choice of air quality model.
本研究将空气质量模型评估国际倡议第三阶段(AQMEII3)框架下生成的模拟垂直臭氧廓线与2010年北美洲的臭氧探空观测数据进行了对比。来自美国和欧洲的四个研究小组提供了模拟的臭氧垂直廓线以开展此项分析。由于一些建模系统在气象驱动因素方面存在差异,风速和温度也被纳入了分析。除了对2010年的季节性臭氧廓线进行评估外,我们还分析了化学惰性示踪剂,以追踪侧向边界条件对建模域内模拟臭氧廓线的影响。最后,通过分析美国西部洲际化学传输实验臭氧探空网络研究(IONS)实验站点的臭氧探空测量数据及相应的模型模拟结果,对2010年5月至6月期间平流层臭氧入侵的情况进行了调查。季节性臭氧廓线的评估结果显示,在大多数站点,1至6千米范围内的臭氧混合比被低估。误差中观察到的季节性变化与臭氧混合比的变化趋势一致,大多数模型的变化程度小于观测值。对化学惰性示踪剂的分析突出了侧向边界条件对对流层低层臭氧混合比(0至2千米)在高达250百帕时的重要性。最后,对于平流层入侵情况,模型通常能够再现大多数入侵的位置和时间,但低估了2至6千米范围内最大混合比的幅度,并且在高达第一千米的范围内高估了臭氧,这可能是由于模型未能准确描述海洋空气的影响。在这个高度范围内,气象驱动因素的选择似乎比空气质量模型的选择更能预测模型的技能水平。