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Quantifying errors in surface ozone predictions associated with clouds over the CONUS: a WRF-Chem modeling study using satellite cloud retrievals

机译:在康明斯云中量化与云相关的表面臭氧预测的误差:使用卫星云检索的WRF-Chem建模研究

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Clouds play a key role in radiation and hence O-3 photochemistry by modulating photolysis rates and light-dependent emissions of biogenic volatile organic compounds (BVOCs). It is not well known, however, how much error in O-3 predictions can be directly attributed to error in cloud predictions. This study applies the Weather Research and Forecasting with Chemistry (WRF-Chem) model at 12 km horizontal resolution with the Morrison microphysics and Grell 3-D cumulus parameterization to quantify uncertainties in summertime surface O-3 predictions associated with cloudiness over the contiguous United States (CONUS). All model simulations are driven by reanalysis of atmospheric data and reinitialized every 2 days. In sensitivity simulations, cloud fields used for photochemistry are corrected based on satellite cloud retrievals. The results show that WRF-Chem predicts about 55% of clouds in the right locations and generally underpredicts cloud optical depths. These errors in cloud predictions can lead to up to 60 ppb of overestimation in hourly surface O-3 concentrations on some days. The average difference in summertime surface O-3 concentrations derived from the modeled clouds and satellite clouds ranges from 1 to 5 ppb for maximum daily 8 h average O-3 (MDA8 O-3) over the CONUS. This represents up to similar to 40% of the total MDA8 O-3 bias under cloudy conditions in the tested model version. Surface O3 concentrations are sensitive to cloud errors mainly through the calculation of photolysis rates (for similar to 80 %), and to a lesser extent to light-dependent BVOC emissions. The sensitivity of surface O-3 concentrations to satellite-based cloud corrections is about 2 times larger in VOC-limited than NOx-limited regimes. Our results suggest that the benefits of accurate predictions of cloudiness would be significant in VOC-limited regions, which are typical of urban areas.
机译:云在辐射中发挥着关键作用,通过调节生物挥发性有机化合物(BVOCs)的光解率和光依赖性排放来发挥辐射和o-3光化学。然而,它尚不为人所知,O-3预测中的错误可以直接归因于云预测中的错误。本研究将天气研究和预测与化学(WRF-CHEM)模型以12公里的水平分辨率与莫里森微物质和GRELL 3-D积云参数化进行了汇总,以量化与连续的美国连续的云层相关的夏季表面O-3预测的不确定性(康士州)。所有模型模拟都是由大气数据的分析驱动的,每2天重新初始化。在灵敏度模拟中,基于卫星云检索校正了用于光化学的云字段。结果表明,WRF-Chem预测右侧位置的约55%云,通常是云光学深度的欠下。云预测中的这些错误可能在几天内导致每小时表面O-3浓度高达60ppb。夏季表面O-3浓度的平均差异来自模型云和卫星云的浓度范围为1至5ppb,在锥形上每日每日8小时平均O-3(MDA8 O-3)。这表示在经过测试模型版本中的多云条件下的总MDA8 O-3偏置的40%。表面O3浓度主要通过计算光解率(类似于80%)并对光依赖性BVOC排放的程度敏感而敏感。表面O-3浓度与卫星基云校正的敏感性在VOC限制的基于卫星的云校正中的敏感性约为NOx限制的制度。我们的研究结果表明,在城市地区的VOC限制区域中,准确预测的云层的好处将是显着的。

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