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Evaluation of UTLS carbon monoxide simulations in GMI and GEOS-Chem chemical transport models using Aura MLS observations

机译:使用Aura MLS观测值评估GMI和GEOS-Chem化学迁移模型中的UTLS一氧化碳模拟

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摘要

This study evaluates the distribution and variation of carbon monoxide (CO)in the upper troposphere and lower stratosphere (UTLS) during 2004–2012 assimulated by two chemical transport models, using the latest version of AuraMicrowave Limb Sounder (MLS) observations. The simulated spatialdistributions, temporal variations and vertical transport of CO in the UTLSregion are compared with those observed by MLS. We also investigate theimpact of surface emissions and deep convection on CO concentrations in theUTLS over different regions, using both model simulations and MLSobservations. Global Modeling Initiative (GMI) and GEOS-Chem simulations ofUTLS CO both show similar spatial distributions to observations. The globalmean CO values simulated by both models agree with MLS observations at 215and 147 hPa, but are significantly underestimated by more than 40 % at100 hPa. In addition, the models underestimate the peak CO values by up to70 % at 100 hPa, 60 % at 147 hPa and 40 % at 215 hPa, withGEOS-Chem generally simulating more CO at 100 hPa and less CO at 215 hPathan GMI. The seasonal distributions of CO simulated by both models are inbetter agreement with MLS in the Southern Hemisphere (SH) than in theNorthern Hemisphere (NH), with disagreements between model and observationsover enhanced CO regions such as southern Africa. The simulated verticaltransport of CO shows better agreement with MLS in the tropics and the SHsubtropics than the NH subtropics. We also examine regional variations in therelationships among surface CO emission, convection and UTLS COconcentrations. The two models exhibit emission–convection–CO relationshipssimilar to those observed by MLS over the tropics and some regions withenhanced UTLS CO.
机译:这项研究使用最新版本的AuraMicrowave Limb Sounder(MLS)观测值,通过两种化学迁移模型评估了2004-2012年对流层上层和平流层下层(UTLS)中一氧化碳(CO)的分布和变化。将UTLS区域中CO的模拟空间分布,时间变化和垂直传输与MLS观测到的进行了比较。我们还使用模型模拟和MLS观测方法研究了不同区域的地面排放和深对流对UTLS中CO浓度的影响。 UTLS CO的全球建模倡议(GMI)和GEOS-Chem模拟都显示出与观测值相似的空间分布。两种模型模拟的全球平均CO值与215和147 hPa的MLS观测值一致,但在100 hPa时被低估了40%以上。此外,这些模型低估了峰值CO值,在100 COhPa时高达70%,在147 hPa时高达60%,在215 hPa时高达40%,而GEOS-Chem通常在100 hPa时模拟更多的CO而在215 hPa时模拟的CO较少。两种模式模拟的CO的季节分布与南半球(SH)的MLS吻合度要好于北半球(NH),在增强型CO区域(如南部非洲)的模型与观测值之间存在分歧。在南亚热带地区,模拟的CO垂直传输与热带和SH亚热带地区的MLS显示出更好的一致性。我们还研究了表面CO排放,对流和UTLS CO浓度之间关系的区域差异。这两个模型显示的排放-对流-CO关系类似于MLS在热带地区和一些UTLS增强的地区观察到的关系。

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