首页> 外文期刊>Atmospheric chemistry and physics >Evaluation of CLaMS, KASIMA and ECHAM5/MESSy1 simulations in the lower stratosphere using observations of Odin/SMR and ILAS/ILAS-II
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Evaluation of CLaMS, KASIMA and ECHAM5/MESSy1 simulations in the lower stratosphere using observations of Odin/SMR and ILAS/ILAS-II

机译:使用Odin / SMR和ILAS / ILAS-II观测资料评估平流层下部的CLaMS,KASIMA和ECHAM5 / MESSy1模拟

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1-year data sets of monthly averaged nitrous oxide (N2O) and ozone (O3)derived from satellite measurements were used as a tool for the evaluation ofatmospheric photochemical models. Two 1-year data sets, one solar occultationdata set derived from the Improved Limb Atmospheric Spectrometer (ILAS and ILAS-II)and one limb sounding data set derived from the Odin Sub-Millimetre Radiometer(Odin/SMR) were employed. Here, these data sets are used for the evaluationof two Chemical Transport Models (CTMs), the Karlsruhe Simulation Model ofthe Middle Atmosphere (KASIMA) and the Chemical Lagrangian Model of theStratosphere (CLaMS) as well as for one Chemistry-Climate Model (CCM),the atmospheric chemistry general circulation model ECHAM5/MESSy1 (E5M1)in the lower stratosphere with focus on the Northern Hemisphere. Since theOdin/SMR measurements cover the entire hemisphere, the evaluation is performedfor the entire hemisphere as well as for the low latitudes, midlatitudes andhigh latitudes using the Odin/SMR 1-year data set as reference. To assess theimpact of using different data sets for such an evaluation study we repeatthe evaluation for the polar lower stratosphere using the ILAS/ILAS-II data set.Only small differences were found using ILAS/ILAS-II instead of Odin/SMR as areference, thus, showing that the results are not influenced by the particularsatellite data set used for the evaluation. The evaluation of CLaMS, KASIMAand E5M1 shows that all models are in agreement with Odin/SMR and ILAS/ILAS-II.Differences are generally in the range of ±20%. Larger differences (upto −40%) are found in all models at 500±25 K for N2O mixing ratiosgreater than 200 ppbv, thus in air masses of tropical character. Generally,the largest differences were found for the tropics and the lowest for thepolar regions. However, an underestimation of polar winter ozone loss wasfound both in KASIMA and E5M1 both in the Northern and Southern Hemisphere.
机译:来自卫星测量的月平均一氧化二氮(N 2 O)和臭氧(O 3 )的1年数据集用作评估大气光化学模型的工具。使用两个1年的数据集,一个来自改进的肢体大气光谱仪(ILAS和ILAS-II)的太阳掩星数据集,以及一个来自奥丁次毫米辐射仪(Odin / SMR)的肢体探测数据集。在这里,这些数据集用于评估两种化学物质运输模型(CTM),中层大气的卡尔斯鲁厄模拟模型(KASIMA)和平流层化学拉格朗日模型(CLaMS)以及一种化学-气候模型(CCM) ,平流层下层的大气化学普遍循环模型ECHAM5 / MESSy1(E5M1),以北半球为重点。由于Odin / SMR测量覆盖整个半球,因此,以Odin / SMR一年数据集为参考,对整个半球以及低纬度,中纬度和高纬度进行评估。为了评估使用不同数据集进行此类评估研究的影响,我们使用ILAS / ILAS-II数据集重复了对极地平流层下层的评估。使用ILAS / ILAS-II代替Odin / SMR作为参考仅发现了很小的差异,因此,表明结果不受用于评估的特定卫星数据集的影响。对CLaMS,KASIMA和E5M1的评估表明,所有模型都与Odin / SMR和ILAS / ILAS-II一致,差异通常在±20%的范围内。在所有模型中,N 2 O混合比大于200 ppbv时,所有模型在500±25 K时存在较大差异(最高-40%),因此在热带气团中。通常,热带地区差异最大,而极地地区差异最小。但是,在北半球和南半球的KASIMA和E5M1中都发现极低的冬季臭氧损失。

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