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Partitioning and budget of inorganic and organic chlorine species observed by MIPAS-B and TELIS in the Arctic in March 2011

机译:MIPAS-B和TELIS在2011年3月在北极观测到的无机和有机氯物种的分配和预算

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摘要

The Arctic winter 2010/2011 was characterized by a persistent vortex with extremely low temperatures in the lower stratosphere above northern Scandinavia leading to a strong activation of chlorine compounds (ClOx) like Cl, Cl2, ClO, ClOOCl, OClO, and HOCl, which rapidly destroyed ozone when sunlight returned after winter solstice. The MIPAS-B (Michelson Interferometer for Passive Atmospheric Sounding) and TELIS (TErahertz and submillimeter LImb Sounder) balloon measurements obtained in northern Sweden on 31 March 2011 inside the polar vortex have provided vertical profiles of inorganic and organic chlorine species as well as diurnal variations of ClO around sunrise over the whole altitude range in which chlorine has been undergoing activation and deactivation. This flight was performed at the end of the winter during the last phase of ClOx deactivation. The complete inorganic and organic chlorine partitioning and budget for 31 March 2011, assumed to be representative for the late-winter Arctic stratosphere, has been derived by combining MIPAS-B and TELIS simultaneously observed molecules. A total chlorine amount of 3.41 ± 0.30 parts per billion by volume is inferred from the measurements (above 24 km). This value is in line with previous stratospheric observations carried out outside the tropics confirming the slightly decreasing chlorine amount in the stratosphere. Observations are compared and discussed with the output of a multi-year simulation performed with the chemistry climate model EMAC (ECHAM5/MESSy Atmospheric Chemistry). The simulated stratospheric total chlorine amount is in accordance with the MIPAS-B/TELIS observations, taking into account the fact that some chlorine source gases and very short-lived species are not included in the model.
机译:北极2010/2011年冬季的特征是持续涡旋,斯堪的纳维亚半岛北部平流层下部温度极低,导致诸如Cl,Cl2,ClO,ClOOCl,OClO和HOCl的氯化合物(ClOx)强烈活化。冬至后阳光返回时破坏了臭氧。 2011年3月31日在瑞典北部极涡内获得的MIPAS-B(米歇尔森被动大气探测干涉仪)和TELIS(TErahertz和亚毫米LImb Sounder)气球测量结果提供了无机和有机氯物种的垂直剖面以及昼夜变化在氯一直处于激活和失活状态的整个海拔范围内,日出前后ClO的变化。该飞行是在冬季结束时在ClOx停用的最后阶段进行的。通过组合MIPAS-B和TELIS同时观测到的分子,可以得出2011年3月31日无机和有机氯的完整分配和预算,这些预算和预算被认为是北极冬季平流层的代表。从测量值(24 km以上)推断总氯含量为十亿分之3.41±0.30份。该值与以前在热带地区进行的平流层观测一致,证实了平流层中的氯含量略有下降。对观测结果进行了比较和讨论,并使用化学气候模型EMAC(ECHAM5 / MESSy大气化学)进行了多年模拟。考虑到某些氯源气体和寿命很短的物种未包括在模型中,模拟的平流层总氯含量符合MIPAS-B / TELIS的观察结果。

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