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Air Mass Origin in the Lower Stratosphere using HALO Measurements and CLaMS Simulations (AMOS)

Applicant Dr. Bärbel Vogel
Subject Area Atmospheric Science
Term from 2016 to 2020
Project identifier Deutsche Forschungsgemeinschaft (DFG) - Project number 316738484
 
Final Report Year 2021

Final Report Abstract

Our project AMOS demonstrates that the transport of air masses out of the Asian monsoon anticyclone into the lower northern extratropical stratosphere is an important driver during summer and fall and is determined by different processes and time scales. The basic transport mechanisms were analysed using simulations with the chemical Lagrangian transport model (CLaMS) combined with airborne measurements with the German aircraft HALO (High Altitude and Long Range Research Aircraft) in the northern Hemisphere as well as with balloon measurements in Asia. The transport of tropospheric trace gases (e.g., H2O, aerosols and their chemical precursors or ozone-depleting substances such as short-lived halogen-containing trace gases) by the Asian monsoon anticyclone into the lower stratosphere changes the chemical composition in this part of the Earth’s atmosphere. Further, radiatively active species transported into the lower extratropical stratosphere have a significant impact on surface climate and can cause regional radiative forcing. In our project AMOS we show that short-lived anthropogenic substances such as PAN, bromine-containing as well as chlorine-containing trace gases in addition to long-lived tracers (e.g. CH4, H2O, CO, N2O, SF6) are transported from sources in Asia via the Asian monsoon anticyclone into the northern extratropical lower stratosphere. In particular the impact of chlorine-containing very short lived-substances that are not regulated by the Montreal Protocol (regulating the production and use of substances that deplete the Earth’s Ozone Layer) and its amendments and adjustments on stratospheric ozone depletion is an important and ongoing investigation. On the one hand increasing anthropogenic emissions in the future are expected due to the strong growth of Asian economies; on the other hand the implementation of new emission control measures (in particular in China) has reduced the anthropogenic emissions of some pollutants transported into the lower stratosphere. It needs to be monitored in the future whether the transport of anthropogenic emissions of ozone-depleting and radiatively active substances into the lower stratosphere will further increase, which will likely impact the surface climate. Second, in the project AMOS it is demonstrated that in addition to the Asian and American summer monsoon systems also transport of tropospheric air by tropical cyclones (typhoons, hurricanes) have an impact on the chemical composition of the northern extratropial lower stratosphere. This transport pathway is in particular important for natural emissions from sea surfaces such as bromine-containing substances that have an impact ozone chemistry. In summary, the project AMOS contributes to the deduction of the source regions of pollutants at the Earth’s surface and their transport pathways to the UTLS, which is important to develop recommendations for regulations of anthropogenic surface emissions. The project is an important contribution to future reports to assess the risks of emissions of ozone-depleting substances and radiatively active substances into the atmosphere e.g. by the World Meteorological Organisation (WMO).

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