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@ARTICLE{Vogel:1006465,
      author       = {Vogel, Bärbel and Volk, C. Michael and Wintel, Johannes
                      and Lauther, Valentin and Müller, Rolf and Patra, Prabir K.
                      and Riese, Martin and Terao, Yukio and Stroh, Fred},
      title        = {{R}econstructing high-resolution in-situ vertical carbon
                      dioxide profiles in the sparsely monitored {A}sian monsoon
                      region},
      journal      = {Communications earth $\&$ environment},
      volume       = {4},
      number       = {1},
      issn         = {2662-4435},
      address      = {London},
      publisher    = {Springer Nature},
      reportid     = {FZJ-2023-01699},
      pages        = {72},
      year         = {2023},
      abstract     = {Atmospheric concentrations of the greenhouse gases carbon
                      dioxide and nitrous oxide haveincreased substantially
                      because of human activities. However, their sources in South
                      Asia,which contribute strongly to the accelerating global
                      growth of carbon dioxide and nitrousoxide, are poorly
                      quantified. Here, we present aircraft measurements with high
                      temporal andvertical resolution up to 20 km during the Asian
                      summer monsoon where rapid upwardtransport of surface
                      pollutants to greater altitudes occurs. Using Lagrangian
                      model simulations, we successfully reconstruct observed
                      carbon dioxide profiles leading to an improvedunderstanding
                      of the vertical structure of carbon dioxide in the Asian
                      monsoon region. Weshow that spatio-temporal patterns of
                      carbon dioxide on the Indian subcontinent driven byregional
                      flux variations rapidly propagate to approximately 13 km
                      with slower ascent above.Enhanced carbon dioxide compared to
                      the stratospheric background can be detected up to20 km. We
                      suggest that the propagation of these signals from the
                      surface to the stratospherecan be used to evaluate transport
                      models and assess carbon dioxide fluxes in South Asia.},
      cin          = {IEK-7},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IEK-7-20101013},
      pnm          = {2112 - Climate Feedbacks (POF4-211)},
      pid          = {G:(DE-HGF)POF4-2112},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000957418500002},
      doi          = {10.1038/s43247-023-00725-5},
      url          = {https://juser.fz-juelich.de/record/1006465},
}