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@ARTICLE{Li:2705,
      author       = {Li, X. and Brauers, T. and Shao, M. and Garland, R.M. and
                      Wagner, T. and Deutschmann, T. and Wahner, A.},
      title        = {{MAX}-{DOAS} measurements in southern {C}hina: retrieval of
                      aerosol extinctions and validation using ground-based
                      in-situ data},
      journal      = {Atmospheric chemistry and physics},
      volume       = {10},
      issn         = {1680-7316},
      address      = {Katlenburg-Lindau},
      publisher    = {EGU},
      reportid     = {PreJuSER-2705},
      pages        = {2079 - 2089},
      year         = {2010},
      note         = {The authors like to thank Roman Sinreich, Udo Friess, and
                      Ulrich Platt (Heidelberg) for lending the Mini-MAX DOAS
                      instrument, for the MiniMax software, and for fruitful
                      discussions. The technical help and support at the field
                      site from the PRiDe-PRD2006 campaign team, especially Rolf
                      Haseler (Julich), Min Hu, Limin Zeng, and Yuanhang Zhang
                      (Beijing) are gratefully acknowledged. We thank all
                      participants of the distributed computing of the RTM. This
                      work was supported by the China National Basic Research and
                      Development Program},
      abstract     = {We performed MAX-DOAS measurements during the PRiDe-PRD2006
                      campaign in the Pearl River Delta region 50 km north of
                      Guangzhou, China, for 4 weeks in June 2006. We used an
                      instrument sampling at 7 different elevation angles between
                      3 degrees and 90 degrees. During 9 cloud-free days,
                      differential slant column densities (DSCDs) of O-4 (O-2
                      dimer) absorptions between 351 nm and 389 nm were evaluated
                      for 6 elevation angles. Here, we show that radiative
                      transfer modeling of the DSCDS can be used to retrieve the
                      aerosol extinction and the height of the boundary layer. A
                      comparison of the aerosol extinction with simultaneously
                      recorded, ground based nephelometer data shows excellent
                      agreement.},
      keywords     = {J (WoSType)},
      cin          = {ICG-2 / JARA-HPC},
      ddc          = {550},
      cid          = {I:(DE-Juel1)VDB791 / $I:(DE-82)080012_20140620$},
      pnm          = {Atmosphäre und Klima},
      pid          = {G:(DE-Juel1)FUEK406},
      shelfmark    = {Meteorology $\&$ Atmospheric Sciences},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000275505500001},
      url          = {https://juser.fz-juelich.de/record/2705},
}