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@ARTICLE{Santee:57883,
      author       = {Santee, M. L. and Lambert, A. and Read, W. G. and Livesey,
                      N. J. and Manney, G. L. and Cofield, R. E. and Cuddy, D. T.
                      and Daffer, W. H. and Drouin, B. J. and Froidevaux, L. and
                      Fuller, R. A. and Jarnot, R. F. and Knosp, B. W. and Perun,
                      V. S. and Snyder, W. V. and Stek, P. C. and Thurstans, R. P.
                      and Wagner, P. A. and Waters, J. W. and Urban, J. and
                      Murtagh, D. and Ricaud, P. and Barret, B. and Kleinböhl, A.
                      and Kuttippurath, J. and Küllmann, H. and von Hobe, M. and
                      Toon, G. C. and Stachnik, R. A.},
      title        = {{V}alidation of the {A}ura {M}icrowave {L}imb {S}ounder
                      {C}l{O} {M}easurements},
      journal      = {Journal of Geophysical Research},
      volume       = {113},
      issn         = {0148-0227},
      address      = {Washington, DC},
      publisher    = {Union},
      reportid     = {PreJuSER-57883},
      pages        = {D15S22},
      year         = {2008},
      note         = {Record converted from VDB: 12.11.2012},
      abstract     = {We assess the quality of the version 2.2 (v2.2) ClO
                      measurements from the Microwave Limb Sounder (MLS) on the
                      Earth Observing System Aura satellite. The MLS v2.2 ClO data
                      are scientifically useful over the range 100 to 1 hPa, with
                      a single- profile precision of similar to 0.1 ppbv
                      throughout most of the vertical domain. Vertical resolution
                      is similar to 3-4 km. Comparisons with climatology and
                      correlative measurements from a variety of different
                      platforms indicate that both the amplitude and the altitude
                      of the peak in the ClO profile in the upper stratosphere are
                      well determined by MLS. The latitudinal and seasonal
                      variations in the ClO distribution in the lower stratosphere
                      are also well determined, but a substantial negative bias is
                      present in both daytime and nighttime mixing ratios at
                      retrieval levels below (i. e., pressures larger than) 22
                      hPa. Outside of the winter polar vortices, this negative
                      bias can be eliminated by subtracting gridded or zonal mean
                      nighttime values from the individual daytime measurements.
                      In studies for which knowledge of lower stratospheric ClO
                      mixing ratios inside the winter polar vortices to better
                      than a few tenths of a ppbv is needed, however, day - night
                      differences are not recommended and the negative bias must
                      be corrected for by subtracting the estimated value of the
                      bias from the individual measurements at each affected
                      retrieval level.},
      keywords     = {J (WoSType)},
      cin          = {ICG-1},
      ddc          = {550},
      cid          = {I:(DE-Juel1)VDB790},
      pnm          = {Atmosphäre und Klima},
      pid          = {G:(DE-Juel1)FUEK406},
      shelfmark    = {Meteorology $\&$ Atmospheric Sciences},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000256061500002},
      doi          = {10.1029/2007JD008762},
      url          = {https://juser.fz-juelich.de/record/57883},
}