articles.bib

@COMMENT{{This file has been generated by bib2bib 1.85}}
@COMMENT{{Command line: /usr/bin/bib2bib -oc acite -ob articles.bib -c 'author : "\(J\(ohan\|\.\)?[ ~]*Arvelius\|Arvelius,[ ~]*J\(ohan\|\.\)?\)" and $type : "ARTICLE"' ../strings.bib ../descartes.bib ../main.bib}}
@ARTICLE{muller2002jgr,
  author = {Rolf M{\"u}ller and Simone Tilmes and Jens-Uwe
                  Gro{\ss} and Daniel S. McKenna and Melanie
                  M{\"u}ller and Ulrich Schmidt and Geoffrey C. Toon
                  and Robert A. Stachnik and James J. Margitan and
                  James W. Elkins and Johan Arvelius and James
                  M. {Russel III}},
  title = {Chlorine Activation and Chemical Ozone Loss Deduced
                  from {HALOE} and Balloon Measurments in the Arctic
                  during the Winter of 1999--2000},
  journal = {J.\ Geophys.\ Res.},
  volume = 108,
  number = {D5},
  doi = {10.1029/2001JD001423},
  month = NOV,
  year = 2002
}
@ARTICLE{robinson2005acp,
  author = {A. D. Robinson and G. A. Millard and F. Danis and
                  M. Guirlet and N. R. P. Harris and A. M. Lee and
                  J. D. McIntyre and J. A. Pyle and J. Arvelius and
                  S. Dagnesjo and S. Kirkwood and H. Nilsson and
                  D. W. Toohey and T. Deshler and F. Goutail and
                  J-P. Pommereau and J. W. Elkins and F. Moore and
                  E. Ray and U. Schmidt and A. Engel and
                  M. M{\"u}ller},
  title = {Ozone loss derived from balloon-borne tracer
                  measurements in the 1999/2000 Arctic winter},
  journal = {Atmos.\ Chem.\ Phys.},
  volume = 5,
  year = 2005,
  pages = {1423--1436},
  month = JUN,
  number = 5,
  note = {{SRef-ID:1680-7324/acp/2005-5-1423}},
  url = {http://www.atmos-chem-phys.net/5/1423/2005/acp-5-1423-2005.pdf},
  issn = {1680-7316}
}
@ARTICLE{rao2003jgr,
  author = {T. Narayana Rao and S. Kirkwood and J. Arvelius and
                  P. von der Gathen and R. Kivi},
  title = {Climatology of {UTLS} Ozone and the ratio of Ozone
                  and Potential Vorticity over Northern {E}urope},
  journal = {J.\ Geophys.\ Res.},
  year = 2003,
  volume = 108,
  number = {D22},
  doi = {10.1029/2003JD003860},
  eid = 4703,
  pdf = {rao2003jgr.pdf}
}
@ARTICLE{hooper2004anngeo,
  author = {Hooper, D. and J. Arvelius and K. Stebel},
  title = {Retrieval of atmospheric static stability from radar
                  return signal power},
  journal = {Ann.\ Geophys.},
  volume = 22,
  number = 11,
  pages = {3781--3788},
  pdf = {hooper2004anngeo.pdf},
  url = {http://www.ann-geophys.net/22/3781/2004/angeo-22-3781-2004.pdf},
  note = {{SRef-ID:1432-0576/ag/2004-22-3781}},
  year = 2004
}
@ARTICLE{rao2004asr,
  author = {T. Narayana Rao and J. Arvelius and S. Kirkwood and
                  P. von der Gathen},
  title = {Climatology of ozone in the troposphere and lower
                  stratosphere over the European Arctic},
  journal = {Adv.\ Space Res.},
  year = 2004,
  volume = 34,
  number = 4,
  pages = {754--758},
  doi = {10.1016/j.asr.2003.05.055},
  abstract = {A brief climatology of ozone using more than 8 years
                  of ozonesonde data in the troposphere and lower
                  stratosphere at two northern high latitude stations,
                  Sodankyla and Ny-Ålesund, is presented. The
                  climatology of ozone clearly shows a significant
                  seasonal cycle with the ozone maxima changing with
                  height. The monthly variability of ozone as well as
                  its seasonal maximum is found near the
                  tropopause. Variation in tropopause height is due
                  mainly to the passage of tropospheric weather
                  systems and is responsible for the large monthly
                  variability of ozone near the tropopause. In the
                  lower stratosphere, interannual variations are at a
                  maximum in winter and spring, and are the result of
                  variations in wave driven stratospheric circulation,
                  which peaks in winter. The present climatology forms
                  a basis for 3-D chemistry transport models to test
                  its ability at high latitudes.}
}
@ARTICLE{rao2008jgr,
  author = {Rao, T. N. and J. Arvelius and S. Kirkwood},
  title = {Climatology of Tropopause Folds over a European
                  Arctic Station -- {Esrange}},
  journal = {J.\ Geophys.\ Res.},
  year = {2008},
  volume = {113},
  optnumber = {},
  month = JUL,
  doi = {10.1029/2007JD009638},
  eid = {D00B03}
}

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