% IMPORTANT: The following is UTF-8 encoded.  This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.

@ARTICLE{Yue:153463,
      author       = {Yue, Jia and Thurairajah, Brentha and Hoffmann, Lars and
                      Alexander, Joan and Chandran, Amal and Taylor, Michael J.
                      and Russell, James M. and Randall, Cora E. and Bailey, Scott
                      M.},
      title        = {{C}oncentric gravity waves in polar mesospheric clouds from
                      the {C}loud {I}maging and {P}article {S}ize experiment},
      journal      = {Journal of geophysical research / Atmospheres},
      volume       = {119},
      number       = {9},
      issn         = {0148-0227},
      reportid     = {FZJ-2014-03061},
      pages        = {5115–5127},
      year         = {2014},
      abstract     = {Five concentric atmospheric gravity wave (AGW) events have
                      been identified in Polar Mesospheric Cloud (PMC) images of
                      the summer mesopause region (~82–84 km) made by the
                      Cloud Imaging and Particle Size (CIPS) instrument on board
                      the Aeronomy of Ice in the Mesosphere satellite during the
                      Northern Hemisphere 2007 and 2009 PMC seasons. The AGWs
                      modulate the PMC albedo, ice water content, and particle
                      size, creating concentric ring patterns. On only one
                      occasion (13 July 2007), the concentric AGWs in PMCs were
                      aligned with AGWs with similar shapes observed in 4.3 µm
                      radiance in the lower stratosphere, as measured by
                      Atmospheric Infrared Sounder (AIRS). Coincident AIRS and
                      Infrared Atmospheric Sounding Interferometer nadir
                      measurements of 8.1 µm radiance reveal a region of deep
                      convection in the troposphere close to the estimated centers
                      of the AGWs in the stratosphere, strongly suggesting that
                      convection is the wave source. The AGWs in CIPS on 13 July
                      2007 were ~1000 km away from the observed deep convection.
                      Three other concentric AGWs in PMCs were 500–1000 km
                      away from deep convection in the troposphere, while no
                      convection was observed related to the wave on 29 July 2009.
                      We perform a 2-D ray tracing study for the AGW event on 13
                      July 2007. The calculated propagation distance is much
                      shorter than the distance between the AGWs in PMCs and the
                      observed convection. The 2-D ray tracing study indicates
                      that the AGWs in PMCs and in the stratosphere are probably
                      excited by different tropospheric convective systems.},
      cin          = {JSC},
      ddc          = {550},
      cid          = {I:(DE-Juel1)JSC-20090406},
      pnm          = {411 - Computational Science and Mathematical Methods
                      (POF2-411)},
      pid          = {G:(DE-HGF)POF2-411},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000338340400006},
      doi          = {10.1002/2013JD021385},
      url          = {https://juser.fz-juelich.de/record/153463},
}