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@ARTICLE{Jia:281895,
      author       = {Jia, Mingjiao and Xue, Xianghui and Dou, Xiankang and Tang,
                      Yihuan and Yu, Chao and Wu, Jianfei and Xu, Jiyao and Yang,
                      Guotao and Ning, Baiqi and Hoffmann, Lars},
      title        = {{A} case study of {A} mesoscale gravity wave in the {MLT}
                      region using simultaneous multi-instruments in {B}eijing},
      journal      = {Journal of atmospheric and solar-terrestrial physics},
      volume       = {140},
      issn         = {1364-6826},
      address      = {Amsterdam [u.a.]},
      publisher    = {Elsevier Science},
      reportid     = {FZJ-2016-01551},
      pages        = {1 - 9},
      year         = {2016},
      abstract     = {In this work, we used observational data from an all-sky
                      airglow imager at Xinglong (40.2 °N, 117.4 °E), a sodium
                      lidar at Yanqing (40.4 °N, 116.0 °E) and a meteor radar at
                      Shisanling (40.3 °N, 116.2 °E) to study the propagation of
                      a mesoscale gravity wave. During the night of March 1, 2011,
                      the imager identified a mesoscale gravity wave structure in
                      the OH airglow that had a wave period of 2 hours, propagated
                      along an azimuthal direction (clockwise) with an angle of
                      163°, a phase speed of 73 m/s, and a horizontal wavelength
                      of 566 km. Simultaneous measurements provided by the sodium
                      lidar also showed a perturbation in the sodium layer with a
                      2-hour period. Based on the SABER/TIMED and radar data, we
                      estimated that the momentum flux and the energy flux of the
                      gravity wave were approximately 0.59 m2/s2 and 0.22 mW/m2,
                      respectively. Ray-tracing analysis showed that the gravity
                      wave was likely generated in the center of Lake Baikal owing
                      to the existence of a jet- front system in the upper
                      troposphere at that time.},
      cin          = {JSC},
      ddc          = {530},
      cid          = {I:(DE-Juel1)JSC-20090406},
      pnm          = {511 - Computational Science and Mathematical Methods
                      (POF3-511)},
      pid          = {G:(DE-HGF)POF3-511},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000372762200001},
      doi          = {10.1016/j.jastp.2016.01.007},
      url          = {https://juser.fz-juelich.de/record/281895},
}