@article{oai:nipr.repo.nii.ac.jp:00001497,
 author = {Kobayashi, Shun'ichi and Ishikawa, Nobuyoshi and Ohata, Tetsuo and Kawaguchi, Sadao},
 journal = {Memoirs of National Institute of Polar Research. Special issue},
 month = {Nov},
 note = {P(論文), Acoustic sounding was used in observing a katabatic wind layer at the lowest few hundred meters over Mizuho Station (70°42′S, 44°20′E, 2230m above sea level), East Antarctica. Some examples of acoustic echo return showed the structure of surface inversions in connection with a katabatic wind and the behavior of breaking waves, e.g.a "herringbone" type structure described by EMMANUEL et al. (J. Atmos. Sci., 29,886,1972) as an unstable wave. Observations disclosed that wave-like motion exists in a layer between the heights of 100 and 300m and it has a shorter period than the calculated value from the Brunt-Vaisala frequency. This discrepancy was explained by a simple two-dimensional wave equation, considering the presence of mean atmospheric flow.},
 pages = {37--49},
 title = {Observation of an atmospheric boundary layer at Mizuho Station using an acoustic sounder},
 volume = {29},
 year = {1983}
}