@article{oai:nipr.repo.nii.ac.jp:00002071,
 author = {Iwasaka, Yasunobu},
 journal = {Memoirs of National Institute of Polar Research. Special issue},
 month = {Dec},
 note = {P(論文), Lidar measurements at Syowa Station (69°00′S, 39°35′E) revealed that the centroid of aerosol layer descended at the rate of 0.8mm/s during winter. If this motion is a substantial movement of aerosol particles, the mass of water transported into the troposphere is about 5×(10)^7t/winter, and the Antarctic winter stratosphere is an important sink of stratospheric water vapor. If it is a downword air motion carrying small ice crystals, the value is reduced to 5×(10)^4t/winter.},
 pages = {13--18},
 title = {Descending motion of Antarctic stratospheric aerosol layer in winter: Possible effect on stratospheric water vapor budget},
 volume = {45},
 year = {1986}
}