@article{oai:nagasaki-u.repo.nii.ac.jp:00020517,
 author = {松島, 晟},
 journal = {長崎大学教養部紀要. 自然科学},
 month = {Dec},
 note = {A wind system and pressure and temperature oscillations are studied when the lower part of the Thermosphere (around 90-110 km) is heated periodically. The obtained results are follows: (1) the wind components and all oscillations predominate in and above the heating layer, (2) only one node is formed in the heating layer in the case of the westerly, northerly and pressure oscillation, and therefore, these phases have a jump of 180 in the same layer, (3) in the case of the vertical wind and the temperature oscillation, no node is formed., 長崎大学教養部紀要. 自然科学. 1971, 12, p.7-13},
 pages = {7--13},
 title = {熱圏下部を周期的に加熱した場合の風系と温度変化について},
 volume = {12},
 year = {1971}
}