背风波
 | 此條目可参照英語維基百科相應條目来扩充。 (2023年9月29日) |
在气象学中，背风波是大气中的定态波。山地波是背风波最常见的形式，是大气内部重力波。背风波是1933年由两名德国滑翔机飞行员汉斯·多伊奇曼和沃尔夫·希尔特在克尔科诺谢山上空发现的[1][2][3]。
参考文献
[编辑]- ^ On March 10, 1933, German glider pilot Hans Deutschmann (1911–1942) was flying over the Riesen mountains in Silesia when an updraft lifted his plane by a kilometer. The event was observed, and correctly interpreted, by German engineer and glider pilot Wolf Hirth (1900–1959), who wrote about it in: Wolf Hirth, Die hohe Schule des Segelfluges [The advanced school of glider flight] (Berlin, Germany: Klasing & Co., 1933). The phenomenon was subsequently studied by German glider pilot and atmospheric physicist Joachim P. Küttner (1909 -2011) in: Küttner, J. (1938) "Moazagotl und Föhnwelle" (Lenticular clouds and foehn waves), Beiträge zur Physik der Atmosphäre, 25, 79–114, and Kuettner, J. (1959) "The rotor flow in the lee of mountains." GRD [Geophysics Research Directorate] Research Notes No. 6, AFCRC[Air Force Cambridge Research Center]-TN-58-626, ASTIA [Armed Services Technical Information Agency] Document No. AD-208862.
- ^ Tokgozlu, A; Rasulov, M.; Aslan, Z. Modeling and Classification of Mountain Waves. Technical Soaring. Vol. 29 no. 1. January 2005: 22. ISSN 0744-8996.
- ^ Article about wave lift. [2006-09-28]. （原始内容存档于2012-02-06）.
