背风波

在气象学中，背风波（）是大气中的定态波。山岳波（）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·多伊奇曼和在克尔科诺谢山上空发现的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.。

参考文献

外部链接

Category:大氣動力學
Category:积云
Category:滑翔技术
Category:重力波
Category:中尺度氣象學
Category:山地气象学
Category:帆船航行