Refers to vertical movements of air as source of energy for carrying out static gliding flight, namely, so-called forced and thermal ascending wind, and then discusses vertical movements caused by frictional changes of the air, known as frictional ascending wind.
Static gliding flight over flat coasts
Statischer Segelflug uber Flachkusten
Zeitschrift fur Flugtechnik und Motorluftschiffahrt ; 14 , n 13-14
1923
2 pages
2 Figs.
Aufsatz (Zeitschrift)
Deutsch
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Static soaring flight over flat sea coasts
NTRS | 1923
|An example of static gliding flight
Engineering Index Backfile | 1923
|Engineering Index Backfile | 1924
|Engineering Index Backfile | 1923
AIAA | 2006
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