noun
Technical meteorological term for an upslope wind caused by daytime heating of a mountain slope. Contrasts with 滑降風 (katabatic wind).
See also: 滑降風
滑昇風は、斜面が日射で暖められることで発生する。
Anabatic winds occur when a slope is heated by solar radiation.
滑降風 is a katabatic wind (downslope), while 滑昇風 is an anabatic wind (upslope).
Compound of 滑昇 (upslope gliding/rising) and 風 (wind). The exact historical derivation is uncertain; the spelling is conventionally associated with the meteorological meaning.