傾けい度ど風ふう

noun

gradient wind

Technical term in meteorology for the theoretical wind that results from a balance of pressure gradient, Coriolis, and centrifugal forces.

• 傾けい度ど風ふうは気き圧あつ傾けい度ど力りょくとコリオリ力りょく、遠えん心しん力りょくの釣つり合あいで決きまる。

  The gradient wind is determined by the balance of pressure gradient force, Coriolis force, and centrifugal force.