[زمین شناسی] جریان دریایی جابجایی آب سطحی اقیانوسها به علت وزش بادهای غالب و اختلاف چگالی ناشی از تغییر دما یا شوری آب است
پیشنهاد کاربران
the continuous, predictable, directional movement of seawater driven by gravity, wind ( Coriolis Effect ) , and water density
An ocean current is a continuous, directed movement of sea water generated by a number of forces acting upon the water, including wind, the Coriolis effect, breaking waves, cabbeling, and temperature and salinity differences. Wikipedia
