A quantity defined as
f = 2ω.sinθ, where ω is the Earth’s
→ angular velocity, 2π/T,
T is the rotation period of the Earth (→ sidereal day),
and θ is the → latitude.
Also called the → Coriolis parameter.
This frequency occurs often in oceanographic studies. If an
→ iceberg is floating
in a frictionless sea, and is given a push and allowed to move freely, it will travel in a
circle of radius U/f, where U is the initial speed imparted by the push.
This circle is called an inertial circle.
See also: → Coriolis effect; → frequency.