Войдите в систему

An accelerating particle experiences a force equal to the mass multiplied by the acceleration in an inertial frame of reference. Consider a particle in a non-inertial frame of reference, such as a sliding ball on a rotating table. The acceleration of the ball in this rotating reference frame is different than in the intertial frame, which modifies its equation of motion. The fictitious forces acting additionally on a rotating frame of reference alter Newton's Second Law expression. Centripetal and Coriolis forces are the fictitious or pseudo forces that act on a particle in a non-inertial frame of reference.

The discovery of the Coriolis force dates back to 1651 when Italian military officers reported that, during artillery practice, the cannon balls always landed to the right of where the calculations predicted. The Coriolis force is named after a French mathematician Gaspard Gustave Coriolis (1792–1843) for his work in the field of rotating reference frames.

The Coriolis force is proportional to the cross-product of the rotating frame's angular velocity vector and the object's velocity vector. Its direction can be estimated using the right-hand rule for the cross-product. Suppose the index finger and thumb are directed toward the object's velocity and the rotating frame's angular velocity, respectively. The middle finger points opposite to the Coriolis force, as indicated by the negative sign in the Coriolis force expression. The work done by Coriolis force is zero since it always acts perpendicular to the object's motion.

Due to the Earth's rotation, the Coriolis force tends to deflect moving bodies toward the right in the northern hemisphere and toward the left in the southern hemisphere. As a result, long-range snipers aim to the left of their target in the northern hemisphere.

The Coriolis force also results in cyclone formation. In the northern hemisphere, air rushing out of a high-pressure system swirls clockwise around the pressure center. Similarly, air flowing into a low-pressure region swirls counterclockwise. The turn direction of the swirling is opposite in the southern hemisphere due to the Coriolis force. The Coriolis force is zero at the equator, and as a result, no cyclones occur at the equatorial axis.

Теги
Coriolis ForceFictitious ForcesNon inertial FrameAngular VelocityCross productNewton s Second LawRotating TableCyclone FormationRight hand RuleEarth RotationDeflectionHigh pressure SystemLow pressure RegionEquatorial Axis

Из главы 10:

article

Now Playing

10.14 : Coriolis Force

Rotation and Rigid Bodies

2.7K Просмотры

article

10.1 : Угловая скорость и смещение

Rotation and Rigid Bodies

11.6K Просмотры

article

10.2 : Угловая скорость и ускорение

Rotation and Rigid Bodies

8.4K Просмотры

article

10.3 : Вращение с постоянным угловым ускорением - I

Rotation and Rigid Bodies

6.4K Просмотры

article

10.4 : Вращение с постоянным угловым ускорением - II

Rotation and Rigid Bodies

5.7K Просмотры

article

10.5 : Связь угловых и линейных величин - I

Rotation and Rigid Bodies

6.2K Просмотры

article

10.6 : Связь угловых и линейных величин - II

Rotation and Rigid Bodies

5.1K Просмотры

article

10.7 : Момент инерции

Rotation and Rigid Bodies

8.8K Просмотры

article

10.8 : Момент инерции и кинетическая энергия вращения

Rotation and Rigid Bodies

6.9K Просмотры

article

10.9 : Момент инерции: расчеты

Rotation and Rigid Bodies

6.4K Просмотры

article

10.10 : Момент инерции составных объектов

Rotation and Rigid Bodies

5.8K Просмотры

article

10.11 : Теорема о параллельной оси

Rotation and Rigid Bodies

6.2K Просмотры

article

10.12 : Теорема о перпендикулярной оси

Rotation and Rigid Bodies

2.4K Просмотры

article

10.13 : Векторное преобразование во вращающихся системах координат

Rotation and Rigid Bodies

1.2K Просмотры

JoVE Logo

Исследования

Образование

О JoVE

Авторские права © 2025 MyJoVE Corporation. Все права защищены