| • कॉरिऑलिस प्राचल • कोरिऑलिस प्रचाल • कोरिऑलिस प्राचल | |
| parameter: मानदण्ड मापदण्ड | |
coriolis parameter मीनिंग इन हिंदी
coriolis parameter उदाहरण वाक्य
उदाहरण वाक्य
अधिक: आगे- where " ? " is the variation of the Coriolis parameter with latitude.
- where f is the Coriolis parameter 2 \ Omega \ sin \ varphi, introduced above ( where \ varphi is the latitude ).
- Using a constant Coriolis parameter prevents the formation of beta gyres which are largely responsible for the North-westward direction of most tropical cyclones.
- In reality, the Coriolis parameter varies with latitude, and so the f-plane approximation is not appropriate when considering flows over large lengthscales.
- Thus the Coriolis parameter, f, is the angular velocity or frequency required to maintain a body at a fixed circle of latitude or zonal region.
- Because these waves are equatorial, the Coriolis parameter vanishes at 0 degrees; therefore, it is necessary to use the equatorial beta plane approximation that states:
- Diego Garcia is at minimum risk from tropical cyclones due to its proximity to the equator where the coriolis parameter required to organise circulation of the upper atmosphere is minimal.
- where f is the Coriolis parameter, v is the azimuthal ( i . e . rotating ) wind speed, and r is the radius to the axis of rotation.
- :: The large-scale oceanic gyres are clockwise in the Northern Hemisphere and counter-clockwise in the Southern Hemisphere, because of the differing sign of the Coriolis parameter.
- He also developed a simple theory of the general ocean circulation postulating a dynamical vorticity balance between the wind-stress curl and the meridional gradient of the Coriolis parameter, the Sverdrup balance.
