coriolis acceleration वाक्य
उदाहरण वाक्य
मोबाइल
- The vector formula for the magnitude and direction of the Coriolis acceleration is derived through vector analysis and is
- :The Coriolis acceleration ( and hence the Coriolis force ) only exists when using polar co-ordinates.
- The pressure gradient force is represented by blue arrows, the Coriolis acceleration ( always perpendicular to the velocity ) by red arrows
- The Coriolis acceleration is perpendicular to the longitudinal flight path and will be of the same magnitude for northbound and southbound flights.
- In the micromechanical type, the Coriolis acceleration is measured by a micro-mechanical capacitive acceleration sensor placed on an oscillating element.
- The pressure-gradient force is represented by blue arrows, the Coriolis acceleration ( always perpendicular to the velocity ) by red arrows
- The asymmetry between the prograde and retrograde satellites can be explained very intuitively by the Coriolis acceleration in the frame rotating with the planet.
- When considering atmospheric or oceanic dynamics, the vertical velocity is small, and the vertical component of the Coriolis acceleration is small compared to gravity.
- At the synoptic scale, the Coriolis acceleration acting on moving air masses ( outside of the tropics ), plays a dominant role in predictions.
- For the acceleration, is the centripetal acceleration and } } the Coriolis acceleration, in addition to the radial acceleration } } and angular acceleration.
- :: : : Might the discrepancy be that you're going for a full-trip average, while Anon was calculating the peak momentary Coriolis acceleration?
- Steve's rough method gives an estimate of 1 / 2, 500 gee, while the actual Coriolis acceleration at the relevant latitude is about 1 / 1, 000 gee.
- It is seen that the Coriolis acceleration not only cancels the centrifugal acceleration, but together they provide a net " centripetal ", radially inward component of acceleration ( that is, directed toward the center of rotation ):
- If the motion of the point is analysed using co-ordinates based on the direction normal to the velocity vector and tangential to the velocity vector there is no 2r'?'term and so no need to resort to a Coriolis acceleration.
- Because this reference frame rotates several times a minute rather than only once a day like the Earth, the Coriolis acceleration produced is many times larger and so easier to observe on small time and spatial scales than is the Coriolis acceleration caused by the rotation of the Earth.
- Because this reference frame rotates several times a minute rather than only once a day like the Earth, the Coriolis acceleration produced is many times larger and so easier to observe on small time and spatial scales than is the Coriolis acceleration caused by the rotation of the Earth.
- In non-vector terms : at a given rate of rotation of the observer, the magnitude of the Coriolis acceleration of the object is proportional to the velocity of the object and also to the sine of the angle between the direction of movement of the object and the axis of rotation.
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