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The formula to calculate the acceleration caused by the Coriolis term is: f=2*omega*sin(phi)*v
where:
-omega is the rotating speed of the Earth around its z-axis (= +/- 2pi radians per 86400 seconds)
-phi is the latitude
-v is the speed of the object.
The get it`s magnitude, simply multiply by the mass of the object.
What else can I help you with?
Who discovered the coriolis force?
The Coriolis force was described by French mathematician and engineer Gaspard-Gustave de Coriolis in 1835. He formulated the concept to explain the deviations in the motion of objects on a rotating surface.
What factors influence the angle at which surface winds cross the isobars?
The pressure gradient force and the Coriolis effect are the main factors influencing the angle at which surface winds cross the isobars. The pressure gradient force creates wind flow from high pressure to low pressure, while the Coriolis effect deflects this flow to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. As a result, surface winds tend to cross the isobars at an angle as they follow the combination of these two forces.
Explain why Geostrophic wind is not possible at the equator?
Geostrophic wind is not possible at the equator because the Coriolis force is negligible at the equator due to the Earth's rotation, resulting in a weak pressure gradient force dominating. This weak Coriolis force prevents the balance between pressure gradient force and Coriolis force required for geostrophic winds.
What produces the strongest Coriolis force?
The strength of the Coriolis force is influenced by the speed of the object or fluid and the latitude at which it is moving. Faster moving objects and those at higher latitudes will experience a stronger Coriolis force.
At which location does the coriolis force have the least effect on wind?
The Coriolis effect has the least effect on winds in equatorial regions and the most effect on winds in polar regions. Coriolis effect deflects winds to the right of their initial direction in the northern hemisphere and left of their initial direction in the southern hemisphere.
What are the factors that influence the speed and direction of wind?
pressure of the area, relief and coriolis forse.
Do sea shells spiral in opposite directions with the direction of the Coriolis force of the hemisphere that they are in?
No, the direction shells spiral in is determined by the genetics of the species. The influence of the Coriolis force on something as small as a sea shell is negligible.
What affect will a reduction in surface wind speed have on the Coriolis force?
A reduction in surface wind speed will have a minor effect on the Coriolis force. The Coriolis force is primarily influenced by the Earth's rotation and the object's velocity, not the speed of the wind. Therefore, a decrease in wind speed will not significantly alter the Coriolis force.
What effect will a reduction in surface wind speed have on the Coriolis force?
The effect that a reduction in surface wind speed will have on the Coriolis force is to reduce the effect of the Coriolis force. Winds blowing at higher speeds are pulled on more by the Coriolis force, which somewhat alters the direction in which they blow.
Who discovered the coriolis force?
The Coriolis force was described by French mathematician and engineer Gaspard-Gustave de Coriolis in 1835. He formulated the concept to explain the deviations in the motion of objects on a rotating surface.
What factors influence the angle at which surface winds cross the isobars?
The pressure gradient force and the Coriolis effect are the main factors influencing the angle at which surface winds cross the isobars. The pressure gradient force creates wind flow from high pressure to low pressure, while the Coriolis effect deflects this flow to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. As a result, surface winds tend to cross the isobars at an angle as they follow the combination of these two forces.
Explain why Geostrophic wind is not possible at the equator?
Geostrophic wind is not possible at the equator because the Coriolis force is negligible at the equator due to the Earth's rotation, resulting in a weak pressure gradient force dominating. This weak Coriolis force prevents the balance between pressure gradient force and Coriolis force required for geostrophic winds.
What produces the strongest Coriolis force?
The strength of the Coriolis force is influenced by the speed of the object or fluid and the latitude at which it is moving. Faster moving objects and those at higher latitudes will experience a stronger Coriolis force.
What influences the magnitude of the Coriolis force?
The magnitude of the Coriolis force is influenced by the speed of the object, the latitude of the object, and the Earth's rotation rate. Objects moving faster or situated at higher latitudes will experience a greater Coriolis force.
What forces influences upper air wind flow when a gradient wind is dominant?
The main forces that influence upper air wind flow when a gradient wind is dominant are the pressure gradient force and the Coriolis force. The pressure gradient force drives the wind from areas of high pressure to areas of low pressure, while the Coriolis force deflects the wind due to the rotation of the Earth, resulting in the wind flowing parallel to the isobars. These two forces work together to create the overall wind pattern in the upper atmosphere.
Does the Coriolis effect make a tornado start to rotate?
No. Tornadoes are too small for the Coriolis effect to influence them.
Does the Coriolis effect influence tides?
No, the Coriolis effect does not directly influence tides. Tides are primarily caused by the gravitational pull of the moon and sun on the Earth's oceans. The Coriolis effect does affect ocean currents and winds, but not tides.
