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The two factors that determine the strength of the Coriolis effect are the rotation speed of the Earth and the latitude of the location. The effect is strongest at the poles and weakest at the equator due to the Earth's rotational speed and curvature.
The core material and the number of windings are major factors. The voltage potential and current run the unit.
The color of the rock is not a major factor that influences the strength of a rock. Factors such as mineral composition, grain size, texture, and porosity play a more significant role in determining a rock's strength.
The strength of an electric field is influenced by two factors: the magnitude of the charge creating the field, and the distance from the charge at which the field is being measured. The larger the charge and the closer the distance, the stronger the electric field will be.
The prevailing winds are set up by the Earth's rotation and the distribution of heat from the sun. Factors that influence their direction and strength include the Coriolis effect, pressure gradients, and the distribution of land and water on the Earth's surface.
No, heating and cooling does not effect the strength of a glass
the factors of the cold war & the missel war in india
There are several factors when it comes to improving ones strength curve, Improve your acceleration ability,starting strength,speed strength, and improving Amortization.Improve these factors and you will transform your strength curve.
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how does tornados effect abiotic and biotics
The magnitude of the charges on the objects and the distance between them are the two main factors that affect the strength of electrostatic forces. Increasing the charges or decreasing the distance between the objects would have the greatest effect on strengthening the electrostatic forces between them.
The three factors that control the path of a surface current are wind direction, the Earth's rotation (Coriolis effect), and the shape of the coastline or the presence of land masses. These factors influence the direction and strength of surface currents in the ocean.