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    Coriolis Force is directly proportional to: (A) Density of air (B) Horizontal velocity of the moving body (C) Spacing of isobars (D) Mass of the movin
    Question



    Coriolis Force is directly proportional to: (A) Density of air (B) Horizontal velocity of the moving body (C) Spacing of isobars (D) Mass of the moving body (E) Sine of the Latitude
    Choose the correct answer:

    A.

    B, D only

    B.

    B, E only

    C.

    B, A, E only

    D.

    B, D, E only

    Correct option is D


    Explanation:
    The Coriolis Force is the apparent force that acts on moving bodies within a rotating reference frame, such as Earth. The magnitude of the Coriolis force is determined by the following factors:
    1. Horizontal Velocity of the Moving Body (Option B): The faster a body moves, the greater the Coriolis force acting on it. The Coriolis force is directly proportional to the velocity.
    2. Mass of the Moving Body (Option D): The Coriolis force increases with the mass of the object because force is related to the mass of the object being acted upon.
    3. Sine of the Latitude (Option E): The Coriolis force is dependent on the sine of the latitude (sinθ), where θ is the latitude. The effect is zero at the equator (sin0∘=0) and maximum at the poles (sin90∘=1).
    Information Booster:
    1. Formula for Coriolis Force: Fc=2mvωsinθ Where:
    · Fc = Coriolis Force
    · m = Mass of the moving object
    · v = Velocity of the object
    · ω = Angular velocity of Earth's rotation
    · sinθ = Sine of the latitude
    2. Key Characteristics of Coriolis Force:
    · Acts perpendicular to the direction of motion.
    · Deflects to the right in the Northern Hemisphere and to the left in the Southern Hemisphere.
    · Does not affect stationary objects.
    3. Effect of Latitude:
    · The Coriolis force is zero at the equator and strongest at the poles.
    · The deflection depends on the latitude of the moving object.
    4. Practical Examples:
    · Cyclones: The Coriolis force influences the rotation of cyclones.
    · Ocean Currents: Patterns of ocean currents are shaped by the Coriolis effect.
    · Ballistic Missiles: Flight paths are adjusted for Coriolis deflection.

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