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    In the Northern Hemisphere, the gradient wind around a high pressure is characterized by:
    Question



    In the Northern Hemisphere, the gradient wind around a high pressure is characterized by:

    A.

    Supergeostrophic and clockwise flow

    B.

    Subgeostrophic and clockwise flow

    C.

    Supergeostrophic and anti-clockwise flow

    D.

    Subgeostrophic and anti-clockwise flow

    Correct option is A

    Explanation:
    Gradient wind is a theoretical wind that results from a balance between:
    · Pressure Gradient Force (PGF)
    · Coriolis Force
    · Centrifugal Force (due to curved path)
    In the Northern Hemisphere, around a high-pressure system (anticyclone):
    · The flow is clockwise due to the Coriolis effect.
    · The wind speed is greater than geostrophic wind (called supergeostrophic) because the centrifugal force adds to the Coriolis force, requiring a higher wind speed to balance the weaker pressure gradient.
    Information Booster:
    · Geostrophic wind is a balance between PGF and Coriolis force (idealized straight-line wind).
    · Supergeostrophic: Wind speed is greater than geostrophic (common in highs).
    · Subgeostrophic: Wind speed is less than geostrophic (common in lows).
    Additional Information:
    · Low pressure systems in the Northern Hemisphere have subgeostrophic and counter-clockwise (cyclonic) flow.
    · This concept is important in meteorology, weather forecasting, and atmospheric dynamics.

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