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    Match List-I with List-II: Choose the correct answer from the options given below:
    Question

    Match List-I with List-II:

    Choose the correct answer from the options given below:

    A.

    (A)-(III), (B)-(I), (C)-(II), (D)-(IV)

    B.

    (A)-(I), (B)-(III), (C)-(IV), (D)-(II)

    C.

    (A)-(III), (B)-(I), (C)-(IV), (D)-(II)

    D.

    (A)-(I), (B)-(III), (C)-(II), (D)-(IV)

    Correct option is A

    1. (A) Environmental Lapse Rate → (III):
    · The environmental lapse rate is the rate at which atmospheric temperature decreases with an increase in altitude in the troposphere.
    · Its average value is approximately 6.49∘C/km.
    2. (B) Dry Adiabatic Lapse Rate → (I):
    · The dry adiabatic lapse rate refers to the rate of temperature decrease when a dry air parcel rises and expands.
    · Its value is approximately 10∘C/km.
    3. (C) Land Breeze → (II):
    · Land breeze occurs during the night when the land cools faster than the sea, causing air to move from the land to the sea.
    4. (D) Sea Breeze → (IV):
    · Sea breeze occurs during the day when the land heats faster than the sea, causing air to move from the sea to the land.
    Thus, the correct matching is (A)-(III), (B)-(I), (C)-(II), (D)-(IV), making the correct answer Option 1.
    Information Booster: 1. Lapse Rates:
    · Environmental Lapse Rate: Refers to the actual temperature gradient in the atmosphere.
    · Dry Adiabatic Lapse Rate: The theoretical cooling rate of rising dry air.
    · Moist Adiabatic Lapse Rate: Slower cooling rate due to latent heat release during condensation.
    2. Land Breeze and Sea Breeze:
    · Land Breeze: Occurs at night due to rapid cooling of land.
    · Sea Breeze: Occurs during the day due to rapid heating of land.
    3. Key Values to Remember:
    · Dry Adiabatic Lapse Rate: 10∘C/km.
    · Environmental Lapse Rate: 6.49∘C/km (on average).
    Additional Knowledge: Lapse Rates:
    · Govern vertical temperature profiles in the atmosphere.
    · Crucial for understanding weather and cloud formation.
    Land and Sea Breezes:
    · Important for local weather patterns, particularly in coastal regions.
    Adiabatic Processes:
    · Play a critical role in atmospheric stability and convection.

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