1. Temperature inversion occurs when temperature increases with height in the troposphere, opposite to the normal lapse rate. This traps cooler air below warmer air, preventing vertical mixing. It often leads to fog, smog accumulation, and poor air quality, especially in urban and valley regions. TurnRead more

    Temperature inversion occurs when temperature increases with height in the troposphere, opposite to the normal lapse rate. This traps cooler air below warmer air, preventing vertical mixing. It often leads to fog, smog accumulation, and poor air quality, especially in urban and valley regions.

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  2. The Coriolis force, caused by Earth’s rotation, deflects moving air masses. Winds bend to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. This force shapes global wind patterns, cyclones and ocean currents, making it essential in understanding atmospheric circulationRead more

    The Coriolis force, caused by Earth’s rotation, deflects moving air masses. Winds bend to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. This force shapes global wind patterns, cyclones and ocean currents, making it essential in understanding atmospheric circulation systems.

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  3. A ceilometer is an instrument used to measure cloud height. It works by sending a laser beam upward and calculating the time taken for reflection from clouds. This helps meteorologists determine cloud base levels, which are important for weather forecasting and aviation safety operations worldwide.Read more

    A ceilometer is an instrument used to measure cloud height. It works by sending a laser beam upward and calculating the time taken for reflection from clouds. This helps meteorologists determine cloud base levels, which are important for weather forecasting and aviation safety operations worldwide.

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  4. In the Northern Hemisphere, winds around a low-pressure center move counter-clockwise due to the Coriolis force. Air converges inward and rises upward, forming clouds and often causing rainfall. This circular motion is typical in cyclones and is essential for understanding storm systems and weatherRead more

    In the Northern Hemisphere, winds around a low-pressure center move counter-clockwise due to the Coriolis force. Air converges inward and rises upward, forming clouds and often causing rainfall. This circular motion is typical in cyclones and is essential for understanding storm systems and weather patterns.

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  5. Horse latitudes are regions around 30° latitude where high pressure dominates, resulting in calm and weak winds. These areas experience dry conditions due to descending air. Historically, ships got stuck here due to lack of wind, giving the region its unique and memorable name. The Competitive ExamRead more

    Horse latitudes are regions around 30° latitude where high pressure dominates, resulting in calm and weak winds. These areas experience dry conditions due to descending air. Historically, ships got stuck here due to lack of wind, giving the region its unique and memorable name.

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