Climatology Basics Quiz
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Questions and Answers

Which of the following statements correctly describes the Coriolis Force?

  • The Coriolis Force is a force that deflects moving objects in the opposite direction of the Earth's rotation.
  • The Coriolis Force is a force that deflects moving objects to the left in the Northern Hemisphere and to the right in the Southern Hemisphere.
  • The Coriolis Force is a force that deflects moving objects in the same direction as the Earth's rotation.
  • The Coriolis Force is a force that deflects moving objects to the right in the Northern Hemisphere and to the left in the Southern Hemisphere. (correct)
  • Why does the equatorial region have low pressure?

  • The air in the equatorial region is being pulled by the Coriolis Force, creating low pressure.
  • The air in the equatorial region is cooler than the surrounding air, causing it to sink and create low pressure.
  • The air in the equatorial region is heated by the sun, causing it to rise and create low pressure. (correct)
  • The air in the equatorial region is constantly moving towards the poles, causing low pressure.
  • What is the primary cause of the subtropical high-pressure belts?

  • The Coriolis effect deflecting winds towards the poles.
  • The convergence of warm air from the tropics and cold air from the poles.
  • The rising of warm, moist air from the equatorial region.
  • The sinking of cool, dry air from the upper atmosphere. (correct)
  • How do surface currents contribute to the global energy balance?

    <p>Surface currents carry warm water from the tropics towards the poles, transferring heat energy to higher latitudes.</p> Signup and view all the answers

    What is the relationship between pressure belts and wind patterns?

    <p>Wind patterns are created by pressure belts, with air flowing from areas of high pressure to areas of low pressure.</p> Signup and view all the answers

    Which of the following is NOT a characteristic of the Subtropical High-pressure belt?

    <p>High precipitation</p> Signup and view all the answers

    Why does the air rise in the Intertropical Convergence Zone (ITCZ)?

    <p>The air is heated by the sun causing it to rise.</p> Signup and view all the answers

    What is the relationship between wind and global energy balance?

    <p>Winds carry heat energy from the tropics to the poles, helping to distribute heat energy more evenly around the Earth.</p> Signup and view all the answers

    What causes the unequal heating of the atmosphere?

    <p>Variations in solar radiation angle</p> Signup and view all the answers

    During which month does the southern hemisphere experience summer?

    <p>December</p> Signup and view all the answers

    What is the primary driver of deep ocean currents?

    <p>Differences in water density</p> Signup and view all the answers

    How do winds contribute to the poleward transfer of energy?

    <p>By transferring warm moist air from tropics</p> Signup and view all the answers

    Which statement best describes the 'heat equator'?

    <p>It shifts north and south with the seasons.</p> Signup and view all the answers

    What is one major effect of latitude on temperature?

    <p>Temperature variations decrease significantly at lower latitudes.</p> Signup and view all the answers

    Which factor does not influence insolation?

    <p>Geological activity</p> Signup and view all the answers

    What characterizes conditions associated with high pressure areas?

    <p>Sinking air and clear skies</p> Signup and view all the answers

    What is a characteristic of polar high pressure systems?

    <p>They are linked to cold, dense air in polar regions.</p> Signup and view all the answers

    Which statement accurately describes the surface winds of the Hadley cell?

    <p>They are referred to as tropical easterlies.</p> Signup and view all the answers

    What happens to air movement during the summer monsoon conditions?

    <p>Warm air rises over land reducing pressure there.</p> Signup and view all the answers

    What is the primary cause of the Coriolis force?

    <p>The rotation of the Earth.</p> Signup and view all the answers

    During monsoon winter conditions, what creates high pressure over mountains?

    <p>Cool air that sinks over the mountains.</p> Signup and view all the answers

    What is the role of the pressure gradient force in wind movement?

    <p>It causes air to move from high pressure to low pressure.</p> Signup and view all the answers

    How do westerly winds behave in the Northern Hemisphere?

    <p>They blow from the north-west.</p> Signup and view all the answers

    What defines the seasonal change observed in monsoon winds?

    <p>Alterations in the wind's prevailing direction.</p> Signup and view all the answers

    Study Notes

    Climatology

    • Climatology is the study of climate and weather patterns.
    • Temperature and pressure are key factors influencing weather patterns.

    Temperature and Pressure

    • High Pressure (HP):
      • Low temperature
      • Sinking air
      • Diverging air
      • Anticlockwise
      • Dry conditions
    • Low Pressure (LP):
      • High temperature
      • Rising air
      • Converging air
      • Clockwise
      • Cloud formation and wet conditions

    Unequal Heating of the Atmosphere

    • Earth's heating is influenced by insolation.
    • Insolation varies with latitude and seasons.
    • The amount of heat energy in the atmosphere depends on the amount of incoming solar radiation reaching the earth's surface.

    Latitude

    • The angle at which the sun's rays strike the Earth's surface affects the amount of solar radiation received.
    • The distance from the sun to the earth also plays a role in radiation intensity.
    • Polar regions receive less direct sunlight and have a lower intensity of radiation.

    Unequal Heating of the Atmosphere continued

    • Seasonal changes affect the intensity of insolation.
    • Locations near the equator experience less variation in temperature.
    • Heat energy is transferred from low latitudes to high latitudes.

    Heating Imbalances

    • The amount of incoming radiation is not the same everywhere, creating surpluses and deficits.
    • Radiation balance isn't uniform across the earth.
    • Areas experience more incoming radiation than outgoing radiation – surplus.
    • Conversely, areas receive less incoming radiation – deficit.
    • The total amount of surplus is equal to the total amount of deficits.

    Mechanisms for Energy Transfer

    • Winds move warm, moist air poleward from the tropics.
    • Ocean currents transport warm water to colder areas, and vice versa.
    • Deep ocean currents are driven by density differences in water (temperature and salinity).

    Activity

    • Students create diagrams depicting the solstice positions of the sun in relation to the Earth.
    • Diagrams include the tilt of the Earth, latitude lines, and arrows depicting the sun's rays.

    Currents

    • Surface currents circulate clockwise in the northern hemisphere and anticlockwise in the southern hemisphere.
    • Surface currents transport warm water toward the poles and cold water toward the equator.

    Energy Transfer by Wind

    • Winds horizontally transport heat energy across Earth.
    • Winds carry warm air from tropical regions to higher latitudes.
    • Winds also carry cold air from polar regions to lower latitudes.
    • This movement helps maintain a global energy balance.

    Unidirectional model of global circulation

    • Illustrates the interconnectedness of air circulation patterns around the planet.

    Important Forces

    • Coriolis force influences the deflection of moving objects (including air masses) due to the Earth's rotation.
    • Ferrel's Law explains the force and its effect on air circulation patterns.
    • Pressure gradient force is the difference in air pressure that causes air to move from high-pressure areas to low-pressure areas.

    World Pressure Belts

    • Pressure belts are arranged in specific locations around the Earth.
    • These belts are associated with temperature differences and with the movement of air (ascending or sinking).

    Three-Cell Circulation Model

    • The model describes the atmospheric circulations that transfer heat around the planet.
      • Equatorial Low (ITCZ): Rising air, associated with condensation, precipitation
      • Subtropical High: Sinking air, clear skies, little precipitation, deserts
      • Polar Low: Air masses cool, sinking, creates pressure systems.
    • Describes the three main circulation cells in the atmosphere

    Surface Winds

    • Easterly winds blow towards the ITCZ from subtropical high pressure belts.
    • Westerly winds blow away from the ITCZ towards the subpolar low.
    • Polar easterlies are surface winds of the polar cell.

    Further Description of the Three Cell Circulation Model

    • The model illustrates the air's movement and the associated weather systems.
    • The three cells (Hadley, Ferrel, Polar) illustrate the global air circulation model.

    Shifting ITCZ

    • The Intertropical Convergence Zone (ITCZ) shifts geographically through the year.
    • Shifting ITCZ impacts rainfall patterns and weather patterns.

    Trade Winds

    • Trade winds from the subtropical highs and towards the ITCZ

    Geostrophic Winds

    • Wind moves from high pressure to low pressure.
    • Pressure gradient force causes wind to move along the pressure difference.
    • Coriolis force deflects wind due to Earth's rotation.
    • Ferrel's Law: describes how Coriolis force affects wind direction in each hemisphere.

    Monsoon Winds

    • A seasonal reversal of wind direction.
    • In summer, winds blow from the ocean towards the land (moist).
    • In winter, winds blow from the land toward the ocean (dry).
    • Warm air rises over land; cool, dry air descends over land.
    • Land heats and cools faster than water, causing variations in pressure.

    Monsoon Summer Conditions

    • Air over land is warmer than surrounding sea water.
    • Warm air rises, creating low pressure over land.
    • Wind blows from the sea to land (moist).
    • Lots of evaporation from the ocean causes wet conditions.

    Monsoon Winter Conditions

    • Air over land is colder than surrounding sea water.
    • Cold air sinks, creating high pressure over land.
    • Wind blows from land towards the sea.
    • This results in dry conditions.

    Föhn Winds

    • Warm, dry winds that descend on the leeward side of mountains.
    • Moist air rises on the windward side, cools, and condenses to form precipitation.
    • Dry air descends on the leeward side, warming adiabatically, resulting in fewer clouds and reduced rainfall.

    Impacts of Berg Winds

    • Encourage veld fires, impacting the environment.
    • Farmers experience losses of equipment.
    • Wildfires impact natural environments, animals, and humans.
    • Drought and dry climates are common impacts of Berg Winds.
    • Berg winds can cause heat stroke, dehydration in humans and animals.

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