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  • Rights: The University of Waikato
    Published 15 April 2009 Referencing Hub media
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    In this video, Dave Campbell and Keith Hunter discuss what weather1 and climate2 are, and how the water cycle3 is key to the weather. Weather describes the condition4 of the air masses overlying land and sea. Climate refers to a pattern of weather over a period of time (such as a season). Weather is the ‘here and now’, while climate is an accumulation of many days’ or even years’ worth of information about the weather.

    Weather and climate are complex processes with many influences: solar radiation5, the tilt of the Earth’s axis, landscape (including buildings and cities), seasons, time of day and human activities. Approximately half of the incoming solar radiation6 is used in evaporating water to the atmosphere7. This water then becomes our weather, which can then recharge water resources of the rest of the planet8 through precipitation9

    Points of interest: Find out what latent heat10 is and why it is important. What is the source of heat energy11 that drives the water cycle?

    Transcript

    PROF DAVID HAMILTON
    The weather and climate are what we call meteorological variables, and they will include important things such as radiation or sunshine, wind, humidity12 and air temperature13 of course.

    NARRATOR
    The water cycle is driven by energy from the sun. Liquid water is evaporated and changed into a gas. This vapour rises and circulates in the atmosphere, cools and changes back into a liquid. This process is called condensation14. Tiny droplets of water in the atmosphere accumulate to form clouds, which then return the water to Earth as rain or snow. The rate of evaporation15 depends on 4 main conditions16 – water body size, heat energy17, atmosphere pressure18, and air movement.

    PROF KEITH HUNTER
    The ocean has a dominant influence on climate and temperature. The process of evaporation of seawater near the equator transfers water vapour19 to the atmosphere, and ultimately recharges all of the water resources on the rest of the planet. But along with that water, the one thing you have to do if you want to convert liquid water into water vapour is you have to provide heat20 energy, and the heat energy is held within the molecules21 of water while they are present in the gas phase, and we call that latent heat

    NARRATOR
    The sun is the source of the heat energy that drives the water cycle and, in turn, influences the weather and climate.

    DR DAVE CAMPBELL
    Roughly a half of the solar radiation that is absorbed at the Earth's surface is used up in evaporating water – in other words, converting water from its liquid form to water vapour as a gas in the atmosphere. So when we talk about a hydrological cycle – which is the movement of water from the surface into the atmosphere, and then it condenses and forms precipitation, falls out as either rain or snow onto the land or ocean surface and then moves back into the ocean if it’s coming off the land.

    PROF KEITH HUNTER
    And when the water vapour condenses back into rain again, then that latent heat is released as heat energy, and it’s that heat energy which drives the wind systems of the atmosphere. It’s that heat energy that causes hurricanes. So if you get a warm period in the Gulf of Mexico, where you get lots of evaporation, then you get hurricanes being formed, and they are at the extreme end of the climate spectrum. But basically wind is created largely by this exchange of heat energy that results from the condensation of water that has come from the ocean.

    Acknowledgements:
    Prof. David Hamilton, Waikato University
    Prof. Keith Hunter, Otago University
    Dr David Campbell, Waikato University

    Sun image, Lykaestria, licensed under Creative Commons
    Globe image, courtesy of NASA
    Wind computer model, Peyman Zawar-Reza, University of Canterbury
    Christchurch smog image, Dr Simon Kingham, University of Canterbury

    1. weather: Daily or short-term conditions like temperature, cloud cover, precipitation and wind affecting a certain area.
    2. climate: The weather conditions of an area averaged over a series of years, usually 30 or more.
    3. water cycle: The continuous movement of water on, above and below the surface of the Earth (also known as the hydrological cycle).
    4. condition: An existing state or situation; a mode or state of being.
    5. solar radiation: Radiant energy emitted by the Sun as a result of nuclear fusion reactions.
    6. radiation: Energy that is transmitted (radiates) from a source in the form of rays or waves or particles.
    7. atmosphere: 1. The layer of gas around the Earth. 2. (atm) A non-SI unit of pressure equivalent to 101.325 kPa.
    8. planet: In our Solar System, a planet is defined as an object that orbits the Sun, is big enough for its own gravity to make it ball-shaped and keeps space around it clear of smaller objects.
    9. precipitation: 1. The formation of an insoluble solid (precipitate) from a given solution by altering either its temperature, concentration or chemical composition. 2. In meteorology, this term describes the formation of rain, hail, snow or ice in the atmosphere.
    10. latent heat: The heat necessary to transform from one state of matter (i.e. solid) to another (i.e. liquid) without a rise in temperature until the change is completed.
    11. heat energy (heat): Heat energy: the transfer of energy in materials from the random movement of the particles in that material. The greater the random movement of particles the more heat energy the material has. Temperature is a measure of the heat energy of a material.
      Heat: the flow of energy from a warm object to a cooler object.
    12. humidity: The amount of water vapour in the air.
    13. temperature: A measure of the degree of hotness or coldness of an object or substance. Temperature is measured with a thermometer calibrated in one or more temperature scales. Kelvin scale temperature is a measure of the average energy of the molecules of a body.
    14. condensation: A change of molecular state where gas becomes liquid due to cooling.
    15. evaporation: The process by which a liquid is converted into a gas, without necessarily reaching the boiling point.
    16. condition: An existing state or situation; a mode or state of being.
    17. heat energy (heat): Heat energy: the transfer of energy in materials from the random movement of the particles in that material. The greater the random movement of particles the more heat energy the material has. Temperature is a measure of the heat energy of a material.
      Heat: the flow of energy from a warm object to a cooler object.
    18. pressure: The force per unit area that acts on the surface of an object.
    19. water vapour: The gas phase of water.
    20. heat energy (heat): Heat energy: the transfer of energy in materials from the random movement of the particles in that material. The greater the random movement of particles the more heat energy the material has. Temperature is a measure of the heat energy of a material.
      Heat: the flow of energy from a warm object to a cooler object.
    21. molecule: Two or more atoms bonded together. The molecule of an element has all its atoms the same. The molecule of a compound has two or more different atoms.
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      weather

    1. + Create new collection
    2. Daily or short-term conditions like temperature, cloud cover, precipitation and wind affecting a certain area.

      condition

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    4. An existing state or situation; a mode or state of being.

      atmosphere

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    6. 1. The layer of gas around the Earth.

      2. (atm) A non-SI unit of pressure equivalent to 101.325 kPa.

      latent heat

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    8. The heat necessary to transform from one state of matter (i.e. solid) to another (i.e. liquid) without a rise in temperature until the change is completed.

      temperature

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    10. A measure of the degree of hotness or coldness of an object or substance. Temperature is measured with a thermometer calibrated in one or more temperature scales. Kelvin scale temperature is a measure of the average energy of the molecules of a body.

      pressure

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    12. The force per unit area that acts on the surface of an object.

      climate

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    14. The weather conditions of an area averaged over a series of years, usually 30 or more.

      solar radiation

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    16. Radiant energy emitted by the Sun as a result of nuclear fusion reactions.

      planet

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    18. In our Solar System, a planet is defined as an object that orbits the Sun, is big enough for its own gravity to make it ball-shaped and keeps space around it clear of smaller objects.

      heat energy (heat)

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    20. Heat energy: the transfer of energy in materials from the random movement of the particles in that material. The greater the random movement of particles the more heat energy the material has. Temperature is a measure of the heat energy of a material.
      Heat: the flow of energy from a warm object to a cooler object.

      condensation

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    22. A change of molecular state where gas becomes liquid due to cooling.

      water vapour

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    24. The gas phase of water.

      water cycle

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    26. The continuous movement of water on, above and below the surface of the Earth (also known as the hydrological cycle).

      radiation

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    28. Energy that is transmitted (radiates) from a source in the form of rays or waves or particles.

      precipitation

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    30. 1. The formation of an insoluble solid (precipitate) from a given solution by altering either its temperature, concentration or chemical composition.

      2. In meteorology, this term describes the formation of rain, hail, snow or ice in the atmosphere.

      humidity

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    32. The amount of water vapour in the air.

      evaporation

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    34. The process by which a liquid is converted into a gas, without necessarily reaching the boiling point.

      molecule

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    36. Two or more atoms bonded together. The molecule of an element has all its atoms the same. The molecule of a compound has two or more different atoms.