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Weather dynamics Day 2 – Heat Science 10.

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Presentation on theme: "Weather dynamics Day 2 – Heat Science 10."— Presentation transcript:

1 Weather dynamics Day 2 – Heat Science 10

2 Heat Thermal energy: the energy of the average movement of the particles (atoms, ions, molecules) of a substance Heat: transfer of thermal energy from one object to another. Goes from high to low thermal energy

3 Heat transfer There are 3 methods of heat transfer conduction convection radiation Song:

4 Conduction Conduction: heat transfer through collisions between high and low energy particles Usually with solids i.e. a pot on the stove or between a solid and a liquid/gas

5 Convection Convection: heat transfer during which high energy particles rise. Hot particles rise (because they are less dense) Cold particles fall (because they are more dense) This movement creates convection currents. Usually with liquids and gases – Why not with solids?

6 Radiation Radiation: heat transfer through electromagnetic waves.
These waves transport energy through space and release it only when they interact with certain types of matter No particles are necessary for this transfer

7 Types of Thermal Energy Transfer

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9 The Earth’s Energy Budget
No life on Earth would be possible if all the Sun’s energy was absorbed by the biosphere (land, air, water) without losing any of it Temperature would continue rising too high The Earth radiates as much energy into space as it absorbs from the Sun Radiation back into space = absorption from Sun

10 Heating Air Solar radiation is the primary source of energy that heats soil and water.

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13 Wind Wind is created from unequal heating of air.

14 To Do Day 2 Questions


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