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- Evaporation
- Forms clouds
- Rains down
Q 2
Cirrus:
cirrus cloud is a spiral wispy looking cloud that are very thin, the cirrus cloud is mainly made up of ice crystals and are usually found high above the earths surface.
Cumulus:
These clouds are puffy like cotton wool, on fine days these clouds are found scattered across the sky.
Stratus:
These clouds are usually sheets or layers across the sky.

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It begins to build up in thunder clouds as small ice particles lift higher than larger ones. The small particles carry a +(positive) charge and the larger ones a -(negative) charge

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When a large difference in a vertical column in the atmosphere

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Tornado's form when strong updraughts of air rise in a funnel shape. The air touching the earth moves slower that the air above it. This causes the air to 'roll over' and get sucked up, rotating through the inside of the cloud.

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Some examples of extreme  weather are: Hurricanes, tornado's, lightning and thunder.

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Extreme weather can make a big impact on many people and plants. Something else that it damages is farmers, because when it rains a lot it makes farms very very wet, and then when cattle go in there they pug the ground and it can ruin paddocks very quickly.

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Low pressure areas are marked with a "L". Low pressure areas face wind inwards. These winds push the warm air up like a funnel, and cool air rushes in to replace it. As the warm air rises it cools, forming water vapour and then clouds, leading them to rain.

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Areas of high pressure are marked with a "H" and this represents "fine" weather with few clouds. Wind on edge of "H" can be strong.

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The lines on the weather maps are called "isobars". The numbers on the lines show the air pressure.

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The weather maps we see on T.V and in the newspaper and are called "surface charts". The lines and symbols represent weather patterns on earth.

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The sun warms up the land and sea. This heat radiates upwards. As the warm air rises it expands. As it expands it cools down. The now colder air becomes denser and sinks back to earth. We experience this circulation of air as wind.

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Same as hail but without the wind forcing it back into the clouds.

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If the temperature in the atmosphere is freezing, the water vapour forms into ice which drops down from the clouds as hail. Wind gusts push the snow back up into the clouds lot's of times breaking it into hailstones.

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As water vapour evaporates into the air, it joins together with other water droplets to form clouds. When the clouds are to heavy the water vapour falls as rain ( precipitation).