Answer: Tempeture, air pressure, centripetal acceleration and Earth rotation.
<u>Temperature: </u>Warm air and cold air have different density. As warm air is less dense than cold air, it rides up and over the cold air causing winds.
<u>Air Pressure: </u>At the Earth's surface, wind blows horizontally from high pressure to low pressure areas. Wind is faster in bigger pressure differences.
<u>Centripetal Acceleration:</u> air speed is influenced by centripital acceleration this way, the direction of wind in the center of the circulation is also influenced. Cyclones, for example, are a association of centripital acceleration and air pressure differences.
<u>Earth's Rotation:</u> Wind direction chance can be caused by the rotation of Earth on its axis. The Coriolis effect, easterlies are examples of the influence of the earth’s rotation on Wind.
Answer:
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Water pollution affects marine ecosystems by completely killing it off. Pollution kills fish, reefs, and other underwater life. With this pollution, animal's behaviors can change, and habitats are destroyed.
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Fossils.
Early in the 20th century, Alfred Wegener, primarily, established the continental drift theory. According to Wegener, continents are mobile on the surface of the Earth and were previously connected to form a single supercontinent. Scientists did not think that the continents could migrate when Wegener was alive.
In rocks that are the same age but on continents that are currently far apart, ancient fossils of the same species of extinct plants and animals can be found. Wegener claimed that the species had coexisted, but that once they died and become petrified, the lands had separated. According to his theory, the creatures couldn't have crossed the seas.
1. Glossopteris seed fern fossils were too heavy for the wind to carry them that far.
2. Mesosaurus was a reptile that could swim, although it could only do it in freshwater.
3. The terrestrial reptiles Cynognathus and Lystrosaurus were incapable of swimming.
Learn more about continental drift theory here:
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