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Changes in Climate. Pgs 83 - 87. Ice Ages. The geologic record indicates that the Earth’s climate has been much colder than it is today. Ice ages are periods of time in which ice collects in high latitudes and moves toward lower latitudes.
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Changes in Climate Pgs 83 - 87
Ice Ages • The geologic record indicates that the Earth’s climate has been much colder than it is today. • Ice ages are periods of time in which ice collects in high latitudes and moves toward lower latitudes. • Major ice ages have occurred during the Earth’s history. • The most recent one started about 2 million years ago.
Glacial and Interglacial Periods • There are periods of cold and warmth during ice ages. • They are glacial and interglacial periods. • Glacial periods have large sheets of ice covering large areas. • The amount of water involved in a glacial period causes the sea level to drop. • Warmer times that occur between glacial periods are interglacial periods. • The last interglacial period began 10,000 years ago and is still occurring.
Motions of the Earth • Once theory that attempts to explain the gradual cooling and warming of the Earth is the Milankovitch theory. • His theory proposes that the changes in the Earth’s orbit and tilt of the Earth’s axis cause ice ages.
Volcanic Eruptions • Catastrophic events, like volcanic eruptions can influence the climate. • Volcanic eruptions send large amounts of dust, ash, and smoke into the atmosphere. • These particles block out the sun’s rays and cool the Earth.
Plate Tectonics • The climate is influenced by plate tectonics and continental drift too. • One ice age theory proposes that when the continents are aligned in polar regions, there is a greater chance for a glacial period. • We had a glacial period like this with Pangea over 250 million years ago.
Global Warming • Global warming – a rise in the average temperature that can result from an increase in the greenhouse effect. • The green house effect – the Earth’s natural heating process in which the gases in the atmosphere trap thermal energy. • Greenhouse gases allow sunlight to pass through the atmosphere, but trap heat absorbed by air molecules. • Greenhouse effect can increase if there is an increase in the amount of greenhouse gases in the atmosphere, like carbon dioxide. • Deforestation, clearing forests, aides to global warming because trees remove CO2 from the atmosphere.
Consequences of Global Warming • Some scientists think that if the average global temperature continues to rise, the polar ice caps will melt. • If they do, then the global sea level will rise and flood coastal cities. • Global climate patterns would change due to the new ocean level and amount of water vapor in the air.