How does the location of the continents affect the global climate?

According to tectonics theory of plates, tectonic plates carrying world continents slowly move in relation to each other and regroup them noticeably only in the time sections of millions of years. Tectonic boards move as fast as your nails grow. They are pushed by a phenomenon called the spread of the seabed, where the edges of the ocean plates are constantly set up on the cloak, allowing new magma to hurry to fill the cracks that form in the center of the album. The slits caused by the spread of the seabed are extending in one continuous line along the ocean floors of the world.

The location of the continents affects the global climate in several ways. The relative arrangement of continents can regulate the arrival and leaving the main ice ages more than solar cycles or any other factor. If there is a continent around the northern or southern polar regions, it is at risk that it becomes shiny and affecting the global climate. Especially in the case of Antaractica, which is exclusively polar, freezing Cirkopo beginsLara stream circulate the continent and causes feedback on cooling cycles. As a result, the Antarctic interior is the largest desert in the world; The desert is defined as the absence of moisture. Extremely low temperatures lock all the humidity in the ice.

Once, tens of millions of years, Antarctica was a fresh forest continent. During most of the planet's history, forests spread from pole to pole. Dinosaurs fossils were found to 20 degrees of Paleolatite of the South Pole. This is particularly remarkable because the dinosaurs had slower metabolism than mammals and probably did not deal with the cold. Their sensitivity to the global climate is probably what contributed to their fall. Their inability to deal with global climate changes is what led the mammal to survive the mass extinction of APRO dinosaurs (with the exception of birds ancestors).

Another factor that strongly influenceThe global climate is whether the continents are pushed against each other, as in the supercontinent of Panga, or to a large extent apart, as it is today. When the continents are together, it means that most of their soil is very far from the oceans, making moisture more difficult to get and produce deserts. It is assumed that the largest desert ever existed was the center of the continent of the pangea. Today, life in the interior of most continents is abundant, but then the Pange's Center would not have virtually all life.