Answer:
They receive less radiation from the sun, due to their orientation relative to incoming sunlight.
Explanation:
Earth has multiple different climate zones, roughly arranged by latitude. The difference in climates comes because of multiple factors, but the most important one is the Sun and the sunlight of it. Because Earth has a rounded shape, different parts of it receive different amounts of sunlight.
If we compare the tropical and polar regions as two contrasting regions, we can see huge differences. The tropical regions are warm or hot all year round, while the polar regions are very cold throughout all of the year. The tropical regions though receive sunlight at a much more direct angle, thus the sunlight is much more concentrated and heats up the region. The polar regions receive sunlight at a very low angle, so they are dispersing over a very wide area so they can not warm up the region.
Answer:
5A: Northwest Region: Rocky Mountains
2B: West Region: Great Basin Desert
4C: South West Region: Grand Canyon
3D: Midwest Region: Great Plains
6E: Southeast Region: Everglades
1F: Mid-Atlantic Region: Many bays and good harbors
7G: Northeast Region: Rocky coastline and small coastal islands
Explanation:
Answer:
Convectional precipitation
Explanation:
<em>Convectional precipitation is a type of precipitation that occurs in the low latitudes. </em>
The low latitudes are typically the tropical belt of the world which straddles the equator.
- During convectional precipitation, high amount of solar insolation rapidly heats the ground evaporating surface water to form rain clouds.
Orographic precipitation occurs in high altitude regions. The peaks causes the formation of rain clouds which leads to a mountain have a windward and leeward sides.
Frontal precipitation occurs at the point of convergence of two air masses, one warm and the other cold.
So, convectional precipitation is the appropriate choice here.
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