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It is called solar gain.
Every location on Earth receives sunlight at least part of the year. The amount of solar radiation that reaches any one "spot" on the Earth's surface varies according to these factors:Geographic locationTime of daySeasonLocal landscapeLocal weather.Diffuse and Direct Solar RadiationAs sunlight passes through the atmosphere, some of it is absorbed, scattered, and reflected by the following: Air moleculesWater vaporCloudsDustPollutantsForest firesVolcanoes.This is called diffuse solar radiation. The solar radiation that reaches the Earth's surface without being diffused is called direct beam solar radiation. The sum of the diffuse and direct solar radiation is called global solar radiation. Atmospheric conditions can reduce direct beam radiation by 10% on clear, dry days and by 100% during thick, cloudy days.
The area on the dry sheltered side of a mountain that receives very little rain is called a "Rain Shadow"
The process that you describe is called, "Photosynthesis".
polar desert
When the side of the moon facing the earth receives no sunlight it is called a new moon
Mesopelagic
Photic zone
yes No. Everywhere on Earth receives sunlight, however in the polar regions in the winter there are many days without sunlight - this phenomenon is called the "Polar Night".
Photosynthesis takes place in chloroplasts. The chloroplasts contains the pigment called chlorophyll where it receives sunlight.
Photosynthesis takes place in chloroplasts. The chloroplasts contains the pigment called chlorophyll where it receives sunlight.
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The Moon only seems to "change shape". We only see one side of the Moon from Earth. The variation in the amount of sunlight hitting that side of the Moon, as it orbits Earth, is why we see the apparent changes in shape. These changes are called "lunar phases".
All of the Antarctic is considered on average, a desert. The polar plateau receives the least amount of precipitation and the Antarctic Peninsula receives the most.
The winter solstice.
is called the phases of the moon.