because it is near in the sun and it gets direct light.
The tilt of the Earth's axis causes different parts of the Earth to receive sunlight more directly, leading to variations in temperature and different seasons. As the Earth orbits the sun, the varying angle of sunlight reaching different regions causes changes in temperature throughout the year.
The term used to describe the gradual increase of the average air temperature in the Earth's lower atmosphere is "global warming."
Approximately 30% of Earth's land does not receive sufficient precipitation, making it arid or semi-arid. This can lead to desertification and impact ecosystems and human livelihoods in these regions.
Regions away from the equator receive less solar radiation because the angle at which the sunlight strikes the Earth's surface is more oblique, spreading the energy over a larger area. This reduces the intensity of solar radiation received compared to the more direct and concentrated sunlight at the equator.
The Earth's temperature range can vary greatly depending on the location and time of year. On average, Earth's temperature ranges from about -50°C in Antarctica to about 50°C in hot desert regions.
Regions of the earth that receive less heat, such as polar regions and higher altitudes, tend to have colder air temperatures compared to areas near the equator. This is due to the angle of the sun's rays and the amount of daylight hours these regions receive, resulting in less direct sunlight and warmth. This leads to cooler temperatures in these areas.
NEAR THE pOLES
The tilt of the Earth's axis causes different parts of the Earth to receive sunlight more directly, leading to variations in temperature and different seasons. As the Earth orbits the sun, the varying angle of sunlight reaching different regions causes changes in temperature throughout the year.
The six climate regions are primarily defined by factors such as temperature, precipitation, humidity, and vegetation patterns. These regions help geographers classify and understand the diverse climates found on Earth.
The term used to describe the gradual increase of the average air temperature in the Earth's lower atmosphere is "global warming."
Earth's polar regions are the areas of the globe surrounding the poles also known..part of what little sunlight the Polar regions receive, contributing to the cold.
Approximately 30% of Earth's land does not receive sufficient precipitation, making it arid or semi-arid. This can lead to desertification and impact ecosystems and human livelihoods in these regions.
Temperature, Wind, Position of the Earth
Regions away from the equator receive less solar radiation because the angle at which the sunlight strikes the Earth's surface is more oblique, spreading the energy over a larger area. This reduces the intensity of solar radiation received compared to the more direct and concentrated sunlight at the equator.
The Earth's temperature range can vary greatly depending on the location and time of year. On average, Earth's temperature ranges from about -50°C in Antarctica to about 50°C in hot desert regions.
The Earth has two hemispheres: the Northern Hemisphere and the Southern Hemisphere, divided by the Equator. These hemispheres are often used to describe different regions or seasons on Earth.
The regions on Earth where life is possible are called habitable zones. These zones are characterized by suitable conditions such as the presence of water, appropriate temperature, and a stable environment that can support life.