tha atmosphere has a lower heat capacity
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's average surface temperature during the twentieth century was around 13.9 to 15.1 degrees Celsius, depending on data sources.
Temperature increases as you move from the Earth's surface towards the center. This is because the Earth's core is extremely hot due to the heat generated from radioactive decay and residual heat from the planet's formation.
When the sun's rays are concentrated, the temperature on Earth can vary greatly depending on factors such as location, time of day, and atmospheric conditions. In general, the temperature can reach over 100 degrees Fahrenheit in areas like deserts where sunlight is intense and there is little cloud cover to block it.
During the Precambrian time, the Earth's atmosphere underwent significant changes, transitioning from a reducing atmosphere dominated by gases like methane and ammonia to an oxidizing atmosphere with increasing levels of oxygen, due to the development of photosynthetic organisms. This increase in oxygen levels laid the foundation for the evolution of complex multicellular life forms.
The atmosphere has lower heat capacity
The temperature on the moon ranges from roughly +100C during the lunar day to -100C during the lunar night.
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 earths axis is not tilted directly toward the sun.
it depends on the deepth
The Earth's average surface temperature during the twentieth century was around 13.9 to 15.1 degrees Celsius, depending on data sources.
Temperature increases as you move from the Earth's surface towards the center. This is because the Earth's core is extremely hot due to the heat generated from radioactive decay and residual heat from the planet's formation.
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When the sun's rays are concentrated, the temperature on Earth can vary greatly depending on factors such as location, time of day, and atmospheric conditions. In general, the temperature can reach over 100 degrees Fahrenheit in areas like deserts where sunlight is intense and there is little cloud cover to block it.
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Heats it up
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