Because the rays of the sun bounces off the clouds and back into space before reaching the surface of the Earth.
High clouds (like cirrus clouds) tend to have a cooling effect on the Earth's surface by reflecting incoming solar radiation back to space. Low clouds (like stratus clouds) can have a warming effect by trapping heat and reducing the amount of outgoing longwave radiation that escapes into space.
Clouds can cool down the Earth by reflecting incoming sunlight back into space, which reduces the amount of solar radiation reaching the Earth's surface. They also increase the Earth's albedo, which is its ability to reflect sunlight. Additionally, clouds can trap heat radiated from the Earth's surface, but their overall cooling effect usually outweighs this warming effect.
Clouds can slow the rate of the Earth's heating by reflecting incoming solar radiation back into space, which reduces the amount of sunlight reaching the Earth's surface. Additionally, clouds can also absorb and emit thermal radiation, trapping some of the heat emitted by the Earth and preventing it from escaping into space.
No, the total amount of water on Earth remains relatively constant due to the water cycle. Water evaporates from bodies of water, condenses into clouds, and falls back to Earth as precipitation. This cycle ensures that the overall amount of water on Earth remains constant.
Cumulus clouds are typically closer to the Earth than cirrus clouds. Cumulus clouds are generally found at lower altitudes, while cirrus clouds are found at higher altitudes.
Yes, the presence of clouds can affect the amount of solar energy intercepted by Earth. Clouds can reflect, absorb, and scatter solar radiation, reducing the amount of sunlight that reaches the Earth's surface. This can impact the overall energy balance of the Earth's climate system.
The ozone layer has the greatest effect on the amount of ultraviolet radiation received at the earth's surface from the Sun. Cloud formation and atmospheric thickness, in combination with solar angle, have the greatest effect on the amount of visible and infrared radiation received at the earth's surface from the sun
High clouds (like cirrus clouds) tend to have a cooling effect on the Earth's surface by reflecting incoming solar radiation back to space. Low clouds (like stratus clouds) can have a warming effect by trapping heat and reducing the amount of outgoing longwave radiation that escapes into space.
Parallax
The amount of starlight received on Earth varies depending on factors like the distance from the star, the star's luminosity, and atmospheric conditions. On average, about 1 billionth of the total light emitted by the Sun reaches Earth's surface, providing energy for life and driving Earth's climate system.
Clouds can cool down the Earth by reflecting incoming sunlight back into space, which reduces the amount of solar radiation reaching the Earth's surface. They also increase the Earth's albedo, which is its ability to reflect sunlight. Additionally, clouds can trap heat radiated from the Earth's surface, but their overall cooling effect usually outweighs this warming effect.
Rain can reduce the amount of clouds in the sky, because they are apart of the water cycle. Another name of the process of the clouds is 'condensation'. When the liquid from the clouds overflows from evaporation, the clouds rain. Rain can also add water to the underwater storage after soaking into the earth. The process of going to the underwater storage is called 'infiltration'. The rain can also nourish the plants on earth. I hope this information helps!
There will be no earth there will only clouds
Yes. There are ALWAYS clouds somewhere on Earth.
Clouds can slow the rate of the Earth's heating by reflecting incoming solar radiation back into space, which reduces the amount of sunlight reaching the Earth's surface. Additionally, clouds can also absorb and emit thermal radiation, trapping some of the heat emitted by the Earth and preventing it from escaping into space.
differences in the amount of heat received at different regions of the Earth
The amount of solar energy received in a particular area changes throughout the year mainly due to the Earth's tilt and its orbit around the sun. This results in varying angles of sunlight hitting the Earth's surface, affecting the intensity and duration of sunlight received in different seasons. Additionally, factors like cloud cover, atmospheric conditions, and geographic location also contribute to the variations in solar energy received.