That's a very general question. In the broadest sense, Earth's atmosphere allows life to exist on the Earth. It's a mixture of approximately 78% Nitrogen, 21% Oxygen, and the remaining 1% of other gases (primarily argon). Oxygen, of course, is essential for animal life, and the carbon dioxide in the atmosphere allows for plant life. The atmosphere consists of 5 layers. The outermost layer, the Exosphere, is essentially space with some floating air molecules. The next innermost layer is the Thermosphere, and is, surprisingly, quite prone to extreme temperatures (temperatures are often much higher during daylight and colder during nighttime than Earth's surface at the same time). The next innermost layer is the Mesosphere, where the coldest temperatures on Earth may be found. Going inwards again, the next layer is the Stratosphere, which is particularly important because it contains the ozone layer, a layer of molecules (O3) which absorb harmful UV rays. Without the ozone layer, life could not exist in its present form. And finally we arrive at the Troposphere, which lies directly upon the Earth's surface. The air we breath is trapped in this layer, and much of our weather exists in this layer.
The rock cycle does not directly affect the atmosphere of the Earth. However, the processes within the rock cycle, such as weathering and erosion, can release carbon dioxide into the atmosphere. This can impact the Earth's climate by contributing to the greenhouse effect.
They slow the loss of heat
Variations in temperature can impact the density, pressure, and circulation of the Earth's atmosphere. This can lead to changes in weather patterns, such as the formation of clouds, precipitation, and storm development. Additionally, temperature changes can affect the balance of greenhouse gases in the atmosphere, leading to shifts in climate patterns over time.
As the Earth cooled down, gases such as carbon dioxide and water vapor in the atmosphere started to condense and form oceans. This led to a reduction in the amount of these greenhouse gases in the atmosphere, resulting in a shift towards the composition seen today with nitrogen dominating the atmosphere.
An example of how the atmosphere (air) sphere can affect the hydrosphere (water) sphere is through the process of evaporation. The atmosphere absorbs heat from the sun, causing water to evaporate from oceans, rivers, and lakes. This water vapor then condenses in the atmosphere and falls back to the Earth as precipitation, affecting the water cycle.
Air is Earth's atmosphere.
The rock cycle does not directly affect the atmosphere of the Earth. However, the processes within the rock cycle, such as weathering and erosion, can release carbon dioxide into the atmosphere. This can impact the Earth's climate by contributing to the greenhouse effect.
sexy
Earth's atmosphere has no effect on the moon.
The term "space weather" refers to conditions on the surface of the Sun that ultimately affect Earth and its atmosphere.
the atmosphere absorbs heat from solar radiation; which varies with latitude and seasons
It (gravity) keeps it (atmosphere) close to Earth.
The atmosphere naturally moves along with the Earth, as Earth rotates.Note that Earth's rotation may affect large-scale movements (currents) in the atmosphere - this is called Coriolis forces.
Nothing. Earth's atmosphere does not affect the sun. It does, however, cause Earth's atmosphere to retain more of the heat from the sun.
They slow the loss of heat
it dose not. but what dose is the atmosphere, & how close it is 2 the sun.
vechicle effect the earth by creating global warming into the atmosphere and destroying the o zone layer