The atmosphere becomes less dense with altitude. Atmosphere, thin though it is, has weight, and it is the weight of the air above which compresses the air below it, to greater density.
The function that is decreasing is c) Air pressure in the Earth's atmosphere as a function of altitude. As altitude increases, air pressure decreases due to the thinning of the atmosphere. In contrast, outdoor temperature can vary with time depending on various factors, and the Dow Jones Industrial Average can increase or decrease based on market conditions.
The upper layers of the atmosphere are heated from above, while the lower layers are heated from below, because infrared radiation is given off by the Earth's surface in response to solar heating. The lower troposphere (with its denser molecules and water vapor) receives heat from both re-radiation and convection. The result is that while the atmosphere always gets thinner with altitude, the temperature decreases with altitude in the troposphere, then increases with altitude in the stratosphere. The very high temperatures in the thermosphere are moot because of the low specific heat (energy capacity) of the tenuous gases there.
Rockets generally pass through the Earth's atmosphere at an altitude of about 62 miles (100 kilometers) above the Earth's surface. This point is known as the Kármán line, which marks the boundary between Earth's atmosphere and outer space.
The earths atmosphere is made up of 78% nitrogen and 21% oxygen
Clouds are classified based on their altitude within the atmosphere and their appearance. Altitude classifications include high-level clouds, middle-level clouds, and low-level clouds. Appearance classifications include cumulus clouds (puffy and white), stratus clouds (layered and covering the sky), and cirrus clouds (thin and wispy).
The density of Earth's atmosphere decreases with altitude. As you move higher up in the atmosphere, there are fewer molecules of gases present, leading to lower density.
the altitude
Layers in Earth's atmosphere are primarily separated based on temperature variations caused by differences in altitude and composition. The troposphere is the layer closest to the Earth's surface, where temperature generally decreases with altitude. Above that is the stratosphere, where temperature begins to increase due to the presence of the ozone layer.
One-half of earth's atmosphere lies below the altitude of 5.6 kilometers
1.2 kg/m3at sea level and at 20 C
gas composition of atmosphere (including water vapour); altitude; temperature; and wind velocity.
The temperature zone layer of Earth's atmosphere shown in the cross-section is the stratosphere. This layer is characterized by an increase in temperature with altitude due to the presence of the ozone layer, which absorbs and scatters UV radiation from the sun.
Global. Warming
The gradual increase of the average air temperature in Earth's lower atmosphere is known as global warming.
Because the density of the force increases.
The lowest layer of Earth's atmosphere is called the troposphere. It is where the majority of Earth's weather occurs and contains around 75% of the atmosphere's mass. Temperature decreases with altitude in the troposphere.
Earth's weather primarily occurs in the troposphere, which is the lowest layer of the atmosphere where most of the weather phenomena such as clouds, rain, and storms take place. The thermosphere is a layer higher up in the atmosphere where temperatures increase with altitude due to interaction with solar radiation.