decrease due to expansion
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.
When a humid air mass rises into a cooler temperature area, it may form clouds, precipitation, and potentially thunderstorms. The air cools as it rises, causing the water vapor to condense into droplets, which eventually leads to the formation of clouds and precipitation. This process is known as adiabatic cooling.
A large section of the lower troposphere with uniform temperature and humidity is called an air mass. Air masses are large bodies of air with relatively homogeneous properties that form over specific regions of the Earth's surface.
The troposphere is the lowest layer of Earth's atmosphere, extending from the surface to about 10-15 kilometers in altitude. It is where the majority of Earth's weather occurs and contains most of the atmosphere's mass, water vapor, and aerosols. Temperature generally decreases with altitude in the troposphere.
Large sections of the troposphere with the same temperature and humidity are known as air masses. These air masses can cover thousands of square kilometers and are characterized by their uniform temperature and humidity profiles. When air masses with different properties meet, they can lead to changes in weather patterns.
air mass
No. The majority of it is in the troposphere, but not all of it.
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.
When a humid air mass rises into a cooler temperature area, it may form clouds, precipitation, and potentially thunderstorms. The air cools as it rises, causing the water vapor to condense into droplets, which eventually leads to the formation of clouds and precipitation. This process is known as adiabatic cooling.
A large section of the lower troposphere with uniform temperature and humidity is called an air mass. Air masses are large bodies of air with relatively homogeneous properties that form over specific regions of the Earth's surface.
The troposphere is the lowest layer of Earth's atmosphere, extending from the surface to about 10-15 kilometers in altitude. It is where the majority of Earth's weather occurs and contains most of the atmosphere's mass, water vapor, and aerosols. Temperature generally decreases with altitude in the troposphere.
Large sections of the troposphere with the same temperature and humidity are known as air masses. These air masses can cover thousands of square kilometers and are characterized by their uniform temperature and humidity profiles. When air masses with different properties meet, they can lead to changes in weather patterns.
as we know that energy is associated with matter i.e. energy cannot be present without matter but matter can be without energy. as we go up in atmosphere density decreases mass also decreases due to which most of the energy escapes
troposphere
yes.
An increase in temperature usually causes an increase in volume. Since the mass doesn't change, density decreases. tt
As altitude increases, the temperature usually decreases in the troposphere, which is the layer of the atmosphere where weather occurs. This relationship is known as the lapse rate. The altitude of a base cloud can vary depending on the temperature and humidity of the air mass it forms in.