Expands --- Nova Net Answer
Energy from the geosphere is primarily transferred to the atmosphere through processes like radiation and conduction. Solar radiation heats the Earth's surface, which in turn heats the air above it. This warmed air rises due to convection, transferring energy to the atmosphere.
Convection heats the atmosphere by transferring heat through the movement of air masses. Warm air near the Earth's surface rises as it becomes less dense, creating upward motion that transports heat to higher altitudes. This process helps distribute heat throughout the atmosphere and contributes to the formation of weather systems.
The atmosphere. As you go higher in elevation, the atmosphere becomes thinner because the air pressure decreases, leading to lower air density.
The process that transfers energy from the warm surface of the Earth to air particles in the atmosphere is called convection. As the Earth's surface heats up, the air in contact with it also warms up and becomes less dense, causing it to rise. This rising warm air transfers energy to the surrounding cooler air particles through convection currents.
The atmosphere near Earth's surface is heated from below primarily through the process of conduction. This occurs as the Earth's surface absorbs solar radiation and heats up, transferring this heat to the adjacent air molecules through direct contact. As the air warms, it becomes less dense and rises, creating convective currents that distribute the heat throughout the atmosphere.
yes
Air loses density when it heats up because the air molecules become more energetic and spread out, resulting in a decrease in density. Conversely, air becomes more dense when it cools down because the molecules lose energy and come closer together.
The Sun's energy heats the atmosphere.
It heats up a lot and becomes vey hot.
Convection occurs in the atmosphere due to temperature differences between the Earth's surface and the air above it. As the Sun heats the surface, the air near the surface becomes warmer and less dense, causing it to rise. This creates vertical air currents and leads to the circulation of air in the atmosphere.
As the air in the troposphere heats up from the sun, it becomes less dense and starts to rise. This movement creates vertical air currents and leads to the formation of clouds and precipitation. This process is known as convection.
Energy from the geosphere is primarily transferred to the atmosphere through processes like radiation and conduction. Solar radiation heats the Earth's surface, which in turn heats the air above it. This warmed air rises due to convection, transferring energy to the atmosphere.
Convection heats the atmosphere by transferring heat through the movement of air masses. Warm air near the Earth's surface rises as it becomes less dense, creating upward motion that transports heat to higher altitudes. This process helps distribute heat throughout the atmosphere and contributes to the formation of weather systems.
The atmosphere. As you go higher in elevation, the atmosphere becomes thinner because the air pressure decreases, leading to lower air density.
When one ascends in the atmosphere, the air becomes thinner, which means the molecules are more spread out, leading to lower air pressure. Additionally, the temperature typically decreases as you go higher in the atmosphere due to the decrease in density and energy of the air molecules.
The atmosphere is primarily heated by the sun. Solar radiation warms the Earth's surface, which in turn heats the air above it. Other factors that can influence atmospheric warming include greenhouse gases and human activities that release heat-trapping emissions into the atmosphere.
A meteoroid is a solar system object that enters Earth's atmosphere and becomes very hot due to friction with the air. As it travels through the atmosphere, the meteoroid heats up and creates a bright streak of light called a meteor, commonly known as a shooting star.