themosphere
Air in contact with a warm surface is warmed in the winter and cooled in the summer due to heat exchange between the air and the surface. In winter, the warm surface transfers heat to the air, warming it. In summer, the cooler surface absorbs heat from the air, cooling it.
This is a very easy question to answer . Yes the air can be cooled or warmed by the surface below it because say if there was to be a earthquake right now in the ocean the heating of the surfaceunder the water would cause the water the make enormous wave and for te world to shake and depending on how hot the surface is heating.
Only partially, by warm winds. Mainly radiation from our Sun gives us heat.
well hot goes up and cold goes down
Rock is a very poor conductor of heat and there is quite a lot of it between the surface and the mantle. As a result heat conducts to the surface very slowly and quickly radiates into space. As a result the vast majority of heat at Earth's surface comes from the sun. The heat from the mantle is felt at erupting volcanoes where magma, which ultimately gets it heat from the mantle, reaches the surface.
The air in the troposphere is warmed by heat from the Earth's surface through the process of conduction and convection. As the Earth's surface absorbs solar radiation, it heats up and transfers some of this heat to the air directly above it. This warming of the air creates temperature gradients and drives weather patterns and atmospheric circulation.
Air warmed by heat from the Earth's surface is known as "thermal air" or "warm air." When the Sun heats the Earth's surface, it in turn warms the adjacent air, causing it to rise due to its lower density. This process is crucial for weather patterns and atmospheric circulation, as the rising warm air can lead to cloud formation and precipitation. Additionally, this warmed air plays a significant role in regulating the Earth's climate.
The lower atmosphere, known as the troposphere, is warmed by heat from Earth's surface. This warming is due to the absorption of outgoing radiation by greenhouse gases such as carbon dioxide and water vapor, which trap heat in the atmosphere.
Energy is transferred between the earths surface and the atmosphere via conduction, convection, and radiation. Conduction is the process by which heat energy is transmitted through contact with neighboring molecules.
pressure from the heat under the earths surface
Earth's surface is free to radiate heat into space. The interior is not. The interior does transfer heat the the surface, but rather slowly. It is hot due to residual heat from Earth's formation and from the heat generated by the decay of radioactive elements.
Air in contact with a warm surface is warmed in the winter and cooled in the summer due to heat exchange between the air and the surface. In winter, the warm surface transfers heat to the air, warming it. In summer, the cooler surface absorbs heat from the air, cooling it.
The surface of the Earth is more effectively warmed by radiation heat transfer than by conduction or convection. This is because radiation from the sun can penetrate the atmosphere and reach the Earth's surface, where it is absorbed and converted into heat. Conduction and convection play a role in redistributing this heat throughout the atmosphere.
Beneath the surface of the earth temperature remains the same. Within the Earth, irregular convection cells within the mantle transfer heat from the core to the surface of the planet. Volcanoes and earthquakes are two examples of heat transferring from the interior to the surface.
The sun heats the atmosphere. Solar radiation largely passes through the atmosphere and warms the surface of the earth. The earth then radiates heat up into the lower levels of the atmosphere where greenhouse gases warm. The warmed greenhouse gases then continue to radiate heat in all directions warming the atmosphere and again the earth's surface.
Heat from the sun
The atmosphere near Earth's surface is primarily warmed through the process of conduction, where heat is transferred from the Earth's surface to the air molecules in direct contact with it. Additionally, sunlight absorbed by the Earth's surface is re-radiated as heat, warming the surrounding air.