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.
The sun can only shine on part of the earth's surface at any one time. This is why we have day and night in a rolling approach as the earth rotates.
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.
The troposphere is the layer of Earth's atmosphere where air is most likely warmed by conduction. This is the lowest layer of the atmosphere where weather events occur, and conduction is the main mechanism through which heat is transferred near the Earth's surface.
The atmosphere is warmed by the heat radiating from Earth's surface. This process helps to regulate the planet's temperature and create the conditions necessary for life to thrive.
It's warmed from the surface. Shortwave radiation passes through the atmosphere, or at least about half of it, where it reaches the ground and is absorbed. The ground re-emits it at a longer wavelength, thereby warming the lower atmosphere.
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.
The movement of the atmosphere redistributes heat and moisture, creating weather patterns such as winds, storms, and precipitation. This process helps regulate temperature differences between regions on Earth, leading to a more balanced climate system.
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.
By the emission of the terrestrial radiation. Terrestrial radiation is emitted in the infrared long-wavelength part of the spectrum. It is terrestrial radiation rather than solar radiation that directly warms the lower atmosphere.
The atmosphere helps keep earth's surface warm, but does not generate heat itself. The earth is warmed primarily by solar radiation (heat from the sun), and to a lesser extent by the slow decay of long lived heavy isotopes within earth's mantle and core.
The atmosphere helps keep earth's surface warm, but does not generate heat itself. The earth is warmed primarily by solar radiation (heat from the sun), and to a lesser extent by the slow decay of long lived heavy isotopes within earth's mantle and core.
Assuming that the atmosphere is distributed evenly all over the Earth, its center of mass is of course at the Earth's center. If for any reason there is more atmosphere on one side than on the other, the center of mass would be slightly away from Earth's center.