The primary source of energy that heats the atmosphere is the Sun. Solar radiation warms the Earth's surface, which in turn heats the lower atmosphere through conduction and convection. Additionally, the atmosphere also retains some heat from the Earth's surface.
Energy from the sun reaches the Earth through electromagnetic radiation, mostly in the form of visible light. This energy heats the Earth's surface, which in turn warms the atmosphere through convection and radiation. Some of the sun's energy is also absorbed by the atmosphere, contributing to its overall temperature and driving weather patterns.
Outer space is not considered part of the sun's atmosphere. The sun's atmosphere consists of layers such as the photosphere, chromosphere, and corona, which are directly connected to the sun itself. Outer space, on the other hand, is the vast expanse beyond the sun's outermost layer, where the sun's influence diminishes.
The sun has three main layers: the core, where nuclear fusion occurs; the radiative zone, where energy is transported by electromagnetic radiation; and the convective zone, where energy is transported by convection. The sun's atmosphere includes the photosphere, chromosphere, and corona.
From the Sun's core, energy moves through the radiative zone, across the tachocline (transition layer) to the convective zone, and then to the outer convective zone with its visible granulation.
The Sun is the main source of energy for convection in the atmosphere and the oceans. The Sun, heat radiated form the Sun is the main source of energy driving convection in the atmosphere and oceans. There is also a small input form geothermal energy.
The Sun is the main source of energy for convection in the atmosphere and the oceans. The Sun, heat radiated form the Sun is the main source of energy driving convection in the atmosphere and oceans. There is also a small input form geothermal energy.
The Sun is the main source of energy for convection in the atmosphere and the oceans. The Sun, heat radiated form the Sun is the main source of energy driving convection in the atmosphere and oceans. There is also a small input form geothermal energy.
The Sun is the main source of energy for convection in the atmosphere and the oceans. The Sun, heat radiated form the Sun is the main source of energy driving convection in the atmosphere and oceans. There is also a small input form geothermal energy.
Vertical convection in both the ocean and atmosphere is caused by uneven HEATing.The source of energy for convection in the ocean and atmosphere is heating from the sun.
the primary source of ocean currents is the sun but other direct energy sources are1. global wind patternsa. trade windsb. the westerly winds*wind is the cause of surface currents in the oceans.
convection!
Vertical convection in both the ocean and atmosphere is caused by uneven HEATing.The source of energy for convection in the ocean and atmosphere is heating from the sun.
The main cause of convection in the atmosphere is uneven heating of the Earth's surface by the sun. As air near the surface is heated, it becomes less dense and rises, creating vertical movement of air known as convection. This process is important for transferring heat and moisture throughout the atmosphere.
The primary source of energy that heats the atmosphere is the Sun. Solar radiation warms the Earth's surface, which in turn heats the lower atmosphere through conduction and convection. Additionally, the atmosphere also retains some heat from the Earth's surface.
The source of energy that drives convection within the Earth's atmosphere is primarily solar radiation. The sun heats the Earth's surface unevenly, causing air to warm and rise in some areas and cool and sink in others, creating convection currents. This process is responsible for distributing heat and moisture throughout the atmosphere.
Energy from the sun reaches the Earth through electromagnetic radiation, mostly in the form of visible light. This energy heats the Earth's surface, which in turn warms the atmosphere through convection and radiation. Some of the sun's energy is also absorbed by the atmosphere, contributing to its overall temperature and driving weather patterns.