The sun's heat is distributed throughout the world by a process called radiation. This involves the sun emitting energy in the form of electromagnetic waves, which travel through space and warm the Earth's atmosphere and surface when they are absorbed. Heat is then further distributed through processes like conduction, convection, and ocean currents.
The Earth retains heat better due to its thicker atmosphere and higher heat capacity compared to the moon. The atmosphere acts as a barrier, trapping heat on Earth, while the moon has no atmosphere to retain heat, causing rapid heat loss at night.
The three types of heat transfer that work together to heat the atmosphere are conduction, convection, and radiation. Conduction transfers heat from the Earth's surface to the lower atmosphere through direct contact. Convection carries heat upward through the atmosphere by warm air rising and cool air sinking. Radiation from the sun warms the Earth's surface, which then radiates heat back into the atmosphere. Together, these processes create a dynamic system that helps regulate the temperature of the atmosphere.
No, a planet without an atmosphere cannot have a greenhouse effect because the atmosphere is necessary to trap heat and create the warming effect. Without an atmosphere, there is no mechanism to retain heat and create the greenhouse effect.
Jupiter is much warmer than Mars. Jupiter's atmosphere contains gases that trap heat, creating extremely high temperatures throughout the planet. Mars, on the other hand, has a thin atmosphere that does not retain heat well, resulting in much colder temperatures.
IDONTKNOW
Yes, heat energy is constantly redistributed globally through processes such as ocean currents, atmospheric circulation, and the water cycle. This helps to regulate Earth's climate and temperature by moving heat from warmer regions to cooler regions.
# Coduction # Radiation # Convention # Latent heat # Heat pipes # I learned that convection currents transfer heat throughout the troposphere. (part of the atmosphere)
Heat is primarily transferred through the atmosphere through convection, where warmer air rises and cooler air sinks. This process creates circulation patterns that distribute heat around the globe. Additionally, heat can also be transferred by radiation as the sun's rays heat the Earth's surface and atmosphere.
Heat primarily travels in the atmosphere through convection, where warm air rises and cooler air sinks. This process creates vertical movement of air, helping to distribute heat throughout the atmosphere. Additionally, heat can also be transferred through radiation, where the Earth absorbs and emits heat energy from the sun.
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.
Heat energy is redistributed through processes such as conduction, convection, and radiation. In conduction, heat is transferred through direct contact between materials. Convection involves the movement of fluids to distribute heat. Radiation transfers heat through electromagnetic waves. These processes work together to redistribute thermal energy in various systems.
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.
Two examples of convection are sea breezes and thunderstorms. Convection contributes to the movement of heat in the atmosphere by transferring heat from the Earth's surface to the air through the process of warm air rising and cool air sinking. This creates vertical movement of air, which helps distribute heat throughout the atmosphere.
Most of the energy in Earth's atmosphere, oceans, and living systems comes from the sun. Solar radiation is absorbed by the Earth's surface and then redistributed throughout the planet through processes like convection, evaporation, and the water cycle, powering various systems and processes in the environment.
Through deep ocean currents and atmosphere currents i.i the elnemo (high speed jet wind current) circulating the globe.
it is spread by a fire being started because the wind can blow it through the atmosphere because smoke is just like oxygen and it is light .