Air molecules spread out and heat up primarily in the troposphere, which is the lowest layer of the Earth's atmosphere. This layer extends from the surface up to about 8 to 15 kilometers (5 to 9 miles) high, depending on geographic location and weather conditions. The troposphere is where most weather phenomena occur, and it is heated by the Earth's surface, causing air to rise and cool as it expands.
The thermosphere is the hottest layer of the Earth's atmosphere because it absorbs high-energy solar radiation, particularly ultraviolet and X-ray radiation. Despite the high temperatures, the air molecules in the thermosphere are so spread out that they cannot transfer their heat effectively, leading to the perception of extreme heat without much actual warmth.
The stratosphere is the layer of the atmosphere that is relatively calm and has stable temperatures. This layer is above the troposphere and contains the ozone layer, which helps trap heat in the atmosphere. Temperatures in the stratosphere increase with altitude due to the absorption of ultraviolet radiation by the ozone layer.
The layer of the Sun's atmosphere that can normally be seen is the photosphere. This is the visible surface of the Sun that emits light and heat and is responsible for the majority of the sunlight we receive on Earth.
The layer of the atmosphere that can reach temperatures up to 1800 degrees Celsius is the thermosphere. In this layer, temperatures increase significantly with altitude due to the absorption of high-energy solar radiation. Although the thermosphere can reach such extreme temperatures, it would not feel hot to a human because the air is so thin that there are not enough air molecules to transfer heat effectively.
The thermosphere is the warmest layer of the atmosphere primarily due to its absorption of high-energy solar radiation, particularly ultraviolet (UV) and X-ray radiation. This energy excites the sparse gas molecules present in this layer, leading to significantly higher temperatures, which can reach up to 2,500°C (4,500°F) or more. However, despite these high temperatures, the thermosphere would not feel hot to a human because of the extremely low density of the air, meaning there are very few molecules to transfer heat.
The thermosphere is the hottest layer of the Earth's atmosphere because it absorbs high-energy solar radiation, particularly ultraviolet and X-ray radiation. Despite the high temperatures, the air molecules in the thermosphere are so spread out that they cannot transfer their heat effectively, leading to the perception of extreme heat without much actual warmth.
One way that heat energy is spread through the atmosphere is through radiation. Conduction and convection are two other ways that heat energy is spread through the atmosphere.
The three molecules that trap heat in the atmosphere are carbon dioxide, methane, and water vapor.
The heat on Earth is contributing to the depletion of the ozone layer. Greenhouse gases emitted from human activities trap heat in the Earth's atmosphere, leading to global warming. This warming can affect the stability of the ozone layer, causing ozone molecules to break down more easily and thinning the ozone layer.
The uppermost layer of the atmosphere is the thermosphere. It feels cold because even though there are few gas molecules present to transfer heat, the few molecules that are present can have very high energies due to high temperatures created by solar radiation. This means that even though the temperature is high, it may not feel hot due to the lack of molecules to transfer that heat.
Greenhouse gases don't reflect anything. They absorb energy from incoming sunlight and warm up. The warm gas molecules then share the heat with all other molecules in the atmosphere. Many people think there is a layer of greenhouse gas "up there" that reflects the heat back to Earth. This is not the case, The gases are mixed all through the atmosphere, not concentrated in a layer.
The troposphere is the layer of the atmosphere that traps infrared heat radiation. It is responsible for the greenhouse effect, which helps regulate Earth's temperature by trapping heat.
The three molecules that trap heat in the atmosphere are carbon dioxide (CO2), methane (CH4), and water vapor (H2O).
An atmosphere is a gaseous layer round a planetary body, held there by the gravity of the said body. Atmospheres being fluids spread heat round planets from hot areas to cooler areas.
Conduction is the type of heat transfer that is most effective in the lowest 3mm of the atmosphere. Conduction involves the transfer of heat through direct contact between molecules, making it the dominant heat transfer mechanism in the thin boundary layer near the Earth's surface.
Conduction in the atmosphere happens when heat is transferred through direct contact between the surface of the Earth and the air above it. The warmer surface heats up the air molecules in contact with it, causing them to move faster and spread the heat to neighboring molecules. This process helps to balance temperature differences between the Earth's surface and the air.
Meteors burn up in the mesosphere as they encounter resistance from air molecules at high speeds, resulting in friction and heat that vaporize the meteoroid.