I don't know what you mean by "warm the density of the air" but if you mean heat up the air in general, I guess not if it is directly a few inches below the surface, because the earth's core doesn't warm it, and the sun can't warm it.
The sun heats the surface of the Earth, and some of this heat goes into warming the air near the surface.
As air gets warmer, it expands and becomes less dense.
Where the air is over a parts of the Earth's Surface that is warm, the air warms. Warm air rises and as it rises it is replaced by cooler air that is sucked in from parts of the Earth's surface which are comparatively cooler. This movement causes a cyclic circulation of the air called win and weather.
When the sun warms the earth, the warmed earth emits infrared radiation. Some of this is captured by greenhouse gases in the atmosphere which then warms up. The more greenhouse gases there are, the warmer it gets. And that is how global warming works.
The atmosphere begins at the Earth's surface (or the ocean's), and extends upward. Generally air density decreases with altitude, although temperature differences can alter that somewhat.
The sun heats the surface of the Earth, and some of this heat goes into warming the air near the surface.
As air gets warmer, it expands and becomes less dense.
Air density is higher near the surface of the Earth. As you climb away from the surface, the pressure decreases.
When the act of the Earth's surface absorbing the sun's energy, it turns light into heat. The heat on the Earth's surface warms the air above it causing the air over the equator to get warmer than the surface air.
Sunlight comes in and warms the Earth's surface. It warms the gases in the air too, at least some of them with a How_is_earth's_atmosphere_similar_to_a_greenhousesize that gets excited by sunlight.
Heat ! The sun warms the air, which rises... Cold air flows into the 'void' to fill it - it's the movement of the air that creates the wind.
Where the air is over a parts of the Earth's Surface that is warm, the air warms. Warm air rises and as it rises it is replaced by cooler air that is sucked in from parts of the Earth's surface which are comparatively cooler. This movement causes a cyclic circulation of the air called win and weather.
Where the air is over a parts of the Earth's Surface that is warm, the air warms. Warm air rises and as it rises it is replaced by cooler air that is sucked in from parts of the Earth's surface which are comparatively cooler. This movement causes a cyclic circulation of the air called win and weather.
it changes
When the sun warms the earth, the warmed earth emits infrared radiation. Some of this is captured by greenhouse gases in the atmosphere which then warms up. The more greenhouse gases there are, the warmer it gets. And that is how global warming works.
The second way in which the sun influences earth's weather is through the water cycle. As the sun warms the Earth's surface, WATER EVAPORATES FROM THE OCEANS INTO THE AIR.
The atmosphere begins at the Earth's surface (or the ocean's), and extends upward. Generally air density decreases with altitude, although temperature differences can alter that somewhat.