Hint: Water, a substance made of the compound components hydrogen and oxygen, exists in vaporous, fluid, and solid states. It is one of the most widely found and fundamental mixes. A tasteless and scentless fluid at room temperature, it has the significant capacity to break down numerous different substances. Water in its vapor form is a greenhouse gas found in the earth’s atmosphere.
Water Vapor is known as a variable gas which implies, the percentage of water vapor in the atmosphere is not fixed. This variety results because of impacts from temperature, elevation, and accessibility of water to dissipate into the air. As temperature builds, at that point an expanding measure of fluid or strong water can disintegrate into the air. This is restricted however by the accessibility of water to evaporate. The hottest places on earth could have a lot of dampness noticeable all around relying upon accessibility. Hot temperatures and warm sea waters are the best blends for high measures of dampness. Indeed, even in these areas, the greatest measure of water vapor as a level of the air is a couple of percents. The measure of water vapor in the air will in general diminish with height. This is because temperatures decline with altitude and the accessibility of a moisture source is farther away.
Note: Water is continually cycling through the environment. Water evaporates from the Earth's surface and ascends on warm updrafts into the climate. It condenses into mists, is passed up the breeze, and afterward falls back to the Earth as a downpour or snow. This cycle is one significant way that warmth and energy are moved from the outside of the Earth to the air and moved to start with one spot then onto the next on our planet.