Tag: hydrologic cycle

Acid rain is caused by a chemical reaction that begins when compounds like sulfur dioxide and nitrogen oxides are released into the air. These substances can rise very high into the atmosphere, where they mix and react with water, oxygen, and other chemicals to form more acidic pollutants, known as acid rain.

Precipitation is any type of water that forms in the Earth's atmosphere and then drops onto the surface of the Earth.

The rain that falls from clouds but freezes before it reaches the ground is called sleet or ice pellets.

Snow is precipitation that falls in the form of ice crystals

Hail  forms when very cold water droplets freeze, or turn solid, as soon as they touch things like dust or dirt

Water vapor in the atmosphere is visible as clouds and fog.

It forms mist. It is a phenomenon caused by the small water droplets of water suspended in the air. When the warm moist air meets the sudden cooling, mist is formed.

The process of changing of water from the liquid state to the gaseous state is called evaporation. It occurs every day in natural and man-made environments. It occurs most often around the areas which are situated near water bodies. It is the most important process in case of water cycle because the water from water bodies goes into atmosphere through the process of evaporation. The rate of evaporation increases with the increase in the temperature.

The amount of water vapor in the air is known as humidity. It can make hot temperatures even more unbearable than they already are. It affects both weather as well as climate. It also affects global climate change. Both low humidity as well as high humidity is harmful for us. Humidity is of two types:- Absolute humidity and Relative humidity.

Hail is a small ball of ice in the atmosphere, especially at night. It is a result of precipitation. It is produced by intense thunderstorms when snow and rain coexists. As the snowflakes fall, liquid water freezes onto them. It forms ice pellets that continue to grow as more droplets accumulate. When the ball of ice becomes so large and heavy, they fall as hailstones.

Cirrus, cumulus, and stratus are the types of cloud. Cirrus clouds are very thin and white in colour. They are formed of ice crystals and give a feathery appearance. They are the highest clouds. Cumulus clouds are generally dense and with sharp outlines, developing vertically in the form of rising mounds, domes or towers, of which the bulging upper parts often resemble a cauliflower. Stratus clouds resemble fog and made up of almost equal layers. Occasionally, they are broken into patches separated by blue sky by the incoming wind. Stratus clouds are grey in colour. 

The particles of condensed moisture held in suspension close to the surface of the earth are known as mist. They form at lower density as compared to fog. Their visibility is more than 1,000 meters. They are quicker to dissipate. They can rapidly disappear with even slight winds. Mist is what we see when we see our breath on a cold day.

An isohyet is a line on a map connecting points that receive the same amount of rainfall over a given period.

Water in atmosphere is recharged through hydrological cycle. In hydrological cycle, water is evaporated from the surface of the ocean. As moist air is lifted, it cools and clouds are formed by condensation of water vapors. These clouds transfer this water to ground through rains. Groundwater either seeps its way to into the oceans, rivers, and streams, or is released back into the atmosphere through transpiration. This cycle keeps repeating itself to keep balance of water.