Precipitation
Continuous condensation in the atmosphere leads to the growth of condensed particles, which eventually become too heavy to remain suspended in the air and fall to the Earth’s surface. This process is known as precipitation. Precipitation can occur in the form of liquid or solid particles. Rainfall refers to precipitation in the form of liquid water, while snowfall occurs when temperatures are below freezing, causing water vapor to crystallize into hexagonal snowflakes.
In addition to rain and snow, other forms of precipitation include sleet and hail, although these are less common and occur sporadically. Sleet occurs when raindrops freeze into small pellets of ice as they pass through a subfreezing layer of air near the ground. Hailstones, on the other hand, form when raindrops are carried upward into colder atmospheric layers, causing them to freeze and accumulate layers of ice. Hailstones can have multiple concentric layers of ice, resulting in their characteristic rounded shape.
Water in the Atmosphere| Class 11 Geography Notes
Water in the Atmosphere is a major part of our climate system. Water is present in our atmosphere in three forms gaseous, liquid, and solid. In the circulation process of water in the atmosphere, evaporation is really important. It is a process where water changes its form from liquid state to vapor and moves to the Earth’s surface into the atmosphere.
In this article, we are going to discuss the Water in the Atmosphere in detail.
Water in the Atmosphere| Class 11 Geography Notes