As temperature increases, the kinetic energy of water molecules also increases. This causes them to move faster and escape the surface of the water, leading to a higher rate of evaporation.
Hot water has a higher temperature, which means its molecules have more energy and are able to break free from the surface and evaporate at a faster rate than cold water molecules.
The larger the surface area of water, the more molecules are exposed to the air and can escape as vapor. This means that water in a wide and shallow container will evaporate faster than water in a tall and narrow container.
Other factors that can affect the rate of evaporation include humidity, air flow, and air pressure. Higher humidity can slow down evaporation as there is already a lot of water vapor in the air, while low humidity can speed up evaporation. Air flow can carry away water vapor, also increasing the rate of evaporation. Changes in air pressure can also affect the rate of evaporation.
Evaporation is a key part of the water cycle, where water from bodies of water, plants, and the ground evaporates into the air as water vapor. This water vapor then condenses to form clouds, which eventually lead to precipitation and the replenishment of bodies of water. This cycle ensures a continuous supply of water on Earth.