A drop of water can take a variety of paths. Some of it evaporates and returns to the atmosphere, while other parts sink into the earth and become groundwater or soil moisture, and still other parts run off into rivers and streams. Nearly all of the water eventually drains into oceans or other aquatic bodies, where the cycle repeats.
According to studies, over 90% of the moisture in our atmosphere comes from the evaporation of oceans, seas, and other bodies of water , which is the process by which water transforms from a liquid to a gas. Plants release the majority of the remaining 10% that is found in the atmosphere through transpiration. Water is absorbed by plants through their roots, and it is then expelled through tiny pores on the underside of their leaves.
In addition, a tiny amount of water vapour is released into the atmosphere as a result of infiltration, which is the direct transformation of water from a solid (ice or snow) to a gas. When the temperature remains below freezing, infiltration causes snow banks to gradually diminish.
Together, evaporation, transpiration, infiltration, and volcanic emissions account for almost all of the atmospheric water vapour that isn't introduced by human activity. While the hydrologic cycle's surface-to-atmosphere component is mostly driven by ocean evaporation, transpiration also plays a significant role.
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