hydrological cycle | water cycle| Rain water cycle an overview

What is Hydrology?

Hydrology is the science that deals with the occurrence, distribution, and disposal of water on Earth, encompassing various phases of the hydrologic cycle.

What is the Hydrologic Cycle?

The hydrologic cycle is a continuous water transfer cycle in nature with three main phases:

  • Evaporation and evapotranspiration
  • Precipitation
  • Runoff

Phases of the Hydrologic Cycle

  • Evaporation and Evapotranspiration: Water evaporates from ponds, lakes, reservoirs, and oceans, and transpiration occurs from vegetation. These vapors rise to the sky, condense, and form clouds, leading to precipitation.
  • Precipitation: When an air mass cools to the dew point temperature with seeding agents present, condensation occurs, forming raindrops that fall as rain, sleet, or snow. Precipitation is unevenly distributed across the Earth.
  • Runoff: Part of the precipitation flows over the land as runoff, part infiltrates the soil, replenishes the groundwater table, and eventually returns to water bodies. Surface runoff is stored in reservoirs for various uses.

Why is Runoff Important?

Runoff is crucial for civil engineers as it involves storing surface runoff in tanks and reservoirs for irrigation, municipal water supply, hydroelectric power, and other uses.

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What is Infiltration?

Infiltration is the process by which water reaching the ground surface enters the soil. The infiltration rate, measured in mm per hour, is governed by gravity and capillary action.

What Factors Influence Infiltration?

  • Soil Texture and Structure: Coarse soils encourage high infiltration.
  • Vegetation Type and Cover: Vegetation creates more porous soil, promoting infiltration.
  • Soil Moisture: Dry soil encourages high infiltration, but infiltration decreases with increasing soil moisture until it stabilizes.
  • Topsoil Layer: Porous topsoil due to insects and burrowing animals enhances infiltration.
  • Agricultural Practices: Soil compaction from farming reduces infiltration.

What is Evaporation?

Evaporation is the process where water turns into vapor due to solar heating. The rate of evaporation depends on water temperature, air temperature, humidity, and wind.

How is Evaporation Measured?

Evaporation is measured using a pan with an initial water depth of 20 cm. Daily measurements are taken to determine the volume of water needed to maintain the level, accounting for rainfall during the same period.

What is Runoff?

Runoff is the total amount of water flowing in a stream, consisting of several components:

  • Overland Flow: Water flowing as a thin sheet across the surface.
  • Interflow: Horizontal movement of infiltrating water.
  • Base Flow: Groundwater flow into the stream.
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Hydrology deals with the occurrence, distribution, and disposal of water on Earth through the hydrologic cycle, which includes phases like evaporation, precipitation, and runoff. The water cycle is crucial for understanding how freshwater is distributed and stored, affecting climate change and water resources. Infiltration and evapotranspiration are essential processes within this cycle. The importance of water on Earth and the impact of climate change on water resources underscore the need for comprehensive study and management. Runoff water cycle examples illustrate the practical applications, such as in municipal water supply and hydroelectric power.

hydrological cycle | water cycle| Rain water cycle an overview
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