Hydrology is formed by two words: "hydro" and "logy" meaning "water" and "science".
Hydrology is the scienceconcerned with the occurrence, distribution, movement and properties of all the waters of the Earth.
Hydrology is applied to major civil engineering projects such as
(I) designing and construction of hydraulic structures for flood control, (II) dam & hydroelectric power project
(III) water supply and drainage projects.
Scope of Hydrology
The maximumprobable flood
The water yield from a basin
The ground water development
The maximum intensity of storm and its frequency
Journey of water from the ocean to atmosphere and back to the earth and ultimately to the ocean through the processes of evaporation, precipitation, percolation, runoff called the hydrologic cycle.
The three fundamental processes of the hydrological cycle are
(a) evaporation and transpiration,
(b) precipitation
(c) runoff.
Evaporation is the physical process by water from freesurface and land areas vaporized into the atmosphere.
Precipitation is the product of the condensation of atmosphericwater vapor that falls under gravitational into the land & oceans, includes rain, snow and other forms of water.
Transpiration is the evaporation of water into the atmosphere from the leaves and stems of the living plants.
Interception is the precipitation that is caught by plantsurfaces and evaporates back to the atmosphere.
Evapotranspiration is the sum of interception, transpiration, and evaporation from soils and water bodies
Infiltration is the movement of water from the landsurface to the upperlayer of the soil.
Percolation is the movement of water from one soil zone to a lower soil zone.
Runoff is a part of precipitation which flows over groundsurface or appears in surface streams, rivers, or drains.
Ice caps and glaciers : 29,200 * 10^12 m3 > 2.14%
Atmosphere (water vapor) 13* 10^12 m3 >0.001
Oceans : 1,320,000* 10^12 m3 >97.3
R= 8.314J/mol.K
The water balance equation is given by In-Out = Delta(S) or P-Q-EV = Delta (S)
The residence time (Tr), is the average duration for a water molecule spend in a water body/reservoir
Residence Time (Tr) = Volume of the water/ Total flowrate