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Created By:
Civil-B Students
Jay S. Singhania (146490306107)
Vishvajit M. Shekhva
(146490306104)
Viren K. Trivedi (146490306115)
Pratik Sisodiya (146490306108)
Jaysinh Vala (146490306120)
Guided By:
Mr. K. H. Bhatt
Mr. M. B. Shrivastav
Mr. P. D. Gohil
Hydrological Cycle is the descriptive termapplied to the circulation of waterfrom
oceans to the atmosphere and back to the ground (precipitation).
In simple words, it is the earth’s water circulatory cycle.
This cycle starts fromthe evaporationof waterfromthe waterfilled bodies (oceans,
seas, lakes, ponds, etc).
The interesting fact is that themaximumamount of evaporation occurs fromthe
oceans and thus the smaller sources of waterfilled bodies like ponds, lakes, etcdon’t
empty up too early.
Also some of thewater gets evaporated fromtheporesof the vegetation due to the
sun’s heat whichis known as Transpiration.
Now, this water rises up in the atmosphere due to pressure difference.
And whenthis water rises tooup in the atmosphere, it condenses up due to the coldness
and forms the state of the clouds.
The cloudsare thus the condensedair forms which rise up in the air.
These clouds move withthe windand whenthese clouds are obstructeddue to and of the
reasons (like the high mountains, etc), they dropthe water as precipitation.
Now whenthis waterfalls on the earthsurface, some of the water getsabsorbed in
the groundand thus infiltrates deepin the ground and joins the sub-soil waterlevel
or groundwater level.
Now, the waterwhichdoes not getsabsorbed in the groundsurface, flows in the form
of the runoff.
Now this water, whichflows as runoff (inrivers), flows to the oceans and joins to the
ocean water.
Thus this cyclecontinues as evaporationto the precipitation.
Processes Involved In The Hydrological Cycle
 Evaporation and Transpiration
 Precipitation
 Runoff
Evaporation and Transpiration
 Due to heat of the sun, the water fromthe surfaces of the water
filledbodies (like oceans, seas, ponds, lakes etc) and moist water
surfaces evaporates. This is known as Evaporation.
 Now, when the moisture is lost fromthe surface of the vegetation,
due to the sun’s heat, it is known as transpiration
Precipitation
 The fall of the moisturefromtheatmosphere, in any formis knownas
the Precipitation.
Precipitatio
n
Liquid
Precipitation
Rainfall
Frozen
Precipitation
Snow Hail Sleet
Freezing
Rain
Runoff (R)
 Part of precipitationthat does not gets absorbed in the groundsurface and
also not get evaporatedflows on theearthsurface as runoff.

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The Hydrological Cycle

  • 1.
  • 2. Created By: Civil-B Students Jay S. Singhania (146490306107) Vishvajit M. Shekhva (146490306104) Viren K. Trivedi (146490306115) Pratik Sisodiya (146490306108) Jaysinh Vala (146490306120)
  • 3. Guided By: Mr. K. H. Bhatt Mr. M. B. Shrivastav Mr. P. D. Gohil
  • 4. Hydrological Cycle is the descriptive termapplied to the circulation of waterfrom oceans to the atmosphere and back to the ground (precipitation). In simple words, it is the earth’s water circulatory cycle.
  • 5. This cycle starts fromthe evaporationof waterfromthe waterfilled bodies (oceans, seas, lakes, ponds, etc). The interesting fact is that themaximumamount of evaporation occurs fromthe oceans and thus the smaller sources of waterfilled bodies like ponds, lakes, etcdon’t empty up too early. Also some of thewater gets evaporated fromtheporesof the vegetation due to the sun’s heat whichis known as Transpiration.
  • 6. Now, this water rises up in the atmosphere due to pressure difference. And whenthis water rises tooup in the atmosphere, it condenses up due to the coldness and forms the state of the clouds. The cloudsare thus the condensedair forms which rise up in the air. These clouds move withthe windand whenthese clouds are obstructeddue to and of the reasons (like the high mountains, etc), they dropthe water as precipitation.
  • 7. Now whenthis waterfalls on the earthsurface, some of the water getsabsorbed in the groundand thus infiltrates deepin the ground and joins the sub-soil waterlevel or groundwater level. Now, the waterwhichdoes not getsabsorbed in the groundsurface, flows in the form of the runoff.
  • 8. Now this water, whichflows as runoff (inrivers), flows to the oceans and joins to the ocean water. Thus this cyclecontinues as evaporationto the precipitation.
  • 9. Processes Involved In The Hydrological Cycle  Evaporation and Transpiration  Precipitation  Runoff
  • 10. Evaporation and Transpiration  Due to heat of the sun, the water fromthe surfaces of the water filledbodies (like oceans, seas, ponds, lakes etc) and moist water surfaces evaporates. This is known as Evaporation.  Now, when the moisture is lost fromthe surface of the vegetation, due to the sun’s heat, it is known as transpiration
  • 11. Precipitation  The fall of the moisturefromtheatmosphere, in any formis knownas the Precipitation. Precipitatio n Liquid Precipitation Rainfall Frozen Precipitation Snow Hail Sleet Freezing Rain
  • 12. Runoff (R)  Part of precipitationthat does not gets absorbed in the groundsurface and also not get evaporatedflows on theearthsurface as runoff.