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water is stored for later use in natural water
sources, such as Ocean atmosphere moisture
groundwater aquifers, soil water and natural
wetlands, and also small artificial ponds,
tanks and reservoirs behind major dams.
By – Amitabh kumar singh
TYPESOFWATERSTORAGE
Ocean water
Atmosphere moisture
Surface water
Distribution of Earth’s Water
96.5 %
3.5 %
Fig. no:-1http://www.cs.cmu.edu/afs/andrew/scs/cs/15-
463/f07/proj2/www/aaiordac/images/clouds.jpg
https://ij-
.
Where is all the water?
 96.5% in Oceans
 1.7 % in Ice
 .63% in groundwater
 .007% in salty lakes and streams
 .009% in fresh water lakes and streams
 .001% in the atmosphere
Surface water notes:
fresh water?
 68.7% in ice
 30.1% in groundwater
 .36% in freshwater lakes and streams
 .001% in the atmosphere
Wat er So urce Wat er Vol ume
(cu. m i.)
Wat er Vol ume
(cu. k m)
% of T otal Wat er
Oceans 321,000,000 1,338,000 ,000 96.5%
Total globa l wat er 332,500,000 1,386,000 ,000 --
Gleick, P. H., 199 6: Wate r reso ur ce s. In En cyclopedia of Climate and Wea th er , ed . by S. H. S chn eider, O xfo rd
Uni ve rsity Press, New York, vol. 2, pp. 817-82 3.
Storage of water in a
ocean in the form of salty
water which is not use
domestic purpose
Fig. no:-2.
http://www.cs.cmu.edu/afs/andrew/scs/cs/15-463/f07/proj2/www/aa/images/clouds.jpg
https://ij-
Storage in the atmosphere:
 0.001%
 Water vapor
 Clouds,
condensed
water vapor,
moisture in air
Fig. no:-3http://www.cs.cmu.edu/afs/andrew/scs/cs/15-463/f07/proj2/www/aaiordac/images/clouds.jpg
https://ij-
.
 is the water found underground in the
cracks and spaces in soil, sand and rock.
Fig. no:-4. Jump up to:a b c "Groundwater" (PDF). EPA.gov.
Fig. no:-5. Jumrp up to:a b c "Groundwater" (PDF). EPA.gov.
 Describes the amount ofwater
contained in thesoil.
 The amount of water that’s in the soil.
Fig. no:-6http://www.cs.cmu.edu/afs/andrew/scs/cs/15-463/f07/proj2/www/aaiordac/images/clouds.jpg
https://ij-
.
RIVER
Fig. no:-7 http://www.montereyinstitute.org/noaa/less
on07.html.
– water that
flows over land
into rivers
Stages of a Stream/River
Youthful – fastest time of erosion, almost
no tributaries
Mature – reduced erosion, wellestablished
tributaries, meanders, and
oxbow lakes
Meanders – winding of low-gradient streams
Oxbow lakes – lakes formed when meanders
are cut off
Old – deposits its sediments from a
decrease in slope, eventually becomes a
flat plain
 Glacial ice covers 11% of all land
 Represents a large % of all freshwater
 Mountain snowfields are “reservoirs” for
many water-supply systems
› 75% in Western States
How much of
all freshwater?
Fig. no:-8.
 Land area that is saturated withwater,
either permanently orseasonally.
Fig. no:-9 Jump up^ The Wetlands and Poverty Reduction Project, Wetlands International, 12-2005
.
 These can be defined as community-builtor
household waterstores.
 Filled by rainwater, groundwater infiltrationor
surface runoff.
Fig. no:-10
www/aaiordac/images/clouds.jpg
Fig. no:-11.
 A barrier constructed to hold back water and
raise its level, the resulting reservoir being
used in the generation of electricity or as a
water supply.
Fig. no:-12
www/aaiordac/images/clouds.jpg.
CONCLUSION
storage of fresh water on the earth is limited(or
very few amount of 3.5 %) and utilization of
fresh water increase day by day. but recharge
of ground and surface water decrease.
so my suggestion to all of my friend to reduce
the wasting of water
REFERANCE
http://www.cs.cmu.edu/afs/andrew/scs/cs/15-
463/f07/proj2/www/aaiordac/images/clouds.jpg
https://ij-
healthgeographics.biomedcentral.com/articles/10.1186/1476-072X-9-54
^ Jump up to:a b c "Groundwater" (PDF). EPA.gov.
Jump up^ Finding ways to boost productivity and reduce poverty through
better water management in Africa Success Stories, Issue 4, 2010, IWMI.
Jump up^ The Wetlands and Poverty Reduction Project, Wetlands
International, 12-2005
THANKS

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water storage ppt

  • 1. water is stored for later use in natural water sources, such as Ocean atmosphere moisture groundwater aquifers, soil water and natural wetlands, and also small artificial ponds, tanks and reservoirs behind major dams. By – Amitabh kumar singh
  • 3. Distribution of Earth’s Water 96.5 % 3.5 % Fig. no:-1http://www.cs.cmu.edu/afs/andrew/scs/cs/15- 463/f07/proj2/www/aaiordac/images/clouds.jpg https://ij- .
  • 4. Where is all the water?  96.5% in Oceans  1.7 % in Ice  .63% in groundwater  .007% in salty lakes and streams  .009% in fresh water lakes and streams  .001% in the atmosphere Surface water notes:
  • 5. fresh water?  68.7% in ice  30.1% in groundwater  .36% in freshwater lakes and streams  .001% in the atmosphere
  • 6. Wat er So urce Wat er Vol ume (cu. m i.) Wat er Vol ume (cu. k m) % of T otal Wat er Oceans 321,000,000 1,338,000 ,000 96.5% Total globa l wat er 332,500,000 1,386,000 ,000 -- Gleick, P. H., 199 6: Wate r reso ur ce s. In En cyclopedia of Climate and Wea th er , ed . by S. H. S chn eider, O xfo rd Uni ve rsity Press, New York, vol. 2, pp. 817-82 3. Storage of water in a ocean in the form of salty water which is not use domestic purpose Fig. no:-2. http://www.cs.cmu.edu/afs/andrew/scs/cs/15-463/f07/proj2/www/aa/images/clouds.jpg https://ij-
  • 7. Storage in the atmosphere:  0.001%  Water vapor  Clouds, condensed water vapor, moisture in air Fig. no:-3http://www.cs.cmu.edu/afs/andrew/scs/cs/15-463/f07/proj2/www/aaiordac/images/clouds.jpg https://ij- .
  • 8.  is the water found underground in the cracks and spaces in soil, sand and rock. Fig. no:-4. Jump up to:a b c "Groundwater" (PDF). EPA.gov.
  • 9. Fig. no:-5. Jumrp up to:a b c "Groundwater" (PDF). EPA.gov.
  • 10.  Describes the amount ofwater contained in thesoil.  The amount of water that’s in the soil. Fig. no:-6http://www.cs.cmu.edu/afs/andrew/scs/cs/15-463/f07/proj2/www/aaiordac/images/clouds.jpg https://ij- .
  • 12. Stages of a Stream/River Youthful – fastest time of erosion, almost no tributaries Mature – reduced erosion, wellestablished tributaries, meanders, and oxbow lakes Meanders – winding of low-gradient streams Oxbow lakes – lakes formed when meanders are cut off Old – deposits its sediments from a decrease in slope, eventually becomes a flat plain
  • 13.  Glacial ice covers 11% of all land  Represents a large % of all freshwater  Mountain snowfields are “reservoirs” for many water-supply systems › 75% in Western States How much of all freshwater? Fig. no:-8.
  • 14.  Land area that is saturated withwater, either permanently orseasonally. Fig. no:-9 Jump up^ The Wetlands and Poverty Reduction Project, Wetlands International, 12-2005 .
  • 15.  These can be defined as community-builtor household waterstores.  Filled by rainwater, groundwater infiltrationor surface runoff. Fig. no:-10 www/aaiordac/images/clouds.jpg Fig. no:-11.
  • 16.  A barrier constructed to hold back water and raise its level, the resulting reservoir being used in the generation of electricity or as a water supply. Fig. no:-12 www/aaiordac/images/clouds.jpg.
  • 17. CONCLUSION storage of fresh water on the earth is limited(or very few amount of 3.5 %) and utilization of fresh water increase day by day. but recharge of ground and surface water decrease. so my suggestion to all of my friend to reduce the wasting of water
  • 18. REFERANCE http://www.cs.cmu.edu/afs/andrew/scs/cs/15- 463/f07/proj2/www/aaiordac/images/clouds.jpg https://ij- healthgeographics.biomedcentral.com/articles/10.1186/1476-072X-9-54 ^ Jump up to:a b c "Groundwater" (PDF). EPA.gov. Jump up^ Finding ways to boost productivity and reduce poverty through better water management in Africa Success Stories, Issue 4, 2010, IWMI. Jump up^ The Wetlands and Poverty Reduction Project, Wetlands International, 12-2005

Notas del editor

  1. www/aaiordac/images/clouds.jpg