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Water Conflicts

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WATER CONFLICTS

Water Supply
Global water supplies are linked to three main physical factors: rivers, systems and geology.

Hydrological cycle

The hydrologic cycle begins with the evaporation of water from the surface of the ocean. As warm air is lifted, it cools and water vapour condenses to form clouds. Moisture is transported around the globe until it returns to the surface as precipitation. Once the water reaches the ground, one of two processes may occur:
1) some of the water may evaporate back into the atmosphere or
2) the water may penetrate the surface and become groundwater. Groundwater either seeps its way to into the oceans, rivers, and streams, or is released back into the atmosphere through transpiration. The balance of water that remains on the earth's surface is runoff, which empties into lakes, rivers and streams and is carried back to the oceans, where the cycle begins again.

CLIMATE
The climate is one of the physical factors that affect the global distribution of water.
Climates vary in different parts of the world. An example would be that countries closer to the equator tend to be either very dry and suffer from consistent droughts ( Kenya) or like Indonesia experience severe flooding.

RIVER SYSTEMS
Major rivers around the world store large quantities of water and transfer it across continents. The Amazon and Nile rivers are the worlds’ larges and discharge significant amounts of water from its catchment area into the world’s oceans.
However there can be considerable water loss by evaporation and climatic seasonal changes can also lead to variations in the discharge and produce distinctive river regimes.

GEOLOGY

Finite Resources: The world’s oceans s hold 97.5% of the global water store leaving on liy 2.5% of fresh water available. The water availability is finite. 80% of the oceans water is trapped in snow and permafrost and the remaining

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