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Quaternary paleoenvironments - results

Holocene - Andes


 

Fossil groundwater in the Andes

An example of the importance of knowing more about past climate change

The arid Andes between 18° and 30° South are located in the transition zone between the tropical and westerly circulation belts. This area is characterized by the extreme climate change of the last ice age, e.g. with a humid period during the late-glacial and Early Holocene time in a large part of the region. Today, precipitation rates are lower than 150-200 mm per year. Results from paleoclimatic research suggest that modern recharge of the water resources in this area is very limited, or even below the level of detection. The groundwater resources of today were formed when precipitation rates were two to three times greater than at present. Thus, water is renewed extremely slowly, or even non-renewable at present.
 

Precipitation rates in South America Groundwater reservoirs bearing the water of the past The South American Altiplano around 23°S. Exploitation of water ‚Äì a limited resource

1 - Chilean Altiplano (22-24°S), with mountains above 6000 m.
 

Use the diagrams above to answer the questions below.

1. Why might the water storage be quite limited on the Chilean Altiplano today?
show answer 1

2. What could certain stakeholders (mines, inhabitants of San Pedro, hotels) do to reduce the amount of groundwater needed?
show answer 2

3. How could the mines be obliged to use less water?
show answer 3

 

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29 August 2011
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