UNESCO Central Asia glaciers: GEF infographics

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What is the cryosphere?

Changes in the cryosphere Change in precipitation from snow to rain

Degradation of mountain permafrost

Shift of snow and glaciers to higher elevations

Reduction in glacier area and volume

Cryosphere

Snow

Glacier The seasonal melting of the cryosphere contributes to peak flow in summer

Permafrost

-30%

Melting starts earlier and faster 1970

2020

The cryosphere in Central Asia Melt water from snow and glaciers runs hydropower turbines ... ... contributes to crop irrigation ...

Home to flagship species

Danger from glacial lakes, avalanches

... and the supply of drinking water

! Irrigation

Energy

Ecosystems

Cities

Water and the cryosphere Tien Shan

The Pamirs

1 800 km

2

15 500 km

2

Syr Darya

The future

Snow

More rain

Excessive water supply due to intense melting

Contribution of glacial melt water to upstream river flow

10%

Today

Lack of water supply in summer

40% Amu Darya

Project partners and funders

United Nations Global Environment Development Programme Facility

Participating countries

Kazakhstan

Kyrgyzstan

Tajikistan Turkmenistan Uzbekistan


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