Future snowmelt from Third Pole may decrease drastically

The melting of seasonal snowpacks in Asia provides an even larger contribution to river streamflow. The water supply from snowmelt has changed considerably over the last 40 years and it will further diminish in the future under continued climate change, with potentially strong impacts on downstream water availability.

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Reduced microbial stability linked to soil carbon loss in active layer under alpine permafrost degradation

Links between microbial stability and soil carbon loss in the alpine permafrost uncovered

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