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Climate change can cause alpine meadows to disappear in coming decades: Study

A study has revealed that climate change is having a more profound effect on alpine vegetation than expected.

Climate change can cause alpine meadows to disappear in coming decades: Study

A new study of changing mountain vegetation has suggested that some alpine meadows could disappear within the next few decades as a result of climate change.

The first ever pan-European study carried out by an international group of researchers revealed that climate change is having a more profound effect on alpine vegetation than expected.

Led by researchers from the Austrian Academy of Sciences and the University of Vienna, biologists from 13 different countries in Europe analysed 867 vegetation samples from 60 different summits sited in all major European mountain systems, first in 2001 and then again just seven years later in 2008.

They found strong indications that, at a continental scale, cold-loving plants traditionally found in alpine regions are being pushed out of many habitats by warm-loving plants.

“We expected to find a greater number of warm-loving plants at higher altitudes, but we did not expect to find such a significant change in such a short space of time,” said Michael Gottfried from the Global Observation Research Initiative in Alpine Environments (GLORIA) programme, which coordinated the study.

“Many cold-loving species are literally running out of mountain. In some of the lower mountains in Europe, we could see alpine meadows disappearing and dwarf shrubs taking over within the next few decades,” he warned.

The study, which is the largest and most comprehensive of its kind in the world, confirmed that there is a direct link between growing summer temperature and the shift in alpine plant composition.

“While regional studies have previously made this link, this is the first time it has been shown on a continental scale,” said Gottfried.

This phenomenon, which the GLORIA researchers have called thermophilization, has now been measured and quantified for the first time and is expressed by the researchers as a thermophilization indicator (D).

The study has been published in Nature Climate Change.

 

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