Extreme weather turns arctic BRUN – and this could accelerate climate change



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In recent years, Arctic scientists have made a startling discovery: vast areas of the Arctic are turning brown.

This is partly due to extreme events related to winter conditions, such as brief and short periods of heat.

These events occur when the climate warms up, which occurs twice as fast in the Arctic than in the rest of the planet.

Dead and brown vegetation on a heath in Norway. A Sheffield researcher warned that browning was occurring at an alarming rate, with increasingly severe effects, causing widespread deaths and damage to the planets.

Dead and brown vegetation on a heath in Norway. A Sheffield researcher warned that browning was occurring at an alarming rate, with increasingly severe effects, causing widespread deaths and damage to the planets.

Dead and brown vegetation on a heath in Norway. A Sheffield researcher warned that browning was occurring at an alarming rate, with increasingly severe effects, causing widespread deaths and damage to the planets.

THE TWO KILLERS OF THE ARCTIC THAW

"Frost drought" occurs when the layer of insulating snow, which usually protects plants against the harsh Arctic winter, is melted, usually due to unusually high winter temperatures.

If the plants remain exposed long enough to cold and wind, they continually lose water and are unable to replace it with frozen soil.

Finally, they succumb to drought.

The second effect is "extreme winter warming" – a sudden explosion of high temperatures in winter that melts snow and forces evergreens to get ready for spring by losing their cold tolerance.

When the warm period is over, the return of cold temperatures usually kills the plant.

Extreme events therefore occur more and more often, with more and more serious effects, including extensive damage and the death of Arctic plants.

This "browning" of plant communities has occurred over thousands of square kilometers or more.

However, until recently, we knew very little what this could mean for the balance between carbon uptake and release in Arctic ecosystems.

Since the Arctic stores twice as much carbon as the atmosphere, it is an urgent concern.

Our study has now shown that extreme weather events can significantly reduce the ability of Arctic ecosystems to absorb carbon, which has implications for whether the Arctic will contribute to the fight against climate change or accelerate it. .

To understand the impact of extreme events on arctic moors, we visited the Lofoten Islands in northern Norway, where subarctic coastal plant communities act as an indicator of future climate change in the far north. showing the effects of warming in the region.

We have seen the effects of two extreme weather events in winter.

Firstly, the "frost drought" caused a severe dieback of the plants.

Frost dryness occurs when the layer of insulating snow that usually protects plants from the harsh Arctic winter is melted, usually because of unusually high winter temperatures.

If the plants remain exposed long enough to cold and wind, they continually lose water and are unable to replace it with frozen soil.

ICE MELTING CREATES A NEW DELIVERY ROAD IN THE ARCTIC

The Danish AP Moller-Maersk, the largest shipping group in the world, said that one of his cargo ships had managed to cross the Russian Arctic during a test trip unique because of the melting sea ice.

Palle Laursen, technical director of Maersk, said that "the trial has allowed us to gain outstanding operational experience".

Mr. Laursen added that the Venta Maersk and all embedded systems worked well in an unknown environment.

Melting Ice in the Central Arctic Stefan Hendricks / Alfred Wegener / PA)

Melting Ice in the Central Arctic Stefan Hendricks / Alfred Wegener / PA)

Melting Ice in the Central Arctic Stefan Hendricks / Alfred Wegener / PA)

The world's largest shipping company is experimenting with a "shortened" trade route through the Arctic, as global warming paves the way for the infamous Northeast Passage.

Laursen said the ship arrived in St. Petersburg Friday after leaving Russia's Pacific port city of Vladivostok on August 22.

The ship crossed the Bering Strait on 6 September.

The Northern Sea Route could be a shorter route for East Asian travel in Europe than the Northwest Passage over Canada, as it is likely to be cleared of ice sooner due to the climate change.

Finally, they succumb to drought.

The second event was "extreme winter warming" – a sudden explosion of high temperatures in the winter that melts snow and forces evergreens to get ready for spring by losing their cold tolerance.

When the warm period is over, the return of cold temperatures usually kills the plant.

In this case, however, we found something unexpected.

The heathland plants had survived this extreme warming event in winter, but showed signs of severe stress, visible in the form of a deep dark red color and persistent in the shoots and leaves.

A dark red pigmentation indicates that this plant is stressed by the unpredictable climate.

A dark red pigmentation indicates that this plant is stressed by the unpredictable climate.

A dark red pigmentation indicates that this plant is stressed by the unpredictable climate.

We measured the amount of carbon dioxide absorbed and released by plants in three types of vegetation: damaged heathland (where the dominant evergreen species had been killed by frost drought), stressed moors and healthy moors, and which had escaped the effects of vegetation. an extreme event.

This was done in three measurement periods throughout the growing season.

We found that these extreme winter conditions reduced the amount of carbon absorbed by heathland ecosystems by up to 50% throughout the growing season.

There is a considerable reduction in the ability of an extensive Arctic ecosystem to remove carbon from the atmosphere.

Surprisingly, this was the case both in the damaged moors, where much of the vegetation had been destroyed, and in the stressed moors.

Although the processes behind this change have been different in each type of heath, this clearly shows that we must take into account the role of plant stress in limiting carbon uptake by plants in order to fully appreciate the consequences of extreme weather events.

The more traditional Arctic tundra

The more traditional Arctic tundra

The more traditional Arctic tundra

What does this mean for the Arctic? We now know that extreme weather events could significantly reduce the ability of Arctic ecosystems to absorb carbon and combat climate change.

This is all the more worrying as the effects of browning strongly contrast with those of a better understanding of Arctic ecosystems to climate change: "greening in the Arctic" or the tendency of plants to become higher and more productive as the Arctic summers heat up.

Instruments for measuring the absorption and release of carbon at the test site.

Instruments for measuring the absorption and release of carbon at the test site.

Instruments for measuring the absorption and release of carbon at the test site.

At the present time, many climate models assume arbitrary levels of greening in the Arctic and therefore Arctic ecosystems will use more carbon in the future, which will slow down climate change.

The magnitude of browning observed in recent years, combined with the negative effects on carbon absorption reported here, suggests that the reality could be more complex, challenging our understanding of the role of the Arctic in the climate of the Earth.

What does this mean for us? The impact of extreme weather in the Arctic has global consequences.

It is clear that our current efforts to combat climate change are dangerously inadequate, but ambitious measures could now reduce the temperature predicted for global warming by 7 ° C.

This is essential to minimize the impacts of climate change in Arctic ecosystems and around the world.

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