Arctic sea ice can’t ‘bounce back’

University of Exeter [See my update at the end. -w.]

Quahog clams Credit: Paul Butler
Quahog clams Credit: Paul Butler

Arctic sea ice cannot “quickly bounce back” if climate change causes it to melt, new research suggests.

A team of scientists led by the University of Exeter used the shells of quahog clams, which can live for hundreds of years, and climate models to discover how Arctic sea ice has changed over the last 1,000 years.

They found sea ice coverage shifts over timescales of decades to centuries – so shrinking ice cannot be expected to return rapidly if climate change is slowed or reversed.

The study examined whether past ice changes north of Iceland were “forced” (caused by events such as volcanic eruptions and variations in the sun’s output) or “unforced” (part of a natural pattern).

At least a third of past variation was found to be “forced” – showing the climate system is “very sensitive” to such driving factors, according to lead author Dr Paul Halloran, of the University of Exeter.

“There is increasing evidence that many aspects of our changing climate aren’t caused by natural variation, but are instead ‘forced’ by certain events,” he said.

“Our study shows the large effect that climate drivers can have on Arctic sea ice, even when those drivers are weak as is the case with volcanic eruptions or solar changes.

“Today, the climate driver isn’t weak volcanic or solar changes – it’s human activity, and we are now massively forcing the system.”

Co-author of the study Professor Ian Hall, from Cardiff University, said: “Our results suggest that climate models are able to correctly reproduce the long-term pattern of sea ice change.

“This gives us increased confidence in what climate models are telling us about current and future sea ice loss.”

When there is lots of sea ice, some of this drifts southwards and, by releasing fresh water, can slow the North Atlantic Ocean circulation, otherwise known as the Atlantic Meridional Overturning Circulation (AMOC).

The AMOC brings warm water from the tropics towards the Arctic, so slowing it down cools this region and allows sea ice to grow further.

So, with less ice the AMOC can bring in more warm water – a so-called “positive feedback” where climate change drives further warming and sea ice loss.

Quahog clams are thought to be the longest-living non-colonial animal on Earth, and their shells produce growth rings which can be examined to measure past environmental changes.

Dr Halloran is part of the Global Systems Institute, which brings together experts from a wide range of fields to find solutions to global challenges.

The new study is part of a project including Cardiff University, the Met Office and an international team working on climate model simulations of the last millennium. The work was funded by the Natural Environment Research Council.

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The paper, published in the journal Scientific Reports, is entitled: “Natural drivers of multidecadal Arctic sea ice variability over the last millennium.”

From EurekAlert!

[UPDATE] I suspect Charles won’t complain if I add today’s situation …

Best to all,

w.

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DocSiders
January 23, 2020 9:26 am

What pray tell was the forcing that caused Arctic meltings?

January 23, 2020 12:56 pm

YA YA YA

And my freezer never refreezed after being cleaned.

DO’H !!

January 27, 2020 5:35 pm

“When there is lots of sea ice, some of this drifts southwards and, by releasing fresh water, can slow the North Atlantic Ocean circulation, otherwise known as the Atlantic Meridional Overturning Circulation (AMOC).
The AMOC brings warm water from the tropics towards the Arctic, so slowing it down cools this region and allows sea ice to grow further.
So, with less ice the AMOC can bring in more warm water – a so-called “positive feedback” where climate change drives further warming and sea ice loss.”

When the overturning (AMOC) slows, the warm water travels further into the far North Atlantic and Arctic, and reduces the sea ice. The low MOC events are associated with negative North Atlantic Oscillation episodes. The Gulf Stream does speed up marginally during the low MOC events, but the gross changes are to do with the overturning rate and not the Gulf Stream speed.

“Today, the climate driver isn’t weak volcanic or solar changes – it’s human activity, and we are now massively forcing the system.”

No it’s weaker solar wind conditions since the mid 1990’s driving a warm Atlantic Multidecadal Oscillation phase via negative North Atlantic Oscillation states. A negative feedback to low solar, and normal during each centennial solar minimum.

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Kiwi Gary
January 28, 2020 1:32 am

I wonder whether the researchers bothered to make enquiries of the Russian authorities who are building a new fleet of icebreakers, including 4 nuclear powered units with 3-metre ice thickness capability. But then, the Russians just live there. What would they know compared to professional school-kids on their computers many kilometres distant?

Johann Wundersamer
February 3, 2020 4:07 am

“Today, the climate driver isn’t weak volcanic or solar changes – it’s human activity, and we are now massively forcing the system.”

So why doesn’t Dr. Paul Halloran, of the University of Exeter, REVERSE “our” forcing – opening Red Sea via Suez Channel to Mediterranean and Golf of Mexico to Pacific via Panama Channel.

What too have we overwhelming done to “our” Planet. What’s he awaiting of “us”.

OTOH – long before man walked on Earth the Americas were separated, proto Mare-Nostra and pre Indian Ocean were connected by the Thetis.

– explaining please, Dr. Paul Halloran, of the University of Exeter.