The Times Australia

The Times

World

Weakening or collapse of a major Atlantic current has disrupted NZ’s climate in the past – and could do so again

  • Written by Shaun Eaves, Senior Lecturer in Physical Geography, Te Herenga Waka — Victoria University of Wellington
Weakening or collapse of a major Atlantic current has disrupted NZ’s climate in the past – and could do so again

Recent assessments[1] suggest the ocean current known as Atlantic Meridional Overturning Circulation (AMOC[2]) is slowing down, with collapse a real possibility[3] this century.

The AMOC is a globally important current[4] in the Atlantic Ocean, where surface water moves northward as part of the Gulf Stream and transports warm water towards the Arctic. There it cools and sinks to return southward as a deep ocean current.

Map of sea surface temperatures in the North Atlantic with a schematic diagram of ocean currents.
The Atlantic meridional overturning current (AMOC) transfers heat to the North Atlantic. Recent trends indicate this current may be slowing. Ruijian Gou, CC BY-ND[5]

Collapse of the AMOC would have a devastating effect on climate in Europe. Temperatures in the UK and Scandinavia could drop by 5–15°C in a matter of decades[6].

However, because Earth’s climate system is interconnected, these impacts could have a global reach. Our new research[7] shows past changes in AMOC have had significant impact on temperatures in New Zealand and across the southern hemisphere. These results imply that future collapse of AMOC may accelerate ongoing warming trends.

Lessons from the past

Between 20,000 and 10,000 years ago, Earth transitioned from peak ice-age conditions to a climate more like today’s. This interval featured rising global temperatures, melting ice sheets and climbing sea levels – all phenomena associated with present-day climate change.

Evidence from ice cores in Greenland and marine sediments in the North Atlantic suggests this natural warming event featured several abrupt changes associated with AMOC variability[8].

Using this interval as a natural experiment, we have undertaken research to learn more about how AMOC variability can affect climate in New Zealand.

Two merged photographs show a glacial basin and people among snow-covered rocks.
Evidence preserved in the landscape shows cooling and glacier growth in New Zealand coincided with a strengthening AMOC 14,500 years ago. Huw Horgan, Shaun Eaves, CC BY-ND[9]

To reconstruct how air temperature changed in New Zealand, we examined the past extent of mountain glaciers[10] using evidence preserved in the landscape. Glaciers grow and shrink primarily in response to changing air temperature, which affects the annual balance of snowfall and snow or ice melt. As glaciers change in size, they deposit moraines (rock debris) in the landscape, which can persist for tens of thousands of years.

A female scientist wearing a hard hat inspects mud layers in a sediment core.
The analysis of microfossils in marine sediment cores allows scientists to reconstruct past changes in sea-surface temperature. Jenni Hopkins, CC BY-ND[11]

We combined these land-based observations with reconstructions of sea-surface temperature in the Tasman Sea, which we derived from microfossils (smaller than one millimetre in size) known as foraminifera. These microfossils come in a wide range of species and each has a preferred water temperature.

We quantified changes in foraminifera species in a core of marine sediment to trace how local temperature in the Tasman Sea has varied through time.

Global climate connections

Our results show that changes in air and sea-surface temperature followed a similar pattern in the New Zealand region as Earth warmed following the last ice age.

Warming began in both air and sea at about 18,000 years ago, followed by a cooling event at about 14,500 years ago – the Antarctic Cold Reversal. The timing of these changes matches past changes in the AMOC, as recorded in geological climate records[12] from the North Atlantic region.

We examined computer simulations to test the physical connection between changes in the AMOC and New Zealand’s climate. These simulations used a physics-based climate model[13] that captures atmospheric and ocean circulation and their interaction.

Outputs from climate models show southern hemisphere temperature changes due to AMOC variability.
Climate model experiments show the impact of past AMOC variability on surface temperature in the Southern Hemisphere. Shaun Eaves, CC BY-ND[14]

The model simulations support our geological evidence, showing air and sea surface temperatures in New Zealand respond sensitively to changes in AMOC intensity. When the AMOC weakens and Europe cools, New Zealand and the southern mid-latitudes undergo warming, and vice versa.

The models also indicate changes in the AMOC are transported rapidly, within decades, to New Zealand via shifting global wind systems. Changes in the AMOC disrupt the temperature gradient between the hemispheres, which is a key control on the strength of westerly wind belts in the southern hemisphere, between the latitudes of 40°S and 60°S where New Zealand is.

The westerly winds are important for New Zealand’s climate[15]. They control the path of atmospheric storms and regional ocean currents.

Stronger winds over New Zealand bring regional cooling, as more storms track over the country and warm ocean currents are diverted away from the Tasman Sea into the south Pacific. In contrast, when the AMOC weakens, New Zealand has clearer skies and the Tasman Sea receives more tropical water masses, causing regional warming.

Future implications

Scientists have identified several “tipping points[16]” in Earth’s climate system that may be triggered by human-caused climate change. Once these thresholds are crossed, the consequences cannot be easily undone.

Climbing greenhouse gas concentrations have raised air temperatures in New Zealand, and globally, by about 1.1°C since the late 19th century[17]. Projections suggest New Zealand may end this century 1°C to 3°C warmer than now[18]. However, these estimates do not include the potential impacts of a future AMOC collapse.

Our insights from the recent geological past show this AMOC tipping point has global reach, and could accelerate future warming in New Zealand.

References

  1. ^ assessments (www.nature.com)
  2. ^ AMOC (en.wikipedia.org)
  3. ^ collapse a real possibility (doi.org)
  4. ^ globally important current (tos.org)
  5. ^ CC BY-ND (creativecommons.org)
  6. ^ could drop by 5–15°C in a matter of decades (www.science.org)
  7. ^ new research (doi.org)
  8. ^ several abrupt changes associated with AMOC variability (www.pik-potsdam.de)
  9. ^ CC BY-ND (creativecommons.org)
  10. ^ past extent of mountain glaciers (doi.org)
  11. ^ CC BY-ND (creativecommons.org)
  12. ^ recorded in geological climate records (doi.org)
  13. ^ physics-based climate model (en.wikipedia.org)
  14. ^ CC BY-ND (creativecommons.org)
  15. ^ important for New Zealand’s climate (niwa.co.nz)
  16. ^ tipping points (global-tipping-points.org)
  17. ^ by about 1.1°C since the late 19th century (niwa.co.nz)
  18. ^ 1°C to 3°C warmer than now (environment.govt.nz)

Read more https://theconversation.com/weakening-or-collapse-of-a-major-atlantic-current-has-disrupted-nzs-climate-in-the-past-and-could-do-so-again-231266

Business Marketing

Popular

Launch Your Venture: 5 Tips for Securing Small Business Funding

Funding is crucial for entrepreneurs looking to launch an ambitious business venture or grow an existing one. However, the process of finding sources, writing grant applications, and pitching to investors...

Volodymyr Nosov explained why WhiteBIT exchange has launched the token and how users will benefit from it

Volodymyr Nosov, CEO of cryptocurrency exchange WhiteBIT Digital technology, blockchain in particular, is gradually becoming a familiar part of everyday life for people all over the world. They are the...

Energy-efficient Roof Colors For Autumn

The autumn season is well-known for its colours, so it’s just natural to turn our heads and focus on home maintenance at this time. While many of us think about...