{"id":16670,"date":"2020-02-12T06:38:21","date_gmt":"2020-02-12T11:38:21","guid":{"rendered":"https:\/\/pierrejoris.com\/blog\/?p=16670"},"modified":"2020-02-12T06:38:21","modified_gmt":"2020-02-12T11:38:21","slug":"ancient-antarctic-ice-melt-increased-sea-levels-by-3-metres-and-it-could-happen-again","status":"publish","type":"post","link":"https:\/\/pierrejoris.com\/blog\/ancient-antarctic-ice-melt-increased-sea-levels-by-3-metres-and-it-could-happen-again\/","title":{"rendered":"Ancient Antarctic ice melt increased sea levels by 3+ metres \u2013 and it could happen again.\u00a0"},"content":{"rendered":"
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Via \u00a0\"UNSW<\/a> \u00a0Newsroom \u00a0<\/a>\u00a0& Potsdam-Institut: <\/span><\/h1>\n

\u00a012 FEB 2020<\/span><\/h1>\n<\/div>\n
SHERRY LANDOW<\/div>\n<\/div>\n
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Rising ocean temperatures drove the melting of Antarctic ice sheets and caused extreme sea level rise more than 100,000 years ago, a new international study led by UNSW Sydney shows.<\/p>\n<\/div>\n

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Fine layers of ancient volcanic ash in the ice helped the team pinpoint when the mass melting took place. Image: AntarcticScience.com<\/p>\n<\/div>\n<\/div>\n<\/div>\n

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Mass melting of the West Antarctic Ice Sheet was a major cause of high sea levels during a period known as the Last Interglacial (129,000-116,000 years ago), an international team of scientists led by UNSW\u2019s Chris Turney has found. The research was published today in Proceedings of the National Academy of Sciences (PNAS)<\/em><\/a>.<\/p>\n

The extreme ice loss caused a multi-metre rise in global mean sea levels \u2013 and it took less than 2\u02daC of ocean warming for it to occur.<\/p>\n

\u201cNot only did we lose a lot of the West Antarctic Ice Sheet, but this happened very early during the Last Interglacial,\u201d says Chris Turney, Professor in Earth and Climate Science at UNSW Sydney and lead author of the study.<\/p>\n

Fine layers of ancient volcanic ash in the ice helped the team pinpoint when the mass melting took place. Alarmingly, the results indicated that most ice loss occurred within the first millennia, showing how sensitive the Antarctic is to higher temperatures.<\/p>\n

\u201cThe melting was likely caused by less than 2\u00b0C ocean warming \u2013 and that’s something that has major implications for the future, given the ocean temperature increase and West Antarctic melting that\u2019s happening today,\u201d Professor Turney says.<\/p>\n

During the Last Interglacial, polar ocean temperatures were likely less than 2\u02daC warmer than today, making it a useful period to study how future global warming might affect ice dynamics and sea levels.<\/p>\n

\u201cThis study shows that we would lose most of the West Antarctic Ice Sheet in a warmer world,\u201d says Professor Turney.<\/p>\n

In contrast to the East Antarctic Ice Sheet \u2013 which mostly sits on high ground \u2013 the West Antarctic sheet rests on the seabed. It\u2019s fringed by large areas of floating ice, called ice shelves, that protect the central part of the sheet.<\/p>\n

As warmer ocean water travels into cavities beneath the ice shelves, ice melts from below, thinning the shelves and making the central ice sheet highly vulnerable to warming ocean temperatures.<\/p>\n

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Blue ice areas are created by fierce, high-density winds that remove the top layer of snow and erode the exposed ice. As the ice is removed, ancient ice flows up to the surface, offering an insight into the ice sheet’s history. Image: AntarcticScience.cm<\/p>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n

Going back in time<\/h3>\n

To undertake their research, Professor Turney and his team travelled to the Patriot Hills Blue Ice Area, a site located at the periphery of the West Antarctic Ice Sheet, with support from Antarctic Logistics and Expeditions (or ALE).<\/p>\n

Blue ice areas are the perfect laboratory for scientists due to their unique topography \u2013 they are created by fierce, high-density katabatic winds. When these winds blow over mountains, they remove the top layer of snow and erode the exposed ice. As the ice is removed, ancient ice flows up to the surface, offering an insight into the ice sheet\u2019s history.<\/p>\n

While most Antarctic researchers drill down into the ice core to extract their samples, this team used a different method \u2013 horizontal ice core analysis.<\/p>\n

\u201cInstead of drilling kilometres into the ice, we can simply walk across a blue ice area and travel back through millennia. By taking samples of ice from the surface we are able to reconstruct what happened to this precious environment in the past,\u201d Professor Turney says.<\/p>\n

Through isotope measurements, the team discovered a gap in the ice sheet record immediately prior to the Last Interglacial. This period of missing ice coincides with the extreme sea level increase, suggesting rapid ice loss from the West Antarctic Ice Sheet. The volcanic ash, trace gas samples and ancient DNA from bacteria trapped in the ice all support this finding.<\/p>\n

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Trace gas bubbles in the ice samples. Image: AntarcticScience.com<\/p>\n<\/div>\n<\/div>\n<\/div>\n<\/div>\n

Learning from the Last Interglacial<\/h3>\n

Ice age cycles occur approximately every 100,000 years due to subtle changes in Earth\u2019s orbit around the Sun. These ice ages are separated by warm interglacial periods. The Last Interglacial is the most recent warm period to our current interglacial period, the Holocene.<\/p>\n

While human contribution to global warming makes the Holocene unique, the Last Interglacial remains a useful research point to understand how the planet responds to extreme change.<\/p>\n

\u201cThe future is heading far beyond the range of anything we’ve seen observed in the scientific instrumental record of the last 150 years,\u201d says Professor Turney. \u201cWe have to look further into the past if we\u2019re going to manage future changes.\u201d<\/p>\n

During the Last Interglacial, global mean sea levels were between 6m and 9m higher than present day, although some scientists suspect this could have reached 11m.<\/p>\n

The sea level rise in the Last Interglacial can\u2019t be fully explained by the Greenland Ice Sheet melt, which accounted for a 2m increase, or ocean expansion from warmer temperatures and melting mountain glaciers, which are thought to have caused less than a 1m increase.<\/p>\n

\u201cWe now have some of the first major evidence that West Antarctica melted and drove a large part of this sea level rise,\u201d says Professor Turney.<\/p>\n

An urgent need to minimise future warming<\/h3>\n

The severity of the ice loss suggests that the West Antarctic Ice Sheet is highly sensitive to future ocean warming.<\/p>\n

\u201cThe West Antarctic Ice Sheet is sitting in water, and today this water is getting warmer and warmer,\u201d says Professor Turney, who is also a Chief Investigator of the ARC Centre of Excellence for Australian Biodiversity and Heritage (CABAH).<\/p>\n

Using data gained from their fieldwork, the team ran model simulations to investigate how warming might affect the floating ice shelves. These shelves currently buttress the ice sheets and help slow the flow of ice off the continent.<\/p>\n

The results suggest a 3.8m sea level rise during the first thousand years of a 2\u02daC warmer ocean. Most of the modelled sea level rise occurred after the loss of the ice shelves, which collapsed within the first two hundred years of higher temperatures.<\/p>\n

The researchers are concerned that persistent high sea surface temperatures would prompt the East Antarctic Ice Sheet to melt, driving global sea levels even higher.<\/p>\n

\u201cThe positive feedbacks between a warming ocean, ice shelf collapse, and ice sheet melt suggests that the West Antarctic may be vulnerable to passing a tipping point,\u201d stressed Dr Zo\u00eb Thomas, co-author and ARC Discovery Early Career Research Award (DECRA) Fellow at UNSW.<\/p>\n

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Professor Chris Turney drilling for ice in the Patriot Hills area. Image: AntarcticScience.com<\/p>\n<\/div>\n<\/div>\n<\/div>\n

\u201cAs it reaches the tipping point, only a small increase in temperature could trigger abrupt ice sheet melt and a multi-metre rise in global sea level.\u201d<\/p>\n

At present, the consensus of the Intergovernmental Panel on Climate Change (IPCC) 2013 report suggests that global sea level will rise between 40cm and 80cm over the next century, with Antarctica only contributing around 5cm of this.<\/p>\n

The researchers are concerned that Antarctica\u2019s contribution could be much greater than this.<\/p>\n

\u201cRecent projections suggest that the Antarctic contribution may be up to ten times higher than the IPCC forecast, which is deeply worrying,\u201d says Professor Christopher Fogwill, co-author and Director of The Institute for Sustainable Futures at the UK University of Keele.<\/p>\n

\u201cOur study highlights that the Antarctic Ice Sheet may lie close to a tipping point, which once passed may commit us to rapid sea level rise for millennia to come. This underlines the urgent need to reduce and control greenhouse gas emissions that are driving warming today.\u201d<\/p>\n

Notably, the researchers warn that this tipping point may be closer than we think.<\/p>\n

\u201cThe Paris Climate Agreement commits to restricting global warming to 2\u02daC, ideally 1.5\u02daC, this century,\u201d says Professor Turney.<\/p>\n

\u201cOur findings show that we don\u2019t want to get close to 2\u02daC warming.\u201d<\/p>\n

Professor Turney and his team hope to expand the research to confirm just how quickly the West Antarctic Ice Sheet responded to warming and which areas were first affected.<\/p>\n

\u201cWe only tested one location, so we don\u2019t know whether it was the first sector of Antarctica that melted, or whether it melted relatively late. How these changes in Antarctica impacted the rest of the world remains a huge unknown as the planet warms into the future\u201d he says.<\/p>\n

\u201cTesting other locations will give us a better idea for the areas we really need to monitor as the planet continues to warm.\u201d<\/p>\n<\/div>\n","protected":false},"excerpt":{"rendered":"

Via \u00a0 \u00a0Newsroom \u00a0\u00a0& Potsdam-Institut: \u00a012 FEB 2020 SHERRY LANDOW Rising ocean temperatures drove the melting of Antarctic ice sheets and caused extreme sea level rise more than 100,000 years ago, a new international...<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[],"class_list":["post-16670","post","type-post","status-publish","format-standard","hentry","category-uncategorized"],"_links":{"self":[{"href":"https:\/\/pierrejoris.com\/blog\/wp-json\/wp\/v2\/posts\/16670","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/pierrejoris.com\/blog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/pierrejoris.com\/blog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/pierrejoris.com\/blog\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/pierrejoris.com\/blog\/wp-json\/wp\/v2\/comments?post=16670"}],"version-history":[{"count":2,"href":"https:\/\/pierrejoris.com\/blog\/wp-json\/wp\/v2\/posts\/16670\/revisions"}],"predecessor-version":[{"id":16672,"href":"https:\/\/pierrejoris.com\/blog\/wp-json\/wp\/v2\/posts\/16670\/revisions\/16672"}],"wp:attachment":[{"href":"https:\/\/pierrejoris.com\/blog\/wp-json\/wp\/v2\/media?parent=16670"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/pierrejoris.com\/blog\/wp-json\/wp\/v2\/categories?post=16670"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/pierrejoris.com\/blog\/wp-json\/wp\/v2\/tags?post=16670"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}