{"id":534,"date":"2016-08-16T00:00:00","date_gmt":"2016-08-15T22:00:00","guid":{"rendered":"https:\/\/site.uit.no\/cage\/2016\/08\/16\/sea-ice-strongly-linked-to-climate-change-in-past-90-000-years\/"},"modified":"2023-04-04T10:33:29","modified_gmt":"2023-04-04T08:33:29","slug":"sea-ice-strongly-linked-to-climate-change-in-past-90-000-years","status":"publish","type":"post","link":"https:\/\/site.uit.no\/cage\/2016\/08\/16\/sea-ice-strongly-linked-to-climate-change-in-past-90-000-years\/","title":{"rendered":"Sea ice strongly linked to climate change in past 90 000 years"},"content":{"rendered":"

Expansion and retreat of sea ice varied consistently in pace with rapid climate changes through past 90,000 years, a new study in Nature Communications shows.<\/h4>\n

Text: Maja Sojtaric<\/h6>\n

<\/p>\n

\u201cThe Arctic sea ice responded very rapidly to past climate changes. During the coldest periods of the past 90,000 years the sea ice edge spread relatively quickly to the Greenland-Scotland Ridge, and probably far into the Atlantic Ocean.\u201c says Ulrike Hoff, a researcher at Centre for Arctic Gas Hydrate, Environment and Climate (CAGE) and the first author of the Nature Communications study<\/a>.<\/p>\n

Sea ice amplifies the climate changes that are occurring at any given time. Its growth and melting has profound effects on climate, the marine environment and ocean circulation.
\n
\nTiny pieces that complete the big picture<\/strong><\/p>\n

\"Diatoms
The single celled algae, diatoms, can be seen using Scanning Electron Microscopy. It can take up to a year to clean a sample enough to be able to take a picture like this. Photo: Ulrike Hoff (colours added)<\/figcaption><\/figure>\n

Hoff and colleagues studied the past distribution of sea ice, in the longest existing sea ice record in a marine sediment core. The core was retrieved from the Nordic Seas, from the water depth of 1200m just off the Faroe Islands. It represents 90,000 years of sediment layers, and it is by studying those layers that scientist can reveal the changes in sea ice and past climate.<\/p>\n

It was the tiniest of evidence in these layers that brought this strong confirmation of sea ice behavior to light. They are a type of phytoplankton, called diatoms<\/a>, and they are everywhere around you. Diatoms are single celled algae with a cell wall made up of silica.<\/p>\n

\u201cThey are the golden brown coating in the glass of a street lamp, and shiny stuff in your make-up. They are even used in tooth paste as a cleaning agent,\u201d says Hoff.<\/p>\n

\u201cDiatoms are truly amazing, and can be preserved in marine and lake sediments for millions of years. I have personally examined diatom fossils that are 65 million of years old, and they look much the same as the diatoms that we find living today\u201d<\/p>\n

Possible to determine ice thickness<\/strong><\/p>\n

Not only could Hoff and colleagues assert whether the Nordic seas were covered in sea ice by studying the diatoms, they could also estimate how thick the ice cover was and whether it was seasonal or perennial.<\/p>\n

\"Diatoms
Diatoms have valves that easily dissolve in salty ocean water. But they leave traces of molecules in the sediments that scientists can look for to determine how the populations of algae developed in the past. Photo: Ulrike Hoff (Color added)<\/figcaption><\/figure>\n

 <\/p>\n

Sea ice retreated abruptly during warming events; spread rapidly during cooling phases, and became near perennial and perennial during cold periods and Heinrich events, the study states . (Scroll to\u00a0Background.)<\/p>\n

A few specific species of diatoms use sea ice as habitat; they are attached to the ice itself. If you dive under the ice you can see them as a golden brown coating underneath. But being algae, they depend on the suns rays that penetrate through the ice for photosynthesis. If the ice is too thick, the sun does not reach them, and the production falls rapidly as a result.<\/p>\n

\u201cBy classifying the diatoms in particular sections of the core, and counting them, we could calculate their abundances and estimate the ice thickness. Doing this, one has to keep in mind that as soon as they die, diatoms are quite frail in the salty water. The ocean is quick to reclaim the silica of their valves – and they dissolve. \u201c<\/p>\n

However, as they fall to the bottom of the ocean, they release a very specific lipid called IP25<\/sub> – Ice Proxy with 25 carbon atoms. It is a molecule that does not dissolve as easily in seawater. By testing the core for this lipid, the scientists could determine if a certain diatom population was present in the ocean and how well developed that population was.<\/p>\n

The analyses were conducted by the co-authors Ruediger Stein and Kirsten Fahl from Alfred Wegener Institute, Bremerhaven, Germany.<\/p>\n

First strong evidence<\/strong><\/p>\n

\u201c We have for the first time a strong and detailed evidence of sea ice distribution in the Nordic seas, because of the presence of IP25. <\/sub>Our previous studies from this site, and other sites in the Nordic seas and North Atlantic Ocean, have only been able to infer about presence of sea ice.\u201d states Tine Rasmussen, co-author of the study and professor at CAGE.<\/p>\n

\"Thermohaline_Circulation_2\"
Ocean water is transported around the globe by currents. Blue paths represent deep-water currents of colder and denser ocean water, while red paths represent surface currents of warmer, less dense water. The deep water forms in cold areas of the planet. Illustration: NASA<\/figcaption><\/figure>\n

Rasmussen points out that the sea ice profoundly influences the behavior of ocean currents<\/a>, which in turn influence air temperature.<\/p>\n

For example permanent sea ice cover is not good for deep-water formation, a process that essentially powers what is colloquially known as The Gulf Stream.<\/p>\n

\u201cUnderstanding the influence of sea ice on climate changes<\/a> and ocean currents of the past, helps us understand future development in the ever warming climate.\u201d Rasmussen says.<\/p>\n

 <\/p>\n

Citation: Hoff, U. Rasmussen T.L., Stein, R., Ezat M.M. and Fahl, K. (2016)\u00a0Sea ice and millennial-scale climate variability in the Nordic seas 90 kyr ago to present, Nature Communications 7, Article number: 12247 doi:10.1038\/ncomms12247<\/strong><\/p>\n

\"Fakta_NAT<\/p>\n

 <\/p>\n","protected":false},"excerpt":{"rendered":"

Expansion and retreat of sea ice varied consistently in pace with rapid climate changes through … <\/p>\n

Read more \u00abSea ice strongly linked to climate change in past 90 000 years\u00bb<\/span><\/a><\/p>\n","protected":false},"author":123546,"featured_media":539,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[9],"tags":[],"class_list":["post-534","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-news"],"acf":[],"yoast_head":"\nSea ice strongly linked to climate change in past 90 000 years - CAGE, Centre for Arctic Gas Hydrate, Environment and Climate<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/site.uit.no\/cage\/2016\/08\/16\/sea-ice-strongly-linked-to-climate-change-in-past-90-000-years\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Sea ice strongly linked to climate change in past 90 000 years - 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