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      The far north is burning—and turning up the heat on the planet

      news.movim.eu / ArsTechnica · Wednesday, 10 May, 2023 - 14:21

    PIcture of forest with lots of dead trees

    Enlarge / Fire-damaged trees in a boreal forest near the Saskatchewan River in Alberta, Canada. As northern forests burn, they're releasing massive amounts of carbon. (credit: Ed Jones/Getty Images)

    The far north is both a massive carbon sink and a potent environmental time bomb . The region stores a huge amount of CO 2 in boreal forests and underlying soils. Organic peat soil , for instance, covers just 3 percent of the Earth’s land area (there’s some in tropical regions, too), yet it contains a third of its terrestrial carbon. And Arctic permafrost has locked away thousands of years’ worth of plant matter, preventing rot that would release clouds of planet-heating carbon dioxide and methane .

    But in a pair of recent papers, scientists have found that wildfires and human meddling are reducing northern ecosystems’ ability to sequester carbon, threatening to turn them into carbon sources . That will in turn accelerate climate change, which is already warming the Arctic four and a half times faster than the rest of the world, triggering the release of still more carbon—a gnarly feedback loop.

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      The Arctic Ocean may have gone fresh in ice age times

      Scott K. Johnson · news.movim.eu / ArsTechnica · Friday, 5 February, 2021 - 17:50

    The Arctic Ocean may have gone fresh in ice age times

    Enlarge (credit: Person-with-No Name )

    The Arctic Ocean is many things. Cold and icy come to mind, of course, but "salty" should as well—it’s an ocean, after all. Yet a new study suggests that during certain ice age periods, the Arctic Ocean and the adjacent Greenland and Norwegian Seas (you can guess where those are if you don’t know) were filled with freshwater.

    The paleo evidence for this idea is pretty subtle. The isotope thorium-230 is produced from the decay of uranium-234, which exists in seawater proportionally to its salinity. While the uranium dissolves in seawater, thorium tends to precipitate and fall to the seafloor. Bring up a core of seafloor sediment, then, and rising or falling concentrations of thorium-230 can tell you about rising or falling salinity in that region over time.

    A new study led by Walter Geibert at the Alfred Wegener Institute analyzed a pair of sediment cores taken from the bottom of the Arctic Ocean. In those cores, there are two time intervals during which thorium-230 fell to zero—one interval about 60,000 to 70,000 years ago and another about 130,000 to 150,000 years ago.

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