News / Science News

    Scientists describe how 'upside-down rivers' of warm water break Antarctica's ice shelf

    Researchers from the University of Colorado at Boulder (CU Boulder) in Colorado and the College of Wooster in Ohio reported a new mechanism by which warm ocean currents erode the ice shelves along the coast of Antarctica, contributing to the planet's rising oceans.



    The edge of an ice shelf in Antarctica. Image: NASA/Jane Beitler


    "Warm water circulation is attacking the undersides of these ice shelves at their most vulnerable points," said study co-author Karen Alley. The Wooster professor added, "These effects matter [...] But exactly how much, we don't yet know. We need to."

    The researchers used satellite imagery to identify places where coastal ice sheets had melted, creating areas of open water called polynyas, which, they observed, occurred in the same places every year. From this, they concluded that warm water was reaching the ice sheets in the same places every year as well.

    Because warmer water is more buoyant, says the study, it rises above cooler water, creating what the scientists describe as an "upside-down river" flowing underneath the layers of ice. Ice shelves tend to weaken as they move, forming cracks and crevasses at their edges and stretch points.

    Warm water, being on top, tends to become even more likely to find these cracks, so increasing the ice mass' melt rate.

    Ice shelves are not actually part of the land mass with which they are associated. Rather, they float along the coast nearby. Because they can be prevented from drifting further away by high places in the ocean floor, they can in turn prevent land-associated ice masses from becoming detached.

    "Now we're seeing a new process, where warm water cuts into the shelf from below," said study co-author Ted Scambos of CU Boulder's Cooperative Institute for Research in Environmental Sciences (CIRES). "Like scoring a plate of glass, the trough renders the shelf weak, and in a few decades, it's gone, freeing the ice sheet to ride out faster into the ocean." (Wikinews)

    OCTOBER 14, 2019



    YOU MAY ALSO LIKE

    Materials so small they make nanomaterials look like behemoths.
    Scientists find that eastern U.S. forest complexity improves carbon capture.
    Hotter temperatures mean birds need more water to cool off -- if it's available.
    Scientists determining how today's corn plants will respond to future ozone levels.
    Researchers reported warming seas appear to decrease the efficacy of the chemical compounds that corals release into the water to defend themselves from bacteria and encroaching seaweed, but these losses may be mitigated if there are large numbers of hungry fish around.
    Iridium "loses its identity," and its electrons act oddly, in an ultra-thin film when interfaced with nickel-based layers.

    © 1991-2023 The Titi Tudorancea Bulletin | Titi Tudorancea® is a Registered Trademark | Terms of use and privacy policy
    Contact