• A once-stable glacier in Greenland is no

    From ScienceDaily@1:317/3 to All on Wed Apr 19 22:31:44 2023
    A once-stable glacier in Greenland is now rapidly disappearing
    Study finds warming Atlantic waters threaten previously stable glaciers


    Date:
    April 19, 2023
    Source:
    Ohio State University
    Summary:
    As climate change causes ocean temperatures to rise, one of
    Greenland's previously most stable glaciers is now retreating at
    an unprecedented rate, according to a new study.


    Facebook Twitter Pinterest LinkedIN Email
    FULL STORY ==========================================================================
    As climate change causes ocean temperatures to rise, one of Greenland's previously most stable glaciers is now retreating at an unprecedented
    rate, according to a new study.


    ==========================================================================
    Led by researchers at The Ohio State University, a team found that between
    2018 and 2021, Steenstrup Glacier in Greenland has retreated about 5
    miles, thinned about 20%, doubled in the amount of ice it discharges
    into the ocean, and quadrupled in velocity. According to the study,
    such a rapid change is so extraordinary among Greenland ice formations
    that it now places Steenstrup in the top 10% of glaciers that contribute
    to the entire region's total ice discharge.

    The study was published today in Nature Communications.

    The Steenstrup Glacier is part of The Greenland Ice Sheet, a body of ice
    that covers nearly 80% of the world's largest island, which is also the
    single largest contributor to global sea rise from the cryosphere, the
    portion of Earth's ecosystem that includes all of its frozen water. While
    the region plays a crucial part in balancing the global climate system,
    the area is steadily shrinking as it sheds hundreds of billions of tons
    of ice each year because of global warming.

    Over the past few decades, much of this loss has been attributed to
    accelerated ice discharge from tidewater glaciers, glaciers that make
    contact with the ocean. Many glaciologists believe that this recent
    uptick in ice discharge can be explained by the intrusion of warming
    waters that are being swept from the Atlantic into Greenlandic fjords -- critical oceanic gateways that can impact the stability of local glaciers
    and the health of polar ecosystems.

    The research team aimed to test that theory by examining a glacier in the southeastern region of Greenland called K.I.V Steenstrups Nordre Brae,
    an entity more colloquially known as the Steenstrup Glacier.

    "Up until 2016, there was nothing to suggest Steenstrup was in any
    way interesting," said Thomas Chudley, lead author of the study, who
    completed this work as a research associate at the Byrd Polar and Climate Research Center.

    Chudley is now a Leverhulme research fellow at Durham University in
    the UK.

    "There were plenty of other glaciers in Greenland that had retreated dramatically since the 1990s and increased their contribution to sea
    level rise, but this really wasn't one of them." As far as scientists
    knew, Steenstrup had not only been stable for decades but was generally insensitive to the rising temperatures that had destabilized so many
    other regional glaciers, likely because of its isolated position in
    shallow waters.

    It wasn't until Chudley and his colleagues compiled observational and
    modeling data from previous remote sensing analyses on the glacier
    that the team realized Steenstrup was likely experiencing melt due to
    anomalies in deeper Atlantic water.

    "Our current working hypothesis is that ocean temperatures have forced
    this retreat," Chudley said. "The fact that the glacier's velocity has quadrupled in just a few years opens up new questions about how fast
    large ice masses can really respond to climate change." In recent
    years, glaciologists have been able to use satellite data to estimate
    the potential volume of glacial ice stored at the poles and how it might
    affect current sea levels. For instance, if the Greenland Ice Sheet were
    to melt, Earth's sea levels could rise by nearly 25 feet. In contrast,
    if the ice sheet in Antarctica were to fall apart, it's possible that
    oceans would rise by nearly 200 feet, Chudley said.

    While Greenland and Antarctica would take centuries to collapse
    completely, the global cryosphere has the potential to cause sea levels
    to rise about six feet this century if the West Antarctic Ice Sheet
    undergoes collapse.

    As around 10% of the planet's population lives in low-lying coastal zones, Chudley said that any significant rise in sea level can cause increased
    risk to low-lying islands and coastal communities from storm surges and tropical cyclones.

    In the United States, sea level rise poses a particular risk to coastal
    cities in places like Florida or Louisiana, Chudley said. But that doesn't necessarily mean it's too late to stop such a future from happening. If
    climate policies evolve rapidly, humans might have a chance at halting
    the worst of sea level rise, Chudley said.

    Overall, Steenstrup's unique behavior reveals that even long-term stable glaciers are susceptible to sudden and rapid retreat as warmer waters
    begin to intrude and influence new environments.

    While the research says continued scientific observation of the Steenstrup Glacier should be a priority, it concludes other similar glaciers also
    deserve attention because of their potential to retreat due to warming
    waters.

    Understanding more about these interactions could provide key insight
    into how glaciers thrive in other locations around the world and even
    become an indicator of how these environments might change in the future.

    "What's happening in Greenland right now is kind of the canary in the
    coal mine of what might happen in West Antarctica over the next few
    centuries," Chudley said. "So it would be great to be able to get into
    the fjord with real on-the- ground observations and see how and why
    Steenstrup has changed." This work was supported by NASA. Other Ohio
    State co-authors were Ian M. Howat and Adelaide Negrete of the Byrd
    Polar and Climate Research Center. Michalea D.

    King of the University of Washington was also a co-author.

    * RELATED_TOPICS
    o Earth_&_Climate
    # Global_Warming # Climate # Ice_Ages #
    Snow_and_Avalanches
    o Fossils_&_Ruins
    # Early_Climate # Ancient_DNA # Evolution # Origin_of_Life
    * RELATED_TERMS
    o Ice_sheet o Greenland_ice_sheet o Paleoclimatology
    o Global_warming_controversy o Global_climate_model o
    Climate_change_mitigation o Climate_engineering o Global_warming

    ========================================================================== Story Source: Materials provided by Ohio_State_University. Original
    written by Tatyana Woodall. Note: Content may be edited for style
    and length.


    ========================================================================== Journal Reference:
    1. T. R. Chudley, I. M. Howat, M. D. King, A. Negrete. Atlantic water
    intrusion triggers rapid retreat and regime change at previously
    stable Greenland glacier. Nature Communications, 2023; 14 (1) DOI:
    10.1038/ s41467-023-37764-7 ==========================================================================

    Link to news story: https://www.sciencedaily.com/releases/2023/04/230419125120.htm

    --- up 1 year, 7 weeks, 2 days, 10 hours, 52 minutes
    * Origin: -=> Castle Rock BBS <=- Now Husky HPT Powered! (1:317/3)