• Major Atlantic ocean current system migh

    From ScienceDaily@1:317/3 to All on Thu Aug 5 21:30:42 2021
    Major Atlantic ocean current system might be approaching critical
    threshold

    Date:
    August 5, 2021
    Source:
    Potsdam Institute for Climate Impact Research (PIK)
    Summary:
    A major Atlantic ocean current -- the Atlantic Meridional
    Overturning Circulation, or AMOC -- may have been losing stability
    in the course of the last century, according to new research. A
    potential collapse of this ocean current system could have severe
    consequences.



    FULL STORY ========================================================================== [Ocean waves (stock | Credit: (c) Noradoa / stock.adobe.com] Ocean waves
    (stock image).

    Credit: (c) Noradoa / stock.adobe.com [Ocean waves (stock | Credit:
    (c) Noradoa / stock.adobe.com] Ocean waves (stock image).

    Credit: (c) Noradoa / stock.adobe.com Close The major Atlantic ocean
    current, to which also the Gulf stream belongs, may have been losing
    stability in the course of the last century. This is shown in a new study published in Nature Climate Change. The Atlantic Meridional Overturning Circulation, or AMOC, transports warm water masses from the tropics
    northward at the ocean surface and cold water southward at the ocean
    bottom, which is most relevant for the relatively mild temperatures in
    Europe. Further, it influences weather systems worldwide. A potential
    collapse of this ocean current system could therefore have severe
    consequences.


    ==========================================================================
    "The Atlantic Meridional Overturning really is one of our planet's key circulation systems," says the author of the study, Niklas Boers from the Potsdam Institute for Climate Impact Research, Freie Universita"t Berlin
    and Exeter University. "We already know from some computer simulations
    and from data from Earth's past, so-called paleoclimate proxy records,
    that the AMOC can exhibit -- in addition to the currently attained strong
    mode -- an alternative, substantially weaker mode of operation. This bi-stability implies that abrupt transitions between the two circulation
    modes are in principle possible." Loss of dynamical stability could
    ultimately lead to collapse It has been shown previously that the AMOC
    is currently at its weakest in more than a 1000 years. However, so far it
    has remained an open question whether the observed weakening corresponds
    to a change in the mean circulation state, or whether it is associated
    with an actual loss of dynamical stability. "The difference is crucial,"
    says Niklas Boers, "because the loss of dynamical stability would imply
    that the AMOC has approached its critical threshold, beyond which a
    substantial and in practice likely irreversible transition to the weak
    mode could occur." Long-term observational data of the strength of
    the AMOC does unfortunately not exist, but the AMOC leaves so-called fingerprints in sea-surface temperature and salinity patterns of the
    Atlantic ocean. "A detailed analysis of these fingerprints in eight
    independent indices now suggests that the AMOC weakening during the last century is indeed likely to be associated with a loss of stability,"
    says Boers. "The findings support the assessment that the AMOC decline is
    not just a fluctuation or a linear response to increasing temperatures
    but likely means the approaching of a critical threshold beyond which
    the circulation system could collapse." In addition to global warming, freshwater inflow is a factor -- which is also linked to climate change
    A number of factors are likely important for the phenomenon -- factors
    that add to the direct effect that the warming of the Atlantic ocean has
    on its circulation. These include freshwater inflow from the melting of
    the Greenland ice sheet, melting sea-ice, increasing precipitation and
    river run-off.

    Freshwater is lighter than saltwater and reduces the tendency of the
    water to sink from the surface to greater depths, which is one of the
    drivers of the overturning.

    "I wouldn't have expected that the excessive amounts of freshwater added
    in the course of the last century would already produce such a response in
    the overturning circulation," says Boers. "We urgently need to reconcile
    our models with the presented observational evidence to assess how far
    from or how close to its critical threshold the AMOC really is." While
    the respective relevance of the different factors has to be further investigated, they're all linked to human-caused climate change.

    ========================================================================== Story Source: Materials provided by Potsdam_Institute_for_Climate_Impact_Research_(PIK).

    Note: Content may be edited for style and length.


    ========================================================================== Journal Reference:
    1. Niklas Boers. Observation-based early-warning signals for a
    collapse of
    the Atlantic Meridional Overturning Circulation. Nature Climate
    Change, 2021 DOI: 10.1038/s41558-021-01097-4 ==========================================================================

    Link to news story: https://www.sciencedaily.com/releases/2021/08/210805115420.htm

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