Heinrich Events


Reference list is under construction.



by Yohai Kaspi, Roiy Sayag, Eli Tziperman
Abstract:
Abrupt, switch-like, changes in sea ice cover are proposed as a mechanism for the large-amplitude abrupt warming that seemed to have occurred after each Heinrich event. Sea ice changes are also used to explain the colder-than-ambient glacial conditions around the time of the glacier discharge. The abrupt warming events occur in this mechanism, owing to rapid sea ice melting which warmed the atmosphere via the strong sea ice albedo and insulating feedbacks. Such abrupt sea ice changes can also account for the warming observed during Dansgaard-Oeschger events. The sea ice changes are caused by a weak (order of 5 Sv) response of the thermohaline circulation (THC) to glacier discharges. The main point of this work is therefore that sea ice may be thought of as a very effective amplifier of a weak THC variability, explaining the abrupt temperature changes over Greenland. Synchronous ice sheet collapses from different ice sheets around the North Atlantic, indicated by some proxy records, are shown to be possible via the weak coupling between the different ice sheets by the atmospheric temperature changes caused by the sea ice changes. This weak coupling can lead to a ” nonlinear phase locking” of the different ice sheets which therefore discharge synchronously. It is shown that the phase locking may also lead to ” precursor” glacier discharge events from smaller ice sheets before the Laurentide Ice Sheet discharges. The precursor events in this mechanism are the result rather than the cause of the major glacier discharges from the Laurentide Ice Sheet.
Reference:
A "triple sea-ice state" mechanism for the abrupt warming and synchronous ice sheet collapses during Heinrich events (Yohai Kaspi, Roiy Sayag, Eli Tziperman), In Paleoceanography, volume 19, 2004.
Bibtex Entry:
@article{citeulike:10074608,
    abstract = {{Abrupt, switch-like, changes in sea ice cover are proposed as a mechanism for the large-amplitude abrupt warming that seemed
                        to have occurred after each Heinrich event. Sea ice changes are also used to explain the colder-than-ambient glacial conditions
                        around the time of the glacier discharge. The abrupt warming events occur in this mechanism, owing to rapid sea ice melting
                        which warmed the atmosphere via the strong sea ice albedo and insulating feedbacks. Such abrupt sea ice changes can also account
                        for the warming observed during Dansgaard-Oeschger events. The sea ice changes are caused by a weak (order of 5 Sv) response
                        of the thermohaline circulation (THC) to glacier discharges. The main point of this work is therefore that sea ice may be
                        thought of as a very effective amplifier of a weak THC variability, explaining the abrupt temperature changes over Greenland.
                        Synchronous ice sheet collapses from different ice sheets around the North Atlantic, indicated by some proxy records, are
                        shown to be possible via the weak coupling between the different ice sheets by the atmospheric temperature changes caused
                        by the sea ice changes. This weak coupling can lead to a  ” nonlinear phase locking” of the different ice sheets which therefore
                        discharge synchronously. It is shown that the phase locking may also lead to  ” precursor” glacier discharge events from smaller
                        ice sheets before the Laurentide Ice Sheet discharges. The precursor events in this mechanism are the result rather than the
                        cause of the major glacier discharges from the Laurentide Ice Sheet.
                     }},
    author = {Kaspi, Yohai and Sayag, Roiy and Tziperman, Eli},
    citeulike-article-id = {10074608},
    citeulike-linkout-0 = {http://www.agu.org/pubs/crossref/2004/2004PA001009.shtml},
    citeulike-linkout-1 = {http://dx.doi.org/10.1029/2004PA001009},
    day = {14},
    doi = {10.1029/2004PA001009},
    issn = {0883-8305},
    journal = {Paleoceanography},
    keywords = {abrupt, climate, do-event, glacial, heinrich, ice, paleoclimate, sea-ice, warming},
    month = jul,
    number = {3},
    pages = {PA3004+},
    posted-at = {2011-11-27 13:34:18},
    priority = {2},
    title = {{A "triple sea-ice state" mechanism for the abrupt warming and synchronous ice sheet collapses during Heinrich events}},
    url = {http://dx.doi.org/10.1029/2004PA001009},
    volume = {19},
    year = {2004}
}
Powered by bibtexbrowser
Dr. Jennifer D. Stanford, Geography & Environment, University of Southampton