• New study reveals abrupt shift in tropic

    From ScienceDaily@1:317/3 to All on Mon Jul 3 22:30:28 2023
    New study reveals abrupt shift in tropical Pacific climate during Little
    Ice Age
    The shift to an El Nin~o-like phase between 1600 and 1900 A.D. was
    identified by sediment analysis of a Philippine lake

    Date:
    July 3, 2023
    Source:
    GFZ GeoForschungsZentrum Potsdam, Helmholtz Centre
    Summary:
    An El Nin~o event has officially begun. The climate phenomenon,
    which originates in the tropical Pacific and occurs in intervals of
    a few years will shape weather across the planet for the next year
    or more and give rise to various climatic extremes. El Nin~o-like
    conditions can also occur on longer time scales of decades or
    centuries. This has been shown to have occurred in the recent past.


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    FULL STORY ==========================================================================
    An El Nin~o event has officially begun. The climate phenomenon, which originates in the tropical Pacific and occurs in intervals of a few years
    will shape weather across the planet for the next year or more and give
    rise to various climatic extremes. El Nin~o-like conditions can also occur
    on longer time scales of decades or centuries. This has been shown to have occurred in the recent past by an international research team led by Ana Prohaska of the University of Copenhagen and Dirk Sachse of the German
    Research Centre for Geosciences (GFZ). Their analysis of biomarkers --
    organic molecules or molecular fossils from vascular plants -- in the
    sediments of a lake in the Philippines indicates an unusually dry phase
    in the region during the Little Ice Age between 1600 and 1900 A.D. The
    results have now been published in the journal Communications Earth and Environment. They show how important the understanding of past dynamics
    of the tropical Pacific ocean-atmosphere climate is for the improvement
    of climate models and the prediction of future climate changes.

    Background: The El Nin~o phenomenon A striking feature of climate in the equatorial Pacific is its east-west asymmetry, with warmer surface waters
    in the west and colder surface waters in the east. Easterly winds drive
    surface water westwards, allowing equatorial upwelling to bring cooler
    water to the eastern side. This asymmetry breaks down in today's climate, leading to El Nin~o conditions that occur at irregular intervals of a
    few years and last for 9-12 months.

    During an El Nin~o event, sea surface temperatures along the equator
    increase from the Peruvian coast to the central Pacific. The southeast
    trade wind weakens considerably, and light westerly winds may develop. In
    the western equatorial Pacific, which is otherwise characterised by
    abundant precipitation, an exceptional dryness takes hold, whereas the otherwise dry eastern edges of the Pacific may experience heavy rainfall.

    Against the backdrop of global warming, El Nin~o is expected to bring
    record- breaking high temperatures and various extreme climate events
    globally such as droughts, floods and wildfires, which will significantly affect the lives and well-being of millions of people.

    El Nin~o-like phenomena on longer time scales While El Nin~o is an
    interannual climate phenomenon, the climate system of the tropical
    Pacific can also exhibit El Nin~o-like behaviour on longer time scales
    of decades and centuries, which is linked to the east-west gradient of
    sea surface temperatures in the Pacific. Such behaviour has been shown
    to have transpired in the recent past by a team led by Ana Prohaska,
    assistant professor at the University of Copenhagen and formerly a
    visiting scientist at the GFZ, and Dirk Sachse, working group leader in
    GFZ Section 4.6 "Geomorphology" and director of Topic 5 "Landscapes of the Future" of the Helmholtz research programme "Changing Earth -- Sustaining
    our Future," in the journal Communications Earth and Environment.

    They describe such a pronounced shift to El Nin~o-like conditions in
    the second half of the Little Ice Age, lasting from about 1630 to 1900
    A.D. What is particularly remarkable is the short period of only one
    generation within which conditions changed for a period of more than
    200 years.

    Climate insights into the past through studies of sediment cores The
    research team examined sediment cores from Lake Bulusan in the northern Philippines, which were collected in 2013. The sediment sequence provides insights into the climatic evolution of the past 1,400 years in a region
    that is today strongly affected by El Nin~o events. In particular,
    the researchers analysed the composition of stable hydrogen isotopes in
    leaf wax biomarkers (dDwax). These are molecular fossils that originate
    from the protective surface layer of leaves from vascular plants. The
    analysis provides insights into water supply during their lifetime.

    Drier conditions in the western Pacific during the Little Ice Age The
    study shows a sudden and significant increase in dDwax values between
    1600 and 1650 A.D., indicating a shift towards drier conditions in
    the western tropical Pacific during the second half of the Little Ice
    Age. The researchers attribute this change to a shift in the mean state
    of the tropical Pacific Ocean related to zonal gradients, i.e., east-west differences in sea surface temperature.

    The significance of the current study for climate predictions Ana
    Prohaska, lead author of the study, emphasises the importance of this
    research: "Our study provides compelling evidence for the intricate relationship between zonal gradients in sea surface temperature and hydrological patterns in the tropical Pacific. Understanding the nature
    and pace of past changes in the tropical Pacific climate system is
    critical for predicting future climate change and its potential impact
    on this vulnerable region." Dirk Sachse from the GFZ adds: "Although
    there is increasing evidence that sudden climatic changes have occurred
    in the past, current climate models cannot reproduce such abrupt shifts
    in the mean state in the tropical Pacific.

    This highlights that the understanding of the underlying mechanisms is
    still limited. In the context of anthropogenic climate change, a better understanding of the drivers and consequences of the complex dynamics of
    the mean state of the tropical Pacific is of great importance. For this,
    the integration of palaeoclimatological data into modern climate models
    plays a crucial role."
    * RELATED_TOPICS
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    # Climate # Global_Warming # Environmental_Awareness
    # Weather
    o Fossils_&_Ruins
    # Early_Climate # Evolution # Ancient_DNA # Fossils
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    o El_Nin~o-Southern_Oscillation o Weather o Season o
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    ========================================================================== Journal Reference:
    1. Ana Prohaska, Alistair W. R. Seddon, Bernd Meese, Katherine
    J. Willis,
    John C. H. Chiang, Dirk Sachse. Abrupt change in tropical Pacific
    climate mean state during the Little Ice Age. Communications Earth &
    Environment, 2023; 4 (1) DOI: 10.1038/s43247-023-00882-7 ==========================================================================

    Link to news story: https://www.sciencedaily.com/releases/2023/07/230703133053.htm

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