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|    ScienceDaily to All    |
|    Massive iceberg discharges during the la    |
|    24 Apr 23 22:30:26    |
      MSGID: 1:317/3 64475766       PID: hpt/lnx 1.9.0-cur 2019-01-08       TID: hpt/lnx 1.9.0-cur 2019-01-08        Massive iceberg discharges during the last ice age had no impact on       nearby Greenland, raising new questions about climate dynamics                Date:        April 24, 2023        Source:        Oregon State University        Summary:        New findings suggest that Heinrich Events had no discernible impact        on temperatures in Greenland, which could have repercussions for        scientists' understanding of past climate dynamics.                      Facebook Twitter Pinterest LinkedIN Email              ==========================================================================       FULL STORY       ==========================================================================       During the last ice age, massive icebergs periodically broke off from       an ice sheet covering a large swath of North America and discharged       rapidly melting ice into the North Atlantic Ocean around Greenland,       triggering abrupt climate change impacts across the globe.              These sudden episodes, called Heinrich Events, occurred between 16,000       and 60,000 years ago. They altered the circulation of the world's oceans,       spurring cooling in the North Atlantic and impacting monsoon rainfall       around the world.              But little was known about the events' effect on nearby Greenland, which       is thought to be very sensitive to events in the North Atlantic. A new       study from Oregon State University researchers, just published in the       journal Nature, provides a definitive answer.              "It turns out, nothing happened in Greenland. The temperature just stayed       the same," said the study's lead author, Kaden Martin, a fourth-year       doctoral candidate in OSU's College of Earth, Ocean, and Atmospheric       Sciences. "They had front-row seats to this action but didn't see       the show." Instead, the researchers found that these Heinrich events       caused rapid warming in Antarctica, at the other end of the globe.              The researchers anticipated Greenland, in close proximity to the ice       sheet, would have experienced some kind of cooling. To find that these       Heinrich Events had no discernible impact on temperatures in Greenland is       surprising and could have repercussions for scientists' understanding of       past climate dynamics, said study co-author Christo Buizert, an assistant       professor in the College of Earth, Ocean, and Atmospheric Sciences.              "If anything, our findings raise more questions than answers," said       Buizert, a climate change specialist who uses ice cores from Greenland       and Antarctica to reconstruct and understand the Earth's climate       history. "This really changes how we look at these massive events in       the North Atlantic. It's puzzling that far-flung Antarctica responds       more strongly than nearby Greenland." Scientists drill and preserve       ice cores to study past climate history through analysis of the dust       and tiny air bubbles that have been trapped in the ice over time. Ice       cores from Greenland and Antarctica provide important records of Earth's       atmospheric changes over hundreds of thousands of years.              Records from ice cores from those regions have served as pillars for       scientists' understanding of past climate events, with ice collected       from both locations often telling similar stories, Martin said.              The impact of Heinrich Events on Greenland and Antarctica was not well       understood, spurring Martin and Buizert to try to find out more about       what was happening in those parts of the world.              The core used for the latest study was collected in 1992 from the highest       point of Greenland, where the ice sheet is around 2 miles thick. Since       then, the core has been in storage in the National Science Foundation       Ice Core Facility in Denver.              Advancement in scientific tools and measurements over the last few decades       gave Martin, Buizert and their colleagues the opportunity to re-examine       the core using new methods.              The analysis shows that no changes in temperatures occurred in Greenland       during Heinrich Events. But it also provides a very clear connection       between Heinrich Events and the Antarctic response.              "When these big iceberg discharges happen in the Arctic, we now know       that Antarctica responds right away," Buizert said. "What happens in       one part of the world has an effect on the rest of the world. This       inter-hemispheric connection is likely caused by change in global wind       patterns." The finding challenges the current understanding of global       climate dynamics during these massive events and raises new questions       for researchers, Buizert said. The researchers' next step is to take the       new information and run it through climate models to see if the models       can replicate what occurred.              "There has to be a story that fits all of the evidence, something that       connects all the dots," he said. "Our discovery adds two new dots; it's       not the full story, and it may not be the main story. It is possible that       the Pacific Ocean plays an important role that we haven't figured out       yet." The ultimate goal is to better understand how the climate system       is connected and how the components all interact, the researchers said.              "While Heinrich Events are not going to happen in the future, abrupt       changes in the globally interconnected climate system will happen again,"       Martin said.              "Understanding the global dynamics of the climate system can help us       better project future impacts and inform how we respond and adapt."       Additional co-authors are Ed Brook, Jon Edwards, Michael Kalk and Ben       Riddell- Young of OSU; Ross Beaudette and Jeffrey Severinghaus of the       Scripps Institution of Oceanography; and Todd Sowers of Pennsylvania       State University.              The research was supported by the National Science Foundation, the       Global Climate Change Foundation and the Gary Comer Science and Education       Foundation.               * RELATED_TOPICS        o Earth_&_Climate        # Climate # Global_Warming # Ice_Ages #        Environmental_Awareness        o Fossils_&_Ruins        # Early_Climate # Ancient_DNA # Evolution # Fossils        * RELATED_TERMS        o Temperature_record_of_the_past_1000_years o        Attribution_of_recent_climate_change o Greenland_ice_sheet        o Ice_sheet o Annual_sedimentary_layer o Global_warming o        Chicxulub_Crater o Climate_model              ==========================================================================       Story Source: Materials provided by Oregon_State_University. Original       written by Michelle Klampe. Note: Content may be edited for style       and length.                     ==========================================================================       Journal Reference:        1. Kaden C. Martin, Christo Buizert, Jon S. Edwards, Michael L. Kalk,        Ben        Riddell-Young, Edward J. Brook, Ross Beaudette, Jeffrey        P. Severinghaus, Todd A. Sowers. Bipolar impact and phasing        of Heinrich-type climate variability. Nature, 2023; DOI:        10.1038/s41586-023-05875-2       ==========================================================================              Link to news story:       https://www.sciencedaily.com/releases/2023/04/230424133551.htm              --- up 1 year, 8 weeks, 10 hours, 50 minutes        * Origin: -=> Castle Rock BBS <=- Now Husky HPT Powered! 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