dot
Detailansicht
Katalogkarte GBA
Katalogkarte ISBD
Suche präzisieren
Drucken
Download RIS
Hier klicken, um den Treffer aus der Auswahl zu entfernen
Titel Pronounced warming in the Indian and Pacific sectors of the Southern Ocean during the 1970s
VerfasserIn Chris Turney, Chris Fogwill, Jonathan Palmer, Erik van Sebille, Zoë Thomas, Matt McGlone, Sarah Richardson, Janet Wilmshurst, Pavla Fenwick, Lionel Carter, Richard Jones, Melanie Harsch, Kerry-Jayne Wilson, Graeme Clark, Ezequiel Marzinelli, Tracey Rogers, Eleanor Rainsley, Laura Ciasto, Stephanie Waterman, Australasian Antarctic Expedition 2013-2014 Members
Konferenz EGU General Assembly 2015
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 17 (2015)
Datensatznummer 250103169
Publikation (Nr.) Volltext-Dokument vorhandenEGU/EGU2015-2568.pdf
 
Zusammenfassung
Occupying some 20% of the world’s ocean surface, the Southern Ocean is home to a diverse and unique biota and plays a fundamental role in global oceanic circulation, climate variability, Antarctic ice sheet stability and carbon cycling. Significant warming has been observed over recent decades, most prominently in the Antarctic Circumpolar Current (ACC). The mechanism(s) behind this warming, however, remain uncertain. Here, we integrate historic ocean and atmospheric observations and climate-sensitive tree growth on subantarctic islands from the northern limit of the ACC to extend historic and satellite measurements to produce a unique proxy record of temperature across 4˚ of latitude in the southwest Pacific. We demonstrate a hitherto unobserved abrupt warming during the 1970s that is unprecedented over the past 130 years, coincident with a significant decline in marine vertebrate populations and wider warming across the Indian Ocean. Comparison between our reconstruction and high-resolution ocean modelling provides a possible mechanism, suggesting warmer waters resulted from a poleward migration of the subtropical and ACC fronts. Projected increases in the strength of westerly winds are likely to continue the fronts’ migration, driving warming in the Southern Ocean (>50˚S), with significant impacts on biota.