Tropical forcing of increased Southern Ocean climate variability revealed by a 140-year subantarctic temperature reconstruction

POPULATION-DYNAMICS 550 Stratigraphy anzsrc-for: 0406 Physical Geography and Environmental Geoscience NEW-ZEALAND WEST ANTARCTICA SEALS MIROUNGA-LEONINA Social and Behavioral Sciences 551 Environmental protection 01 natural sciences Environmental pollution CECI [CISM] ROCKHOPPER PENGUINS PAST MILLENNIUM Medicine and Health Sciences Meteorology & Atmospheric Sciences GE1-350 Geosciences, Multidisciplinary Global and Planetary Change GB Multidisciplinary anzsrc-for: 3709 Physical Geography and Environmental Geoscience Palaeontology anzsrc-for: 37 Earth Sciences Geology HEMISPHERE SURFACE CLIMATE 16. Peace & justice TD172-193.5 Physical Sciences 3701 Atmospheric Sciences Geosciences 0406 Physical Geography And Environmental Geoscience 3702 Climate Change Science CAMPBELL-ISLAND TD169-171.8 G1 3708 Oceanography 14. Life underwater anzsrc-for: 3701 Atmospheric Sciences MACQUARIE ISLAND 0105 earth and related environmental sciences 13 Climate Action Science & Technology anzsrc-for: 3702 Climate Change Science Paleontology 37 Earth Sciences 3709 Physical Geography and Environmental Geoscience 14 Life Below Water anzsrc-for: 3708 Oceanography Environmental sciences 13. Climate action ANNULAR MODE
DOI: 10.5194/cp-13-231-2017 Publication Date: 2017-03-15T12:38:10Z
ABSTRACT
Abstract. Occupying about 14 % of the world's surface, the Southern Ocean plays a fundamental role in ocean and atmosphere circulation, carbon cycling and Antarctic ice-sheet dynamics. Unfortunately, high interannual variability and a dearth of instrumental observations before the 1950s limits our understanding of how marine–atmosphere–ice domains interact on multi-decadal timescales and the impact of anthropogenic forcing. Here we integrate climate-sensitive tree growth with ocean and atmospheric observations on southwest Pacific subantarctic islands that lie at the boundary of polar and subtropical climates (52–54° S). Our annually resolved temperature reconstruction captures regional change since the 1870s and demonstrates a significant increase in variability from the 1940s, a phenomenon predating the observational record. Climate reanalysis and modelling show a parallel change in tropical Pacific sea surface temperatures that generate an atmospheric Rossby wave train which propagates across a large part of the Southern Hemisphere during the austral spring and summer. Our results suggest that modern observed high interannual variability was established across the mid-twentieth century, and that the influence of contemporary equatorial Pacific temperatures may now be a permanent feature across the mid- to high latitudes.
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