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
AUTHORS (24)
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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CITATIONS (23)
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