過去の気候変動が海洋循環に与えた影響(Past climate change shifts ocean currents and winds, altering heat and carbon exchange in the Southern Ocean, study finds)

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2025-01-01 カーディフ大学

カーディフ大学が主導する研究により、過去の気候変動が南極環流(ACC)や西風帯の変化を引き起こし、南大洋での熱と炭素交換に影響を与えたことが明らかになりました。約150万年間にわたり、温暖化時には西風帯とACCが極地に移動し、大気中に放出される自然由来の炭素が増加。この現象が現代の気候変動にも関連すると警告されています。本研究は、南大洋が気候調節に果たす役割を強調しています。

<関連情報>

過去190万年間にアフリカの南で変動した南極循環極海流 Shifting Antarctic Circumpolar Current south of Africa over the past 1.9 million years

Aidan Starr, Ian R. Hall, Stephen Barker, Alexandra Nederbragt, […], and Sidney R. Hemming
Science Advances  Published:1 Jan 2025
DOI:https://doi.org/10.1126/sciadv.adp1692

過去の気候変動が海洋循環に与えた影響(Past climate change shifts ocean currents and winds, altering heat and carbon exchange in the Southern Ocean, study finds)

Abstract

The Antarctic Circumpolar Current (ACC) dominates the transfer of heat, salt, and tracers around the Southern Ocean (SO), driving the upwelling of carbon-rich deep waters around Antarctica. Paleoclimate reconstructions reveal marked variability in SO circulation; however, few records exist coupling quantitative reconstructions of ACC flow with tracers of SO upwelling spanning multiple Pleistocene glacial cycles. Here, we reconstruct near-bottom flow speed variability in the SO south of Africa, revealing systematic glacial-interglacial variations in the strength and/or proximity of ACC jets. These are superimposed by warmer-than-present “super-interglacials,” whereby extreme slowdown in the midlatitude ACC (41°S) is opposed by faster flow at higher latitudes (>54°S), implying poleward strengthening of the ACC. Coupled with reconstructions of the subsurface-deep stable carbon isotope gradient, we show that the reorganization of ACC coincides with the upwelling of isotopically light deep waters around Antarctica, likely contributing to the interglacial rise in atmospheric carbon dioxide (CO2) levels.

1702地球物理及び地球化学
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