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Bidecadal North Atlantic ocean circulation variability controlled by timing of volcanic eruptions

Allbwn ymchwil: Cyfraniad at gyfnodolyn › Erthygl › adolygiad gan gymheiriaid

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Bidecadal North Atlantic ocean circulation variability controlled by timing of volcanic eruptions. / Swingedouw, D.; Ortega, P.; Mignot, J. et al.
Yn: Nature Communications, Cyfrol 6, 30.03.2015, t. Article Number 6545.

Allbwn ymchwil: Cyfraniad at gyfnodolyn › Erthygl › adolygiad gan gymheiriaid

HarvardHarvard

Swingedouw, D, Ortega, P, Mignot, J, Guilyardi, E, Masson-Delmotte, V, Butler, PG, Khodri, M & Seferian, R 2015, 'Bidecadal North Atlantic ocean circulation variability controlled by timing of volcanic eruptions', Nature Communications, cyfrol. 6, tt. Article Number 6545. https://doi.org/10.1038/ncomms7545

APA

Swingedouw, D., Ortega, P., Mignot, J., Guilyardi, E., Masson-Delmotte, V., Butler, P. G., Khodri, M., & Seferian, R. (2015). Bidecadal North Atlantic ocean circulation variability controlled by timing of volcanic eruptions. Nature Communications, 6, Article Number 6545. https://doi.org/10.1038/ncomms7545

CBE

Swingedouw D, Ortega P, Mignot J, Guilyardi E, Masson-Delmotte V, Butler PG, Khodri M, Seferian R. 2015. Bidecadal North Atlantic ocean circulation variability controlled by timing of volcanic eruptions. Nature Communications. 6:Article Number 6545. https://doi.org/10.1038/ncomms7545

MLA

Swingedouw, D. et al. "Bidecadal North Atlantic ocean circulation variability controlled by timing of volcanic eruptions". Nature Communications. 2015, 6. Article Number 6545. https://doi.org/10.1038/ncomms7545

VancouverVancouver

Swingedouw D, Ortega P, Mignot J, Guilyardi E, Masson-Delmotte V, Butler PG et al. Bidecadal North Atlantic ocean circulation variability controlled by timing of volcanic eruptions. Nature Communications. 2015 Maw 30;6:Article Number 6545. doi: 10.1038/ncomms7545

Author

Swingedouw, D. ; Ortega, P. ; Mignot, J. et al. / Bidecadal North Atlantic ocean circulation variability controlled by timing of volcanic eruptions. Yn: Nature Communications. 2015 ; Cyfrol 6. tt. Article Number 6545.

RIS

TY - JOUR

T1 - Bidecadal North Atlantic ocean circulation variability controlled by timing of volcanic eruptions

AU - Swingedouw, D.

AU - Ortega, P.

AU - Mignot, J.

AU - Guilyardi, E.

AU - Masson-Delmotte, V.

AU - Butler, P.G.

AU - Khodri, M.

AU - Seferian, R.

PY - 2015/3/30

Y1 - 2015/3/30

N2 - While bidecadal climate variability has been evidenced in several North Atlantic paleoclimate records, its drivers remain poorly understood. Here we show that the subset of CMIP5 historical climate simulations that produce such bidecadal variability exhibits a robust synchronization, with a maximum in Atlantic Meridional Overturning Circulation (AMOC) 15 years after the 1963 Agung eruption. The mechanisms at play involve salinity advection from the Arctic and explain the timing of Great Salinity Anomalies observed in the 1970s and the 1990s. Simulations, as well as Greenland and Iceland paleoclimate records, indicate that coherent bidecadal cycles were excited following five Agung-like volcanic eruptions of the last millennium. Climate simulations and a conceptual model reveal that destructive interference caused by the Pinatubo 1991 eruption may have damped the observed decreasing trend of the AMOC in the 2000s. Our results imply a long-lasting climatic impact and predictability following the next Agung-like eruption.

AB - While bidecadal climate variability has been evidenced in several North Atlantic paleoclimate records, its drivers remain poorly understood. Here we show that the subset of CMIP5 historical climate simulations that produce such bidecadal variability exhibits a robust synchronization, with a maximum in Atlantic Meridional Overturning Circulation (AMOC) 15 years after the 1963 Agung eruption. The mechanisms at play involve salinity advection from the Arctic and explain the timing of Great Salinity Anomalies observed in the 1970s and the 1990s. Simulations, as well as Greenland and Iceland paleoclimate records, indicate that coherent bidecadal cycles were excited following five Agung-like volcanic eruptions of the last millennium. Climate simulations and a conceptual model reveal that destructive interference caused by the Pinatubo 1991 eruption may have damped the observed decreasing trend of the AMOC in the 2000s. Our results imply a long-lasting climatic impact and predictability following the next Agung-like eruption.

UR - https://static-content.springer.com/esm/art%3A10.1038%2Fncomms7545/MediaObjects/41467_2015_BFncomms7545_MOESM1218_ESM.pdf

U2 - 10.1038/ncomms7545

DO - 10.1038/ncomms7545

M3 - Article

VL - 6

SP - Article Number 6545

JO - Nature Communications

JF - Nature Communications

SN - 2041-1723

ER -