ENSO related decadal scale climate variability from the Indo-Pacific Warm Pool

J.M. Brijker; S.J.A. Jung; G.M. Ganssen; T. Bickert; D. Kroon

doi:10.1016/j.epsl.2006.10.017

ENSO related decadal scale climate variability from the Indo-Pacific Warm Pool

J.M. Brijker, S.J.A. Jung, G.M. Ganssen, T. Bickert, D. Kroon

Earth and Climate

Research output: Contribution to Journal › Article › Academic › peer-review

Abstract

The El Niño-Southern Oscillation (ENSO) is a climatic phenomenon that affects socio-economical welfare in vast areas in the world. A continuous record of Holocene ENSO related climate variability of the Indo-Pacific Warm pool (IPWP) is constructed on the basis of stable oxygen isotopes in shells of planktic foraminifera from a sediment core in the western Pacific Ocean. At the centennial scale, variations in the stable oxygen isotope signal (δ

Original language	English
Pages (from-to)	67-82
Journal	Earth and Planetary Science Letters
Volume	253
Issue number	1-2
DOIs	https://doi.org/10.1016/j.epsl.2006.10.017
Publication status	Published - 2006

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10.1016/j.epsl.2006.10.017

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title = "ENSO related decadal scale climate variability from the Indo-Pacific Warm Pool",

abstract = "The El Ni{\~n}o-Southern Oscillation (ENSO) is a climatic phenomenon that affects socio-economical welfare in vast areas in the world. A continuous record of Holocene ENSO related climate variability of the Indo-Pacific Warm pool (IPWP) is constructed on the basis of stable oxygen isotopes in shells of planktic foraminifera from a sediment core in the western Pacific Ocean. At the centennial scale, variations in the stable oxygen isotope signal (δ",

author = "J.M. Brijker and S.J.A. Jung and G.M. Ganssen and T. Bickert and D. Kroon",

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AU - Brijker, J.M.

AU - Jung, S.J.A.

AU - Ganssen, G.M.

AU - Bickert, T.

AU - Kroon, D.

PY - 2006

Y1 - 2006

N2 - The El Niño-Southern Oscillation (ENSO) is a climatic phenomenon that affects socio-economical welfare in vast areas in the world. A continuous record of Holocene ENSO related climate variability of the Indo-Pacific Warm pool (IPWP) is constructed on the basis of stable oxygen isotopes in shells of planktic foraminifera from a sediment core in the western Pacific Ocean. At the centennial scale, variations in the stable oxygen isotope signal (δ

AB - The El Niño-Southern Oscillation (ENSO) is a climatic phenomenon that affects socio-economical welfare in vast areas in the world. A continuous record of Holocene ENSO related climate variability of the Indo-Pacific Warm pool (IPWP) is constructed on the basis of stable oxygen isotopes in shells of planktic foraminifera from a sediment core in the western Pacific Ocean. At the centennial scale, variations in the stable oxygen isotope signal (δ

U2 - 10.1016/j.epsl.2006.10.017

DO - 10.1016/j.epsl.2006.10.017

M3 - Article

SN - 0012-821X

VL - 253

SP - 67

EP - 82

JO - Earth and Planetary Science Letters

JF - Earth and Planetary Science Letters

IS - 1-2

ER -

ENSO related decadal scale climate variability from the Indo-Pacific Warm Pool

Abstract

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