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Environmental magnetism and climate change.

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Environmental magnetism and climate change. / Maher, Barbara A.
In: Contemporary Physics, Vol. 48, No. 5, 09.2007, p. 247-274.

Research output: Contribution to Journal/MagazineJournal articlepeer-review

Harvard

Maher, BA 2007, 'Environmental magnetism and climate change.', Contemporary Physics, vol. 48, no. 5, pp. 247-274. https://doi.org/10.1080/00107510801889726

APA

Vancouver

Maher BA. Environmental magnetism and climate change. Contemporary Physics. 2007 Sept;48(5):247-274. doi: 10.1080/00107510801889726

Author

Maher, Barbara A. / Environmental magnetism and climate change. In: Contemporary Physics. 2007 ; Vol. 48, No. 5. pp. 247-274.

Bibtex

@article{742afd02d1414924bd2a60cac0c708a5,
title = "Environmental magnetism and climate change.",
abstract = "A major and pressing problem is to understand how, and how fast, the Earth{\textquoteright}s climate has changed in the past, with and without human influences on the global carbon cycle. Magnetic, remanence-acquiring, minerals, mostly iron oxides and sulphides, occur ubiquitously in sediments. They can act as sensitive recorders of past climates, because as climate has varied (from glacial to interglacial, for example), the mineralogy, magnetic domain state, composition and source of these minerals has varied. Here, the magnetic properties of windblown dust and interbedded soil layers of the Chinese Loess Plateau are used to calculate rainfall for the last million years, identifying the waxing and waning of the southeast Asian summer monsoon. Comparison of our magnetic rainfall record on land with environmental records from the deep-sea shows that summer monsoon intensity is linked with growth and decay of continental-sized ice sheets, in turn reflecting changes in the Earth{\textquoteright}s orbit around the Sun.",
keywords = "climate change, environmental magnetism, magnetite, magnetic domains",
author = "Maher, {Barbara A}",
year = "2007",
month = sep,
doi = "10.1080/00107510801889726",
language = "English",
volume = "48",
pages = "247--274",
journal = "Contemporary Physics",
issn = "0010-7514",
publisher = "Taylor & Francis",
number = "5",

}

RIS

TY - JOUR

T1 - Environmental magnetism and climate change.

AU - Maher, Barbara A

PY - 2007/9

Y1 - 2007/9

N2 - A major and pressing problem is to understand how, and how fast, the Earth’s climate has changed in the past, with and without human influences on the global carbon cycle. Magnetic, remanence-acquiring, minerals, mostly iron oxides and sulphides, occur ubiquitously in sediments. They can act as sensitive recorders of past climates, because as climate has varied (from glacial to interglacial, for example), the mineralogy, magnetic domain state, composition and source of these minerals has varied. Here, the magnetic properties of windblown dust and interbedded soil layers of the Chinese Loess Plateau are used to calculate rainfall for the last million years, identifying the waxing and waning of the southeast Asian summer monsoon. Comparison of our magnetic rainfall record on land with environmental records from the deep-sea shows that summer monsoon intensity is linked with growth and decay of continental-sized ice sheets, in turn reflecting changes in the Earth’s orbit around the Sun.

AB - A major and pressing problem is to understand how, and how fast, the Earth’s climate has changed in the past, with and without human influences on the global carbon cycle. Magnetic, remanence-acquiring, minerals, mostly iron oxides and sulphides, occur ubiquitously in sediments. They can act as sensitive recorders of past climates, because as climate has varied (from glacial to interglacial, for example), the mineralogy, magnetic domain state, composition and source of these minerals has varied. Here, the magnetic properties of windblown dust and interbedded soil layers of the Chinese Loess Plateau are used to calculate rainfall for the last million years, identifying the waxing and waning of the southeast Asian summer monsoon. Comparison of our magnetic rainfall record on land with environmental records from the deep-sea shows that summer monsoon intensity is linked with growth and decay of continental-sized ice sheets, in turn reflecting changes in the Earth’s orbit around the Sun.

KW - climate change

KW - environmental magnetism

KW - magnetite

KW - magnetic domains

U2 - 10.1080/00107510801889726

DO - 10.1080/00107510801889726

M3 - Journal article

VL - 48

SP - 247

EP - 274

JO - Contemporary Physics

JF - Contemporary Physics

SN - 0010-7514

IS - 5

ER -