(Q58383981)

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Enhancement of dust source area during past glacial periods due to changes of the Hadley circulation

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Enhancement of dust source area during past glacial periods due to changes of the Hadley circulation (English)

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Ulrike Lohmann

3

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Petr Chýlek

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1

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Petr Chylek

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author name string

Glen Lesins

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2

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language of work or name

English

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publication date

1 August 2001

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published in

Journal of Geophysical Research

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volume

106

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issue

D16

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page(s)

18477-18485

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cites work

Atmospheric dust under glacial and interglacial conditions

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https://api.crossref.org/works/10.1029%2F2000JD900583

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21 January 2018

Aerosols and climate.

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21 January 2018

The surface of the ice-age Earth

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https://api.crossref.org/works/10.1029%2F2000JD900583

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21 January 2018

Dust sources and deposition during the last glacial maximum and current climate: A comparison of model results with paleodata from ice cores and marine sediments

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21 January 2018

Changes in Atmospheric Circulation and Ocean Ice Cover over the North Atlantic During the Last 41,000 Years.

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21 January 2018

Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica

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21 January 2018

Tropical paleoclimates at the Last Glacial Maximum: comparison of Paleoclimate Modeling Intercomparison Project (PMIP) simulations and paleodata

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21 January 2018

Late Proterozoic and Paleozoic Tides, Retreat of the Moon, and Rotation of the Earth

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21 January 2018

Abrupt changes in early Holocene tropical sea surface temperature derived from coral records

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21 January 2018

A 30,000-yr isotope climatic record from Antarctic ice

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21 January 2018

Direct radiative forcing by anthropogenic airborne mineral aerosols

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21 January 2018

Influence of ocean heat transport on the climate of the Last Glacial Maximum

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21 January 2018

A sensitivity study of changes in Earth's rotation rate with an atmospheric general circulation model

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21 January 2018

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(Q58383981)

Enhancement of dust source area during past glacial periods due to changes of the Hadley circulation

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