Dust size evidence for opposite regional atmospheric circulation changes over east Antarctica during the last climatic transition

Author:

Delmonte B.,Petit J. R.,Andersen K. K.,Basile-Doelsch I.,Maggi V.,Ya Lipenkov V.

Publisher

Springer Science and Business Media LLC

Subject

Atmospheric Science

Reference36 articles.

1. Andersen KK (1998) Simulations of atmospheric dust in the glacial and interglacial climate. PhD Thesis, Niels Bohr Institute of Astronomy,Physics and Geophysics, University of Copenhagen, Copenhagen, pp 136

2. Basile I (1997) Origine des aérosols volcaniques et continentaux de la carotte de glace de Vostok (Antarctique). PhD Thesis, LGGE-UniversitéJoseph Fourier-Grenoble I, Grenoble, pp 254

3. Basile I, Grousset FE, Revel M, Petit JR, Biscaye PE, Barkov NI (1997) Patagonian origin of glacial dust deposited in East Antarctica (Vostok and Dome C) during glacial stages 2, 4 and 6. Earth Planet Sci Lett 146: 573–589

4. Bogdanovski O (1997) Development of highly-sensitive techniques for Sm-Nd isotopic analysis and their application to the study of terrestrial and extraterrestrial objects. PhD Thesis, Cosmochemistry Department Max Plank Institute, Johannes Gutenberg Universitat, Mainz, Germany

5. Briat M, Royer A, Petit JR, Lorius C (1982) Late glacial input of eolian continental dust in the Dome C ice core: additional evidence from individual microparticle analysis. Ann Glaciol 3: 27–30

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