Compositions of Dust and Sea Salts in the Dome C and Dome Fuji Ice Cores From Last Glacial Maximum to Early Holocene Based on Ice‐Sublimation and Single‐Particle Measurements-Reference-Cited by-同舟云学术

Compositions of Dust and Sea Salts in the Dome C and Dome Fuji Ice Cores From Last Glacial Maximum to Early Holocene Based on Ice‐Sublimation and Single‐Particle Measurements

Published:2020-02-22 Issue:4 Volume:125 Page:
ISSN:2169-897X
Container-title:Journal of Geophysical Research: Atmospheres
language:en
Short-container-title:J. Geophys. Res. Atmos.

Author:

Oyabu I.¹²³^ORCID,Iizuka Y.²^ORCID,Kawamura K.¹⁴⁵^ORCID,Wolff E.⁶^ORCID,Severi M.⁷,Ohgaito R.⁸^ORCID,Abe‐Ouchi A.¹⁸⁹^ORCID,Hansson M.³

Affiliation:

1. National Institute of Polar Research Research Organization of Information and Systems Tokyo Japan

2. Institute of Low Temperature Science Hokkaido University Sapporo Japan

3. Department of Physical Geography Stockholm University Stockholm Sweden

4. Department of Polar Science The Graduate University of Advanced Studies (SOKENDAI) Tokyo Japan

5. Japan Agency for Marine Science and Technology (JAMSTEC) Yokosuka Japan

6. Department of Earth Sciences University of Cambridge Cambridge UK

7. Department of Chemistry “Ugo Schiff” University of Florence Florence Italy

8. Japan Agency for Marine‐Earth Science and Technology Yokohama Japan

9. Atmosphere Ocean Research Institute University of Tokyo Kashiwa Japan

Funder

Japan Society for the Promotion of Science

Royal Society

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2019JD032208

Reference92 articles.

1. Comparing modeled and observed changes in mineral dust transport and deposition to Antarctica between the Last Glacial Maximum and current climates

2. Patagonian origin of glacial dust deposited in East Antarctica (Vostok and Dome C) during glacial stages 2, 4 and 6

3. Aerosol deposited in East Antarctica over the last glacial cycle: Detailed apportionment of continental and sea-salt contributions

4. Optimization of High-Resolution Continuous Flow Analysis for Transient Climate Signals in Ice Cores

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