Hemispheric black carbon increase after the 13th-century Māori arrival in New Zealand-Reference-Cited by-同舟云学术

Hemispheric black carbon increase after the 13th-century Māori arrival in New Zealand

Published:2021-10-06 Issue:7879 Volume:598 Page:82-85
ISSN:0028-0836
Container-title:Nature
language:en
Short-container-title:Nature

Author:

McConnell Joseph R.^ORCID,Chellman Nathan J.,Mulvaney Robert,Eckhardt Sabine,Stohl Andreas,Plunkett Gill^ORCID,Kipfstuhl Sepp,Freitag Johannes,Isaksson Elisabeth,Gleason Kelly E.,Brugger Sandra O.,McWethy David B.,Abram Nerilie J.^ORCID,Liu Pengfei,Aristarain Alberto J.

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

https://www.nature.com/articles/s41586-021-03858-9.pdf

Reference51 articles.

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2. McWethy, D. B. et al. Rapid landscape transformation in South Island, New Zealand, following initial Polynesian settlement. Proc. Natl Acad. Sci. USA 107, 21343–21348 (2010).

3. Walter, R., Buckley, H., Jacomb, C. & Matisoo-Smith, E. Mass migration and the Polynesian settlement of New Zealand. J. World Prehistory 30, 351–376 (2017).

4. Remer, L. A. et al. Global aerosol climatology from the MODIS satellite sensors. J. Geophys. Res. Atmos. 113, D14S07 (2008).

5. Stohl, A., Forster, C., Frank, A., Seibert, P. & Wotawa, G. Technical note: the Lagrangian particle dispersion model FLEXPART version 6.2. Atmos. Chem. Phys. 5, 2461–2474 (2005).

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