Carbonaceous particles reveal that Late Holocene dust causes the dark region in the western ablation zone of the Greenland ice sheet

Wientjes, I.G.M.; De Van Wal, R.S.W.; Schwikowski, M.; Zapf, A.; Fahrni, S.; Wacker, L. (2012). Carbonaceous particles reveal that Late Holocene dust causes the dark region in the western ablation zone of the Greenland ice sheet. Journal of glaciology, 58(210), pp. 787-794. Cambridge: International Glaciological Society 10.3189/2012JoG11J165

Full text not available from this repository. (Request a copy)

Item Type:

Journal Article (Original Article)

Division/Institute:

08 Faculty of Science > Department of Chemistry, Biochemistry and Pharmaceutical Sciences (DCBP)

UniBE Contributor:

Schwikowski, Margit

ISSN:

0022-1430

Publisher:

International Glaciological Society

Language:

English

Submitter:

Factscience Import

Date Deposited:

04 Oct 2013 14:38

Last Modified:

05 Dec 2022 14:12

Publisher DOI:

10.3189/2012JoG11J165

Web of Science ID:

000307208200016

URI:

https://boris.unibe.ch/id/eprint/15408 (FactScience: 222748)

Actions (login required)

Edit item Edit item
Provide Feedback