Articles | Volume 20, issue 1
Atmos. Chem. Phys., 20, 597–612, 2020
https://doi.org/10.5194/acp-20-597-2020
Atmos. Chem. Phys., 20, 597–612, 2020
https://doi.org/10.5194/acp-20-597-2020

Research article 17 Jan 2020

Research article | 17 Jan 2020

Ice core records of levoglucosan and dehydroabietic and vanillic acids from Aurora Peak in Alaska since the 1660s: a proxy signal of biomass-burning activities in the North Pacific Rim

Ambarish Pokhrel et al.

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Svenja Lange on behalf of the Authors (13 Sep 2019)  Author's response
ED: Publish as is (16 Oct 2019) by Carlo Barbante
AR by Ambarish Pokhrel on behalf of the Authors (23 Oct 2019)  Author's response    Manuscript
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Short summary
A 180 m long (ca. 274 year) ice core was drilled in the saddle of the Aurora Peak in Alaska (63.52° N, 146.54° W; elevation: 2,825 m). The ice core samples were derived with O-bis-(trimethylsilyl)trifluoroacetamide with 1 % trimethylsilyl chloride and pyridine followed by gas-chromatography–mass-spectrometry analyses. Levoglucosan, dehydroabietic acid and vanillic acid are reported for the first time from the alpine glacier to better understand historical biomass burning.
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