Ice-core records of biomass burning

Research output: Contribution to journal › Article › peer-review

Standard

Ice-core records of biomass burning. / Rubino, M.; D'onofrio, A.; Seki, O.; Bendle, J. A.

In: The Anthropocene Review, Vol. 3, No. 2, 01.08.2016, p. 140-162.

Research output: Contribution to journal › Article › peer-review

Harvard

Rubino, M, D'onofrio, A, Seki, O & Bendle, JA 2016, 'Ice-core records of biomass burning', The Anthropocene Review, vol. 3, no. 2, pp. 140-162. https://doi.org/10.1177/2053019615605117

APA

Rubino, M., D'onofrio, A., Seki, O., & Bendle, J. A. (2016). Ice-core records of biomass burning. The Anthropocene Review, 3(2), 140-162. https://doi.org/10.1177/2053019615605117

Vancouver

Rubino M, D'onofrio A, Seki O, Bendle JA. Ice-core records of biomass burning. The Anthropocene Review. 2016 Aug 1;3(2):140-162. https://doi.org/10.1177/2053019615605117

Author

Rubino, M. ; D'onofrio, A. ; Seki, O. ; Bendle, J. A. / Ice-core records of biomass burning. In: The Anthropocene Review. 2016 ; Vol. 3, No. 2. pp. 140-162.

Bibtex

@article{ba7022b77dad47068326c981320becbb,
title = "Ice-core records of biomass burning",
abstract = "We review the approaches for estimating biomass burning from ice-cores and consider the challenges and assumptions in their application. In particular, we consider the potential of biomarker proxies for biomass burning, hitherto not widely applied to glacial ice archives. We also review the available records of biomass burning in ice-cores and consider how variations in fire regimes have been related to atmospheric and land-use changes. Finally, we suggest that future developments in ice-core science should aim to combine multiple biomarkers with other records (black carbon, charcoal) and models to discern the types of material being burnt (C3 versus C4 plants, angiosperms, gymnosperms, peat fires, etc.) and to improve constraints on source areas of biomass burning. An ultimate goal is to compare the biomass burning record from ice-cores with hindcasts from models to project how future climate change will influence biomass burning and, inversely, how fire will affect climate.",
keywords = "ammonium, carboxylic acids, dehydroabietic acid, δ13C-CH4, δ18O-CO, formate, levoglucosan, nitrate, vanillic acid",
author = "M. Rubino and A. D'onofrio and O. Seki and Bendle, {J. A.}",
year = "2016",
month = aug,
day = "1",
doi = "10.1177/2053019615605117",
language = "English",
volume = "3",
pages = "140--162",
journal = "The Anthropocene Review",
issn = "2053-0196",
publisher = "SAGE Publications",
number = "2",

}

RIS

TY - JOUR

T1 - Ice-core records of biomass burning

AU - Rubino, M.

AU - D'onofrio, A.

AU - Seki, O.

AU - Bendle, J. A.

PY - 2016/8/1

Y1 - 2016/8/1

N2 - We review the approaches for estimating biomass burning from ice-cores and consider the challenges and assumptions in their application. In particular, we consider the potential of biomarker proxies for biomass burning, hitherto not widely applied to glacial ice archives. We also review the available records of biomass burning in ice-cores and consider how variations in fire regimes have been related to atmospheric and land-use changes. Finally, we suggest that future developments in ice-core science should aim to combine multiple biomarkers with other records (black carbon, charcoal) and models to discern the types of material being burnt (C3 versus C4 plants, angiosperms, gymnosperms, peat fires, etc.) and to improve constraints on source areas of biomass burning. An ultimate goal is to compare the biomass burning record from ice-cores with hindcasts from models to project how future climate change will influence biomass burning and, inversely, how fire will affect climate.

AB - We review the approaches for estimating biomass burning from ice-cores and consider the challenges and assumptions in their application. In particular, we consider the potential of biomarker proxies for biomass burning, hitherto not widely applied to glacial ice archives. We also review the available records of biomass burning in ice-cores and consider how variations in fire regimes have been related to atmospheric and land-use changes. Finally, we suggest that future developments in ice-core science should aim to combine multiple biomarkers with other records (black carbon, charcoal) and models to discern the types of material being burnt (C3 versus C4 plants, angiosperms, gymnosperms, peat fires, etc.) and to improve constraints on source areas of biomass burning. An ultimate goal is to compare the biomass burning record from ice-cores with hindcasts from models to project how future climate change will influence biomass burning and, inversely, how fire will affect climate.

KW - ammonium

KW - carboxylic acids

KW - dehydroabietic acid

KW - δ13C-CH4

KW - δ18O-CO

KW - formate

KW - levoglucosan

KW - nitrate

KW - vanillic acid

U2 - 10.1177/2053019615605117

DO - 10.1177/2053019615605117

M3 - Article

VL - 3

SP - 140

EP - 162

JO - The Anthropocene Review

JF - The Anthropocene Review

SN - 2053-0196

IS - 2

ER -