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Effects of climate-induced changes in isoprene emissions after the eruption of Mount Pinatubo

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Effects of climate-induced changes in isoprene emissions after the eruption of Mount Pinatubo. / Telford, P. J.; Lathiere, Juliette; Abraham, N. L. et al.
In: Procedia Environmental Sciences, Vol. 6, 06.2011, p. 199-205.

Research output: Contribution to Journal/Magazine › Journal article › peer-review

Harvard

Telford, PJ, Lathiere, J, Abraham, NL, Archibald, AT, Braesicke, P, Johnson, CE, Morgenstern, O, O'Connor, FM, Pike, RC, Wild, O, Young, P, Beerling, DJ, Hewitt, CN & Pyle, JA 2011, 'Effects of climate-induced changes in isoprene emissions after the eruption of Mount Pinatubo', Procedia Environmental Sciences, vol. 6, pp. 199-205. https://doi.org/10.1016/j.proenv.2011.05.021

APA

Telford, P. J., Lathiere, J., Abraham, N. L., Archibald, A. T., Braesicke, P., Johnson, C. E., Morgenstern, O., O'Connor, F. M., Pike, R. C., Wild, O., Young, P., Beerling, D. J., Hewitt, C. N., & Pyle, J. A. (2011). Effects of climate-induced changes in isoprene emissions after the eruption of Mount Pinatubo. Procedia Environmental Sciences, 6, 199-205. https://doi.org/10.1016/j.proenv.2011.05.021

Vancouver

Telford PJ, Lathiere J, Abraham NL, Archibald AT, Braesicke P, Johnson CE et al. Effects of climate-induced changes in isoprene emissions after the eruption of Mount Pinatubo. Procedia Environmental Sciences. 2011 Jun;6:199-205. doi: 10.1016/j.proenv.2011.05.021

Author

Telford, P. J. ; Lathiere, Juliette ; Abraham, N. L. et al. / Effects of climate-induced changes in isoprene emissions after the eruption of Mount Pinatubo. In: Procedia Environmental Sciences. 2011 ; Vol. 6. pp. 199-205.

Bibtex

@article{256bd39b2a8e43438537d4b876e1a7a0,
title = "Effects of climate-induced changes in isoprene emissions after the eruption of Mount Pinatubo",
abstract = "The eruption of Mt. Pinatubo in June 1991 was the largest in the twentieth century. One of its effects was to produce cooler and drier conditions in the years following the eruption. We present the results of an integrated model study of the effect of these climatic changes on the emissions of isoprene from the biosphere. Our emissions model simulations showed that global isoprene emissions were reduced by 9% from 1990 to 1992. When incorporated into our model of global atmospheric chemistry this reduction of isoprene emissions led to an increase in the tropospheric OH burden of 2%. This caused an increase in the removal of methane via oxidation by OH of up to 5 Tg per year. This could have contributed to the observed changes in methane growth rate at this time.",
keywords = "Pinatubo, isoprene , biogenic emissions , oxidising capacity , methane",
author = "Telford, {P. J.} and Juliette Lathiere and Abraham, {N. L.} and Archibald, {A. T.} and P. Braesicke and Johnson, {C. E.} and O. Morgenstern and O'Connor, {F. M.} and Pike, {R. C.} and Oliver Wild and Paul Young and Beerling, {D. J.} and Hewitt, {C. N.} and Pyle, {J. A.}",
year = "2011",
month = jun,
doi = "10.1016/j.proenv.2011.05.021",
language = "English",
volume = "6",
pages = "199--205",
journal = "Procedia Environmental Sciences",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Effects of climate-induced changes in isoprene emissions after the eruption of Mount Pinatubo

AU - Telford, P. J.

AU - Lathiere, Juliette

AU - Abraham, N. L.

AU - Archibald, A. T.

AU - Braesicke, P.

AU - Johnson, C. E.

AU - Morgenstern, O.

AU - O'Connor, F. M.

AU - Pike, R. C.

AU - Wild, Oliver

AU - Young, Paul

AU - Beerling, D. J.

AU - Hewitt, C. N.

AU - Pyle, J. A.

PY - 2011/6

Y1 - 2011/6

N2 - The eruption of Mt. Pinatubo in June 1991 was the largest in the twentieth century. One of its effects was to produce cooler and drier conditions in the years following the eruption. We present the results of an integrated model study of the effect of these climatic changes on the emissions of isoprene from the biosphere. Our emissions model simulations showed that global isoprene emissions were reduced by 9% from 1990 to 1992. When incorporated into our model of global atmospheric chemistry this reduction of isoprene emissions led to an increase in the tropospheric OH burden of 2%. This caused an increase in the removal of methane via oxidation by OH of up to 5 Tg per year. This could have contributed to the observed changes in methane growth rate at this time.

AB - The eruption of Mt. Pinatubo in June 1991 was the largest in the twentieth century. One of its effects was to produce cooler and drier conditions in the years following the eruption. We present the results of an integrated model study of the effect of these climatic changes on the emissions of isoprene from the biosphere. Our emissions model simulations showed that global isoprene emissions were reduced by 9% from 1990 to 1992. When incorporated into our model of global atmospheric chemistry this reduction of isoprene emissions led to an increase in the tropospheric OH burden of 2%. This caused an increase in the removal of methane via oxidation by OH of up to 5 Tg per year. This could have contributed to the observed changes in methane growth rate at this time.

KW - Pinatubo

KW - isoprene

KW - biogenic emissions

KW - oxidising capacity

KW - methane

U2 - 10.1016/j.proenv.2011.05.021

DO - 10.1016/j.proenv.2011.05.021

M3 - Journal article

VL - 6

SP - 199

EP - 205

JO - Procedia Environmental Sciences

JF - Procedia Environmental Sciences

ER -