Isoprene emissions from a tundra ecosystem
Whole-system fluxes of isoprene from a moist acidic tundra ecosystem and leaf-level emission rates of isoprene from a common species ( Salix pulchra ) in that same ecosystem were measured during three separate field campaigns. The field campaigns were conducted during the summers of 2005, 2010 and 2...
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ftdoajarticles:oai:doaj.org/article:506cff1b2238442c884d537ed0286af0 2023-05-15T15:00:49+02:00 Isoprene emissions from a tundra ecosystem M. J. Potosnak B. M. Baker L. LeStourgeon S. M. Disher K. L. Griffin M. S. Bret-Harte G. Starr 2013-02-01T00:00:00Z https://doi.org/10.5194/bg-10-871-2013 https://doaj.org/article/506cff1b2238442c884d537ed0286af0 EN eng Copernicus Publications http://www.biogeosciences.net/10/871/2013/bg-10-871-2013.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-10-871-2013 1726-4170 1726-4189 https://doaj.org/article/506cff1b2238442c884d537ed0286af0 Biogeosciences, Vol 10, Iss 2, Pp 871-889 (2013) Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 article 2013 ftdoajarticles https://doi.org/10.5194/bg-10-871-2013 2022-12-31T12:18:16Z Whole-system fluxes of isoprene from a moist acidic tundra ecosystem and leaf-level emission rates of isoprene from a common species ( Salix pulchra ) in that same ecosystem were measured during three separate field campaigns. The field campaigns were conducted during the summers of 2005, 2010 and 2011 and took place at the Toolik Field Station (68.6° N, 149.6° W) on the north slope of the Brooks Range in Alaska, USA. The maximum rate of whole-system isoprene flux measured was over 1.2 mg C m −2 h −1 with an air temperature of 22 °C and a PAR level over 1500 μmol m −2 s −1 . Leaf-level isoprene emission rates for S. pulchra averaged 12.4 nmol m −2 s −1 (27.4 μg C gdw −1 h −1 ) extrapolated to standard conditions (PAR = 1000 μmol m −2 s −1 and leaf temperature = 30 °C). Leaf-level isoprene emission rates were well characterized by the Guenther algorithm for temperature with published coefficients, but less so for light. Chamber measurements from a nearby moist acidic tundra ecosystem with little S. pulchra emitted significant amounts of isoprene, but at lower rates (0.45 mg C m −2 h −1 ) suggesting other significant isoprene emitters. Comparison of our results to predictions from a global model found broad agreement, but a detailed analysis revealed some significant discrepancies. An atmospheric chemistry box model predicts that the observed isoprene emissions have a significant impact on Arctic atmospheric chemistry, including a reduction of hydroxyl radical (OH) concentrations. Our results support the prediction that isoprene emissions from Arctic ecosystems will increase with global climate change. Article in Journal/Newspaper Arctic Brooks Range Climate change north slope Tundra Alaska Directory of Open Access Journals: DOAJ Articles Arctic Biogeosciences 10 2 871 889 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
spellingShingle |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 M. J. Potosnak B. M. Baker L. LeStourgeon S. M. Disher K. L. Griffin M. S. Bret-Harte G. Starr Isoprene emissions from a tundra ecosystem |
topic_facet |
Ecology QH540-549.5 Life QH501-531 Geology QE1-996.5 |
description |
Whole-system fluxes of isoprene from a moist acidic tundra ecosystem and leaf-level emission rates of isoprene from a common species ( Salix pulchra ) in that same ecosystem were measured during three separate field campaigns. The field campaigns were conducted during the summers of 2005, 2010 and 2011 and took place at the Toolik Field Station (68.6° N, 149.6° W) on the north slope of the Brooks Range in Alaska, USA. The maximum rate of whole-system isoprene flux measured was over 1.2 mg C m −2 h −1 with an air temperature of 22 °C and a PAR level over 1500 μmol m −2 s −1 . Leaf-level isoprene emission rates for S. pulchra averaged 12.4 nmol m −2 s −1 (27.4 μg C gdw −1 h −1 ) extrapolated to standard conditions (PAR = 1000 μmol m −2 s −1 and leaf temperature = 30 °C). Leaf-level isoprene emission rates were well characterized by the Guenther algorithm for temperature with published coefficients, but less so for light. Chamber measurements from a nearby moist acidic tundra ecosystem with little S. pulchra emitted significant amounts of isoprene, but at lower rates (0.45 mg C m −2 h −1 ) suggesting other significant isoprene emitters. Comparison of our results to predictions from a global model found broad agreement, but a detailed analysis revealed some significant discrepancies. An atmospheric chemistry box model predicts that the observed isoprene emissions have a significant impact on Arctic atmospheric chemistry, including a reduction of hydroxyl radical (OH) concentrations. Our results support the prediction that isoprene emissions from Arctic ecosystems will increase with global climate change. |
format |
Article in Journal/Newspaper |
author |
M. J. Potosnak B. M. Baker L. LeStourgeon S. M. Disher K. L. Griffin M. S. Bret-Harte G. Starr |
author_facet |
M. J. Potosnak B. M. Baker L. LeStourgeon S. M. Disher K. L. Griffin M. S. Bret-Harte G. Starr |
author_sort |
M. J. Potosnak |
title |
Isoprene emissions from a tundra ecosystem |
title_short |
Isoprene emissions from a tundra ecosystem |
title_full |
Isoprene emissions from a tundra ecosystem |
title_fullStr |
Isoprene emissions from a tundra ecosystem |
title_full_unstemmed |
Isoprene emissions from a tundra ecosystem |
title_sort |
isoprene emissions from a tundra ecosystem |
publisher |
Copernicus Publications |
publishDate |
2013 |
url |
https://doi.org/10.5194/bg-10-871-2013 https://doaj.org/article/506cff1b2238442c884d537ed0286af0 |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Brooks Range Climate change north slope Tundra Alaska |
genre_facet |
Arctic Brooks Range Climate change north slope Tundra Alaska |
op_source |
Biogeosciences, Vol 10, Iss 2, Pp 871-889 (2013) |
op_relation |
http://www.biogeosciences.net/10/871/2013/bg-10-871-2013.pdf https://doaj.org/toc/1726-4170 https://doaj.org/toc/1726-4189 doi:10.5194/bg-10-871-2013 1726-4170 1726-4189 https://doaj.org/article/506cff1b2238442c884d537ed0286af0 |
op_doi |
https://doi.org/10.5194/bg-10-871-2013 |
container_title |
Biogeosciences |
container_volume |
10 |
container_issue |
2 |
container_start_page |
871 |
op_container_end_page |
889 |
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1766332877850542080 |