Strong isoprene emission response to temperature in tundra vegetation

Emissions of biogenic volatile organic compounds (BVOCs) are a crucial component of biosphere-atmosphere interactions. In northern latitudes, climate change is amplified by feedback processes in which BVOCs have a recognized, yet poorly quantified role, mainly due to a lack of measurements and concomitant modeling gaps. Hence, current Earth system models mostly rely on temperature responses measured on vegetation from lower latitudes, rendering their predictions highly uncertain. Here, we show how tundra isoprene emissions respond vigorously to temperature increases, compared to model results. Our unique dataset of direct eddy covariance ecosystem-level isoprene measurements in two contrasting ecosystems exhibited Q10 (the factor by which the emission rate increases with a 10 °C rise in temperature) temperature coefficients of up to 20.8, that is, 3.5 times the Q10 of 5.9 derived from the equivalent model calculations. Crude estimates using the observed temperature responses indicate that tundra vegetation could enhance their isoprene emissions by up to 41% (87%)-that is, 46% (55%) more than estimated by models-with a 2 °C (4 °C) warming. Our results demonstrate that tundra vegetation possesses the potential to substantially boost its isoprene emissions in response to future rising temperatures, at rates that exceed the current Earth system model predictions.

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Bibliographic Details
Main Authors: Seco, Roger, Holst, Thomas, Davie-Martin, Cleo L., Simin, Tihomir, Guenther, Alex, Pirk, Norbert, Rinne, Janne, Rinnan, Riikka
Other Authors: Ministerio de Ciencia e Innovación (España)
Format: artículo biblioteca
Language:English
Published: National Academy of Sciences (U.S.) 2022-09-20
Subjects:Temperature response, VOC emission modeling, Biogenic volatile organic compound fluxes, Biosphere–atmosphere interactions, Eddy covariance,
Online Access:http://hdl.handle.net/10261/279837
http://dx.doi.org/10.13039/501100004837
https://api.elsevier.com/content/abstract/scopus_id/85137676507
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id dig-idaea-es-10261-279837
record_format koha
institution IDAEA ES
collection DSpace
country España
countrycode ES
component Bibliográfico
access En linea
databasecode dig-idaea-es
tag biblioteca
region Europa del Sur
libraryname Biblioteca del IDAEA España
language English
topic Temperature response
VOC emission modeling
Biogenic volatile organic compound fluxes
Biosphere–atmosphere interactions
Eddy covariance
Temperature response
VOC emission modeling
Biogenic volatile organic compound fluxes
Biosphere–atmosphere interactions
Eddy covariance
spellingShingle Temperature response
VOC emission modeling
Biogenic volatile organic compound fluxes
Biosphere–atmosphere interactions
Eddy covariance
Temperature response
VOC emission modeling
Biogenic volatile organic compound fluxes
Biosphere–atmosphere interactions
Eddy covariance
Seco, Roger
Holst, Thomas
Davie-Martin, Cleo L.
Simin, Tihomir
Guenther, Alex
Pirk, Norbert
Rinne, Janne
Rinnan, Riikka
Strong isoprene emission response to temperature in tundra vegetation
description Emissions of biogenic volatile organic compounds (BVOCs) are a crucial component of biosphere-atmosphere interactions. In northern latitudes, climate change is amplified by feedback processes in which BVOCs have a recognized, yet poorly quantified role, mainly due to a lack of measurements and concomitant modeling gaps. Hence, current Earth system models mostly rely on temperature responses measured on vegetation from lower latitudes, rendering their predictions highly uncertain. Here, we show how tundra isoprene emissions respond vigorously to temperature increases, compared to model results. Our unique dataset of direct eddy covariance ecosystem-level isoprene measurements in two contrasting ecosystems exhibited Q10 (the factor by which the emission rate increases with a 10 °C rise in temperature) temperature coefficients of up to 20.8, that is, 3.5 times the Q10 of 5.9 derived from the equivalent model calculations. Crude estimates using the observed temperature responses indicate that tundra vegetation could enhance their isoprene emissions by up to 41% (87%)-that is, 46% (55%) more than estimated by models-with a 2 °C (4 °C) warming. Our results demonstrate that tundra vegetation possesses the potential to substantially boost its isoprene emissions in response to future rising temperatures, at rates that exceed the current Earth system model predictions.
author2 Ministerio de Ciencia e Innovación (España)
author_facet Ministerio de Ciencia e Innovación (España)
Seco, Roger
Holst, Thomas
Davie-Martin, Cleo L.
Simin, Tihomir
Guenther, Alex
Pirk, Norbert
Rinne, Janne
Rinnan, Riikka
format artículo
topic_facet Temperature response
VOC emission modeling
Biogenic volatile organic compound fluxes
Biosphere–atmosphere interactions
Eddy covariance
author Seco, Roger
Holst, Thomas
Davie-Martin, Cleo L.
Simin, Tihomir
Guenther, Alex
Pirk, Norbert
Rinne, Janne
Rinnan, Riikka
author_sort Seco, Roger
title Strong isoprene emission response to temperature in tundra vegetation
title_short Strong isoprene emission response to temperature in tundra vegetation
title_full Strong isoprene emission response to temperature in tundra vegetation
title_fullStr Strong isoprene emission response to temperature in tundra vegetation
title_full_unstemmed Strong isoprene emission response to temperature in tundra vegetation
title_sort strong isoprene emission response to temperature in tundra vegetation
publisher National Academy of Sciences (U.S.)
publishDate 2022-09-20
url http://hdl.handle.net/10261/279837
http://dx.doi.org/10.13039/501100004837
https://api.elsevier.com/content/abstract/scopus_id/85137676507
work_keys_str_mv AT secoroger strongisopreneemissionresponsetotemperatureintundravegetation
AT holstthomas strongisopreneemissionresponsetotemperatureintundravegetation
AT daviemartincleol strongisopreneemissionresponsetotemperatureintundravegetation
AT simintihomir strongisopreneemissionresponsetotemperatureintundravegetation
AT guentheralex strongisopreneemissionresponsetotemperatureintundravegetation
AT pirknorbert strongisopreneemissionresponsetotemperatureintundravegetation
AT rinnejanne strongisopreneemissionresponsetotemperatureintundravegetation
AT rinnanriikka strongisopreneemissionresponsetotemperatureintundravegetation
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spelling dig-idaea-es-10261-2798372024-10-28T21:42:10Z Strong isoprene emission response to temperature in tundra vegetation Seco, Roger Holst, Thomas Davie-Martin, Cleo L. Simin, Tihomir Guenther, Alex Pirk, Norbert Rinne, Janne Rinnan, Riikka Ministerio de Ciencia e Innovación (España) 0000-0002-2078-9956 0000-0002-3360-9395 0000-0002-3710-8715 0000-0002-3914-500X 0000-0002-8137-2329 0000-0003-1168-7138 0000-0001-7222-700X Consejo Superior de Investigaciones Científicas [https://ror.org/02gfc7t72] Temperature response VOC emission modeling Biogenic volatile organic compound fluxes Biosphere–atmosphere interactions Eddy covariance Emissions of biogenic volatile organic compounds (BVOCs) are a crucial component of biosphere-atmosphere interactions. In northern latitudes, climate change is amplified by feedback processes in which BVOCs have a recognized, yet poorly quantified role, mainly due to a lack of measurements and concomitant modeling gaps. Hence, current Earth system models mostly rely on temperature responses measured on vegetation from lower latitudes, rendering their predictions highly uncertain. Here, we show how tundra isoprene emissions respond vigorously to temperature increases, compared to model results. Our unique dataset of direct eddy covariance ecosystem-level isoprene measurements in two contrasting ecosystems exhibited Q10 (the factor by which the emission rate increases with a 10 °C rise in temperature) temperature coefficients of up to 20.8, that is, 3.5 times the Q10 of 5.9 derived from the equivalent model calculations. Crude estimates using the observed temperature responses indicate that tundra vegetation could enhance their isoprene emissions by up to 41% (87%)-that is, 46% (55%) more than estimated by models-with a 2 °C (4 °C) warming. Our results demonstrate that tundra vegetation possesses the potential to substantially boost its isoprene emissions in response to future rising temperatures, at rates that exceed the current Earth system model predictions. We are grateful to ICOS Sweden, the Abisko Scientific Research Station (ANS), and the Finse Alpine Research Centre for providing excellent logistics for the work, and we are grateful in particular to Mikkel Sillesen Matzen, John Hulth, Andreas Westergaard-Nielsen, and Rune Maigaard for field assistance and to Jutta Holst for assistance with data. High-frequency wind data from Abisko were provided by ICOS Sweden, which has been cofinanced by the Swedish Research Council (grant 2019-00205); Abisko-Stordalen has been hosted by ANS and SITES "Swedish Infrastructure for Ecosystem Sciences" (cofinanced by the Swedish Research Council). This research has been supported by the European Research Council (TUVOLU "Tundra Biogenic Volatile Emissions in the 21st Century", grant 771012) under the European Union’s Horizon 2020 research and innovation program, the Independent Research Fund Denmark/Natural Sciences (grant DFF–4181-00141), and the Danish National Research Foundation (CENPERM grant DNRF100). R.S. acknowledges a Ramón y Cajal grant (RYC2020-029216-I) funded by the Spanish Ministry of Science and Innovation and the State Research Agency (MCIN/AEI/10.13039/501100011033) and by the European Social Fund “ESF Investing in Your Future”. IDAEA-CSIC is a Severo Ochoa Centre of Research Excellence (MCIN/AEI, project CEX2018-000794-S). This work is a contribution to the strategic research initiative LATICE "Land–ATmosphere Interactions in Cold Environments" (Faculty of Mathematics and Natural Sciences, University of Oslo, project UiO/GEO103920) and was supported by the EMERALD "Terrestrial ecosystem–climate interactions of our EMERALD planet" project funded by the Research Council of Norway (project 294948). Peer reviewed 2022-09-26T09:20:17Z 2022-09-26T09:20:17Z 2022-09-20 artículo http://purl.org/coar/resource_type/c_6501 Proceedings of the National Academy of Sciences of the United States of America 119 (38) e2118014119 (2022) http://hdl.handle.net/10261/279837 10.1073/pnas.2118014119 http://dx.doi.org/10.13039/501100004837 36095176 2-s2.0-85137676507 https://api.elsevier.com/content/abstract/scopus_id/85137676507 en #PLACEHOLDER_PARENT_METADATA_VALUE# info:eu-repo/grantAgreement/MCIN/AEI/10.13039/501100011033 Proceedings of the National Academy of Sciences of the United States of America Publisher's version https://doi.org/10.1073/pnas.2118014119 Sí open National Academy of Sciences (U.S.)