TY - JOUR

T1 - Seasonal and diel patterns of biogenic volatile organic compound fluxes in a subarctic tundra

AU - Li, Tao

AU - Baggesen, Nanna

AU - Seco, Roger

AU - Rinnan, Riikka

N1 - CENPERMOA[2023] Funding Information: The project was supported by the European Research Council (ERC) under the European Union’s Horizon 2020 research and innovation program (grant agreement No 771012 ), the Danish Council for Independent Research | Natural Sciences ( DFF–4181-00141 ), and the Danish National Research Foundation (Center for Permafrost, CENPERM DNRF100), as well as the Starting Research Fund of Sichuan University and the Fundamental Research Funds for the Central Universities (grant agreement SCU2021D006 ). RS acknowledges a Ramón y Cajal grant ( RYC2020-029216-I ) funded by MCIN/ AEI / 10.13039/501100011033 and by “ ESF Investing in your future”. IDAEA-CSIC is a Severo Ochoa Centre of Research Excellence (MCIN/ AEI , Project CEX2018-000794-S ). We would like to thank Anders Michelsen for maintaining the field site, Thomas Holst for the technical construction of the measurement setups, Cleo Davie-Martin for constructive comments and language revision, and the Swedish Polar Research Secretariat and SITES for the support of the work done at the Abisko Scientific Research Station. Funding Information: The project was supported by the European Research Council (ERC) under the European Union's Horizon 2020 research and innovation program (grant agreement No 771012), the Danish Council for Independent Research | Natural Sciences (DFF–4181-00141), and the Danish National Research Foundation (Center for Permafrost, CENPERM DNRF100), as well as the Starting Research Fund of Sichuan University and the Fundamental Research Funds for the Central Universities (grant agreement SCU2021D006). RS acknowledges a Ramón y Cajal grant (RYC2020-029216-I) funded by MCIN/AEI/10.13039/501100011033 and by “ESF Investing in your future”. IDAEA-CSIC is a Severo Ochoa Centre of Research Excellence (MCIN/AEI, Project CEX2018-000794-S). We would like to thank Anders Michelsen for maintaining the field site, Thomas Holst for the technical construction of the measurement setups, Cleo Davie-Martin for constructive comments and language revision, and the Swedish Polar Research Secretariat and SITES for the support of the work done at the Abisko Scientific Research Station. Publisher Copyright: © 2022 The Authors

PY - 2023

Y1 - 2023

N2 - In arctic and subarctic regions, rapid climate changes enhance biogenic volatile organic compound (BVOC) emissions from vegetation, with potentially significant influence on atmospheric processes. However, the seasonal and diel patterns of bidirectional exchange (flux) of BVOCs remain poorly studied in these regions. Here, we deployed a proton-transfer-reaction time-of-flight mass spectrometer (PTR-TOF-MS) to investigate ecosystem-level BVOC fluxes over a growing season in a subarctic tundra heath in Abisko, Northern Sweden, and to quantify BVOC emissions from two widespread dwarf shrubs in the high latitudes, Salix myrsinites and Betula nana. As expected, ecosystem fluxes of short-chained oxygenated compounds (e.g., methanol, acetaldehyde and acetone) and terpenoids (e.g., isoprene, monoterpenes and sesquiterpenes) followed different seasonal and diel patterns. For the short-chained oxygenated compounds, net emissions dominated and peaked in the early growing season, while net deposition occurred sporadically, particularly at night. In contrast, terpenoids were almost exclusively emitted from the ecosystem, with maxima occurring in the peak growing season. At the branch level, these compound groups were emitted from both S. myrsinites and B. nana in clear diel patterns with high emissions during the day. S. myrsinites was dominated by isoprene emissions whilst B. nana was dominated by terpene emissions. Methanol, acetaldehyde and acetone were emitted at comparable levels and similar patterns from both species. Both ecosystem fluxes and branch emissions responded exponentially to enclosure temperature and depended on light levels. Compared to the BVOC emission models, however, the temperature responses were steeper for isoprene, monoterpenes, methanol and acetone, but weaker for sesquiterpenes. Apart from the well-known compounds, many other BVOCs, such as some carbonyls and nitrogen-containing compounds, were emitted from both the ecosystem and plants with significant contributions to the season variation in ecosystem fluxes. Overall, our study highlights the complexity of subarctic ecosystem BVOC fluxes, which vary both seasonally and diurnally. Vegetation composition changes triggered by climate change will shift BVOC composition, with important implications for atmospheric processes and local climate.

AB - In arctic and subarctic regions, rapid climate changes enhance biogenic volatile organic compound (BVOC) emissions from vegetation, with potentially significant influence on atmospheric processes. However, the seasonal and diel patterns of bidirectional exchange (flux) of BVOCs remain poorly studied in these regions. Here, we deployed a proton-transfer-reaction time-of-flight mass spectrometer (PTR-TOF-MS) to investigate ecosystem-level BVOC fluxes over a growing season in a subarctic tundra heath in Abisko, Northern Sweden, and to quantify BVOC emissions from two widespread dwarf shrubs in the high latitudes, Salix myrsinites and Betula nana. As expected, ecosystem fluxes of short-chained oxygenated compounds (e.g., methanol, acetaldehyde and acetone) and terpenoids (e.g., isoprene, monoterpenes and sesquiterpenes) followed different seasonal and diel patterns. For the short-chained oxygenated compounds, net emissions dominated and peaked in the early growing season, while net deposition occurred sporadically, particularly at night. In contrast, terpenoids were almost exclusively emitted from the ecosystem, with maxima occurring in the peak growing season. At the branch level, these compound groups were emitted from both S. myrsinites and B. nana in clear diel patterns with high emissions during the day. S. myrsinites was dominated by isoprene emissions whilst B. nana was dominated by terpene emissions. Methanol, acetaldehyde and acetone were emitted at comparable levels and similar patterns from both species. Both ecosystem fluxes and branch emissions responded exponentially to enclosure temperature and depended on light levels. Compared to the BVOC emission models, however, the temperature responses were steeper for isoprene, monoterpenes, methanol and acetone, but weaker for sesquiterpenes. Apart from the well-known compounds, many other BVOCs, such as some carbonyls and nitrogen-containing compounds, were emitted from both the ecosystem and plants with significant contributions to the season variation in ecosystem fluxes. Overall, our study highlights the complexity of subarctic ecosystem BVOC fluxes, which vary both seasonally and diurnally. Vegetation composition changes triggered by climate change will shift BVOC composition, with important implications for atmospheric processes and local climate.

KW - BVOC fluxes

KW - Climate change

KW - Diurnal variations

KW - Dwarf shrub

KW - Ecosystem–atmosphere interactions

KW - Seasonal variations

KW - Subarctic tundra

U2 - 10.1016/j.atmosenv.2022.119430

DO - 10.1016/j.atmosenv.2022.119430

M3 - Journal article

AN - SCOPUS:85140273217

VL - 292

JO - Atmospheric Environment

JF - Atmospheric Environment

SN - 1352-2310

M1 - 119430

ER -