Light limitation regulates the response of autumn terrestrial carbon uptake to warming
Global warming is projected to shift the phenology and increase the productivity of northern ecosystems 1 – 6 . Both changes will further feed back to climate through biophysical and biogeochemical processes and are critical for future prediction 7 , 8 . However, it remains unclear whether warming a...
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Published in | Nature climate change Vol. 10; no. 8; pp. 739 - 743 |
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Main Authors | , , , , |
Format | Journal Article |
Language | English |
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Nature Publishing Group UK
01.08.2020
Nature Publishing Group |
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Abstract | Global warming is projected to shift the phenology and increase the productivity of northern ecosystems
1
–
6
. Both changes will further feed back to climate through biophysical and biogeochemical processes and are critical for future prediction
7
,
8
. However, it remains unclear whether warming and the extended growing season, especially in autumn, would lead to increased net ecosystem carbon uptake
9
,
10
. Here we analyse satellite observations, field measurements and model simulations and show a prevalent radiation limitation on carbon uptake in northern ecosystems, especially in autumn. By comparing the start and end of the growing season estimated from vegetation indices and from solar-induced chlorophyll fluorescence (a proxy for gross primary production
11
,
12
(GPP)), we find a greater change in greenness-based start and end of season than that from GPP, mostly caused by the radiation limitation on photosynthesis. This radiation limitation explains the contrasting responses of autumn net carbon exchanges to warming, using both eddy covariance measurements and model simulations from Coupled Model Intercomparison Project Phase 5. Regions with weak radiation limitation benefit more from warming and enhanced vegetation greenness in autumn, where GPP increases can outweigh the warming-induced respiration carbon losses. With continued warming, radiation limitation will increase and exert a strong upper bound on northern ecosystems to act as carbon sinks.
Phenological shifts due to warming extend the growing season for plants, with implications for ecosystem productivity. Carbon uptake through photosynthesis is limited by radiation, particularly in autumn, which explains contrasting regional responses of autumn carbon uptake to rising temperatures. |
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AbstractList | Global warming is projected to shift the phenology and increase the productivity of northern ecosystems1–6. Both changes will further feed back to climate through biophysical and biogeochemical processes and are critical for future prediction7,8. However, it remains unclear whether warming and the extended growing season, especially in autumn, would lead to increased net ecosystem carbon uptake9,10. Here we analyse satellite observations, field measurements and model simulations and show a prevalent radiation limitation on carbon uptake in northern ecosystems, especially in autumn. By comparing the start and end of the growing season estimated from vegetation indices and from solar-induced chlorophyll fluorescence (a proxy for gross primary production11,12 (GPP)), we find a greater change in greenness-based start and end of season than that from GPP, mostly caused by the radiation limitation on photosynthesis. This radiation limitation explains the contrasting responses of autumn net carbon exchanges to warming, using both eddy covariance measurements and model simulations from Coupled Model Intercomparison Project Phase 5. Regions with weak radiation limitation benefit more from warming and enhanced vegetation greenness in autumn, where GPP increases can outweigh the warming-induced respiration carbon losses. With continued warming, radiation limitation will increase and exert a strong upper bound on northern ecosystems to act as carbon sinks.Phenological shifts due to warming extend the growing season for plants, with implications for ecosystem productivity. Carbon uptake through photosynthesis is limited by radiation, particularly in autumn, which explains contrasting regional responses of autumn carbon uptake to rising temperatures. Global warming is projected to shift the phenology and increase the productivity of northern ecosystems 1 – 6 . Both changes will further feed back to climate through biophysical and biogeochemical processes and are critical for future prediction 7 , 8 . However, it remains unclear whether warming and the extended growing season, especially in autumn, would lead to increased net ecosystem carbon uptake 9 , 10 . Here we analyse satellite observations, field measurements and model simulations and show a prevalent radiation limitation on carbon uptake in northern ecosystems, especially in autumn. By comparing the start and end of the growing season estimated from vegetation indices and from solar-induced chlorophyll fluorescence (a proxy for gross primary production 11 , 12 (GPP)), we find a greater change in greenness-based start and end of season than that from GPP, mostly caused by the radiation limitation on photosynthesis. This radiation limitation explains the contrasting responses of autumn net carbon exchanges to warming, using both eddy covariance measurements and model simulations from Coupled Model Intercomparison Project Phase 5. Regions with weak radiation limitation benefit more from warming and enhanced vegetation greenness in autumn, where GPP increases can outweigh the warming-induced respiration carbon losses. With continued warming, radiation limitation will increase and exert a strong upper bound on northern ecosystems to act as carbon sinks. Phenological shifts due to warming extend the growing season for plants, with implications for ecosystem productivity. Carbon uptake through photosynthesis is limited by radiation, particularly in autumn, which explains contrasting regional responses of autumn carbon uptake to rising temperatures. |
Author | Commane, Róisín Williams, A. Park Gentine, Pierre Zhang, Yao Zhou, Sha |
Author_xml | – sequence: 1 givenname: Yao orcidid: 0000-0002-7468-2409 surname: Zhang fullname: Zhang, Yao email: zhangyaonju@gmail.com organization: Department of Earth and Environmental Engineering, Columbia University – sequence: 2 givenname: Róisín orcidid: 0000-0003-1373-1550 surname: Commane fullname: Commane, Róisín organization: Lamont–Doherty Earth Observatory of Columbia University – sequence: 3 givenname: Sha orcidid: 0000-0001-7161-5959 surname: Zhou fullname: Zhou, Sha organization: Department of Earth and Environmental Engineering, Columbia University, Lamont–Doherty Earth Observatory of Columbia University, Earth Institute, Columbia University – sequence: 4 givenname: A. Park surname: Williams fullname: Williams, A. Park organization: Lamont–Doherty Earth Observatory of Columbia University – sequence: 5 givenname: Pierre orcidid: 0000-0002-0845-8345 surname: Gentine fullname: Gentine, Pierre organization: Department of Earth and Environmental Engineering, Columbia University, Earth Institute, Columbia University |
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Snippet | Global warming is projected to shift the phenology and increase the productivity of northern ecosystems
1
–
6
. Both changes will further feed back to climate... Global warming is projected to shift the phenology and increase the productivity of northern ecosystems1–6. Both changes will further feed back to climate... |
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SubjectTerms | 704/158/2165 704/47 Autumn Biogeochemistry Carbon Carbon exchange Carbon sinks Carbon uptake Chlorophyll Chlorophylls Climate Change Climate Change/Climate Change Impacts Computer simulation Covariance Earth and Environmental Science Ecosystems Eddy covariance Environment Environmental Law/Policy/Ecojustice Fluorescence Global warming Growing season Intercomparison Letter Light effects Photosynthesis Productivity Radiation Satellite observation Seasons Temperature rise Upper bounds Uptake Vegetation |
Title | Light limitation regulates the response of autumn terrestrial carbon uptake to warming |
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