Interannual precipitation controls on soil CO2 fluxes in high elevation conifer and aspen forests

Long-term soil CO _2 emission measurements are necessary for detecting trends and interannual variability in the terrestrial carbon cycle. Such records are becoming increasingly valuable as ecosystems experience altered environmental conditions associated with climate change. From 2013 to 2021, we c...

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Main Authors: Mariah S Carbone, Andrew D Richardson, billy barr, Max Berkelhammer, Claudia M Boot, Austin Simonpietri, Christopher J Still
Format: Article
Language:English
Published: IOP Publishing 2023-01-01
Series:Environmental Research Letters
Subjects:
Online Access:https://doi.org/10.1088/1748-9326/ad07b5
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author Mariah S Carbone
Andrew D Richardson
billy barr
Max Berkelhammer
Claudia M Boot
Austin Simonpietri
Christopher J Still
author_facet Mariah S Carbone
Andrew D Richardson
billy barr
Max Berkelhammer
Claudia M Boot
Austin Simonpietri
Christopher J Still
author_sort Mariah S Carbone
collection DOAJ
description Long-term soil CO _2 emission measurements are necessary for detecting trends and interannual variability in the terrestrial carbon cycle. Such records are becoming increasingly valuable as ecosystems experience altered environmental conditions associated with climate change. From 2013 to 2021, we continuously measured soil CO _2 concentrations in the two dominant high elevation forest types, mixed conifer and aspen, in the upper Colorado River basin. We quantified the soil CO _2 flux during the summer months, and found that the mean and total CO _2 flux in both forests was related to the prior winter’s snowfall and current summer’s rainfall, with greater sensitivity to rainfall. We observed a decline in surface soil CO _2 production, which we attributed to warming and a decrease in amount and frequency of summer rains. Our results demonstrate strong precipitation control on the soil CO _2 flux in mountainous regions, a finding which has important implications for carbon cycling under future environmental change.
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spelling doaj.art-b77dfc84a92b4a0bb4b74a37a119a8782023-11-07T07:52:36ZengIOP PublishingEnvironmental Research Letters1748-93262023-01-01181212400910.1088/1748-9326/ad07b5Interannual precipitation controls on soil CO2 fluxes in high elevation conifer and aspen forestsMariah S Carbone0https://orcid.org/0000-0002-7832-7009Andrew D Richardson1https://orcid.org/0000-0002-0148-6714billy barr2Max Berkelhammer3https://orcid.org/0000-0002-8924-716XClaudia M Boot4https://orcid.org/0000-0002-1487-242XAustin Simonpietri5https://orcid.org/0000-0001-6671-1487Christopher J Still6https://orcid.org/0000-0002-8295-4494Center for Ecosystem Science and Society, Northern Arizona University , Flagstaff, AZ, United States of America; Rocky Mountain Biological Laboratory , Gothic, CO, United States of AmericaCenter for Ecosystem Science and Society, Northern Arizona University , Flagstaff, AZ, United States of America; School of Informatics, Computing, and Cyber Systems, Northern Arizona University , Flagstaff, AZ, United States of AmericaRocky Mountain Biological Laboratory , Gothic, CO, United States of AmericaRocky Mountain Biological Laboratory , Gothic, CO, United States of America; Department of Earth and Environmental Sciences, University of Illinois , Chicago, IL, United States of AmericaDepartment of Chemistry and Natural Resource Ecology Laboratory, Colorado State University , Fort Collins, CO, United States of AmericaCenter for Ecosystem Science and Society, Northern Arizona University , Flagstaff, AZ, United States of America; Rocky Mountain Biological Laboratory , Gothic, CO, United States of AmericaRocky Mountain Biological Laboratory , Gothic, CO, United States of America; Department of Forest Ecosystems and Society, Oregon State University , Corvallis, OR, United States of AmericaLong-term soil CO _2 emission measurements are necessary for detecting trends and interannual variability in the terrestrial carbon cycle. Such records are becoming increasingly valuable as ecosystems experience altered environmental conditions associated with climate change. From 2013 to 2021, we continuously measured soil CO _2 concentrations in the two dominant high elevation forest types, mixed conifer and aspen, in the upper Colorado River basin. We quantified the soil CO _2 flux during the summer months, and found that the mean and total CO _2 flux in both forests was related to the prior winter’s snowfall and current summer’s rainfall, with greater sensitivity to rainfall. We observed a decline in surface soil CO _2 production, which we attributed to warming and a decrease in amount and frequency of summer rains. Our results demonstrate strong precipitation control on the soil CO _2 flux in mountainous regions, a finding which has important implications for carbon cycling under future environmental change.https://doi.org/10.1088/1748-9326/ad07b5soil CO2 fluxsoil respirationsnowmonsoon rainmontane forestsmixed conifer
spellingShingle Mariah S Carbone
Andrew D Richardson
billy barr
Max Berkelhammer
Claudia M Boot
Austin Simonpietri
Christopher J Still
Interannual precipitation controls on soil CO2 fluxes in high elevation conifer and aspen forests
Environmental Research Letters
soil CO2 flux
soil respiration
snow
monsoon rain
montane forests
mixed conifer
title Interannual precipitation controls on soil CO2 fluxes in high elevation conifer and aspen forests
title_full Interannual precipitation controls on soil CO2 fluxes in high elevation conifer and aspen forests
title_fullStr Interannual precipitation controls on soil CO2 fluxes in high elevation conifer and aspen forests
title_full_unstemmed Interannual precipitation controls on soil CO2 fluxes in high elevation conifer and aspen forests
title_short Interannual precipitation controls on soil CO2 fluxes in high elevation conifer and aspen forests
title_sort interannual precipitation controls on soil co2 fluxes in high elevation conifer and aspen forests
topic soil CO2 flux
soil respiration
snow
monsoon rain
montane forests
mixed conifer
url https://doi.org/10.1088/1748-9326/ad07b5
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