Evaluation of long-term carbon dynamics in a drained forested peatland using the ForSAFE-Peat model

<p>Management of drained forested peatlands has important implications for carbon budgets, but contrasting views exist on its effects on climate. This study utilised the dynamic ecosystem model ForSAFE-Peat to simulate biogeochemical dynamics over two complete forest rotations (1951–2088) in a...

Full description

Saved in:
Bibliographic Details
Main Authors: D. Escobar, S. Manzoni, J. Tapasco, P. Vestin, S. Belyazid
Format: Article
Language:English
Published: Copernicus Publications 2025-04-01
Series:Biogeosciences
Online Access:https://bg.copernicus.org/articles/22/2023/2025/bg-22-2023-2025.pdf
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1849712317563928576
author D. Escobar
D. Escobar
S. Manzoni
J. Tapasco
P. Vestin
S. Belyazid
author_facet D. Escobar
D. Escobar
S. Manzoni
J. Tapasco
P. Vestin
S. Belyazid
author_sort D. Escobar
collection DOAJ
description <p>Management of drained forested peatlands has important implications for carbon budgets, but contrasting views exist on its effects on climate. This study utilised the dynamic ecosystem model ForSAFE-Peat to simulate biogeochemical dynamics over two complete forest rotations (1951–2088) in a nutrient-rich drained peatland afforested with Norway spruce (<i>Picea abies</i>) in southwestern Sweden. Model simulations aligned well with observed groundwater levels (<span class="inline-formula"><i>R</i><sup>2</sup>=0.78</span>) and soil temperatures (<span class="inline-formula"><i>R</i><sup>2</sup>≥0.76</span>) and captured seasonal and annual net ecosystem production patterns, although daily variability was not always well represented. Simulated carbon exchanges (a positive sign indicates gains, and a negative sign indicates losses) were analysed considering different system boundaries (the soil; the ecosystem; and the ecosystem and the fate of harvested wood products, named ecosystem–HWP) using the net carbon balance (NCB) and the integrated carbon storage (ICS) metrics. Model results indicated negative NCB and ICS across all system boundaries, except for a positive NCB calculated by the end of the simulation at the ecosystem–HWP level. The soil exhibited persistent carbon losses primarily driven by peat decomposition. At the ecosystem level, net carbon losses were reduced as forest growth partially offset soil losses until harvesting. NCB was positive (2307 <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow class="unit"><msub><mi mathvariant="normal">g</mi><mi mathvariant="normal">C</mi></msub><mspace width="0.125em" linebreak="nobreak"/><msubsup><mi mathvariant="normal">m</mi><mi mathvariant="normal">soil</mi><mrow><mo>-</mo><mn mathvariant="normal">2</mn></mrow></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="37pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="08c543144338314f4b10ced4437b56cb"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-22-2023-2025-ie00001.svg" width="37pt" height="17pt" src="bg-22-2023-2025-ie00001.png"/></svg:svg></span></span>) at the ecosystem–HWP level due to the slow decay of harvested wood products, but ICS was negative (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M4" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>-</mo><mn mathvariant="normal">0.59</mn><mo>×</mo><msup><mn mathvariant="normal">10</mn><mn mathvariant="normal">6</mn></msup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="59pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="7373506b0fc74b809df7466427be02df"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-22-2023-2025-ie00002.svg" width="59pt" height="14pt" src="bg-22-2023-2025-ie00002.png"/></svg:svg></span></span> <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M5" display="inline" overflow="scroll" dspmath="mathml"><mrow class="unit"><msub><mi mathvariant="normal">g</mi><mi mathvariant="normal">C</mi></msub><mspace linebreak="nobreak" width="0.125em"/><mi mathvariant="normal">yr</mi><mspace linebreak="nobreak" width="0.125em"/><msubsup><mi mathvariant="normal">m</mi><mi mathvariant="normal">soil</mi><mrow><mo>-</mo><mn mathvariant="normal">2</mn></mrow></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="47pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="51823c91fe35764f0b30cdb8d6a2dadf"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-22-2023-2025-ie00003.svg" width="47pt" height="17pt" src="bg-22-2023-2025-ie00003.png"/></svg:svg></span></span>) due to the large initial carbon losses. This study highlights the importance of system boundary selection and temporal dynamics in assessing the carbon balance of forested drained peatlands.</p>
format Article
id doaj-art-fdcc58c41c0041d6a456aa914a642bd4
institution DOAJ
issn 1726-4170
1726-4189
language English
publishDate 2025-04-01
publisher Copernicus Publications
record_format Article
series Biogeosciences
spelling doaj-art-fdcc58c41c0041d6a456aa914a642bd42025-08-20T03:14:19ZengCopernicus PublicationsBiogeosciences1726-41701726-41892025-04-01222023204710.5194/bg-22-2023-2025Evaluation of long-term carbon dynamics in a drained forested peatland using the ForSAFE-Peat modelD. Escobar0D. Escobar1S. Manzoni2J. Tapasco3P. Vestin4S. Belyazid5Department of Physical Geography and Bolin Centre for Climate Research, Stockholm University, 106 91 Stockholm, SwedenClimate Action, Alliance of Bioversity International and the International Centre for Tropical Agriculture (CIAT), Palmira 763537, ColombiaDepartment of Physical Geography and Bolin Centre for Climate Research, Stockholm University, 106 91 Stockholm, SwedenClimate Action, Alliance of Bioversity International and the International Centre for Tropical Agriculture (CIAT), Palmira 763537, ColombiaDepartment of Physical Geography and Ecosystem Science, Lund University, 22362 Lund, SwedenDepartment of Physical Geography and Bolin Centre for Climate Research, Stockholm University, 106 91 Stockholm, Sweden<p>Management of drained forested peatlands has important implications for carbon budgets, but contrasting views exist on its effects on climate. This study utilised the dynamic ecosystem model ForSAFE-Peat to simulate biogeochemical dynamics over two complete forest rotations (1951–2088) in a nutrient-rich drained peatland afforested with Norway spruce (<i>Picea abies</i>) in southwestern Sweden. Model simulations aligned well with observed groundwater levels (<span class="inline-formula"><i>R</i><sup>2</sup>=0.78</span>) and soil temperatures (<span class="inline-formula"><i>R</i><sup>2</sup>≥0.76</span>) and captured seasonal and annual net ecosystem production patterns, although daily variability was not always well represented. Simulated carbon exchanges (a positive sign indicates gains, and a negative sign indicates losses) were analysed considering different system boundaries (the soil; the ecosystem; and the ecosystem and the fate of harvested wood products, named ecosystem–HWP) using the net carbon balance (NCB) and the integrated carbon storage (ICS) metrics. Model results indicated negative NCB and ICS across all system boundaries, except for a positive NCB calculated by the end of the simulation at the ecosystem–HWP level. The soil exhibited persistent carbon losses primarily driven by peat decomposition. At the ecosystem level, net carbon losses were reduced as forest growth partially offset soil losses until harvesting. NCB was positive (2307 <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow class="unit"><msub><mi mathvariant="normal">g</mi><mi mathvariant="normal">C</mi></msub><mspace width="0.125em" linebreak="nobreak"/><msubsup><mi mathvariant="normal">m</mi><mi mathvariant="normal">soil</mi><mrow><mo>-</mo><mn mathvariant="normal">2</mn></mrow></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="37pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="08c543144338314f4b10ced4437b56cb"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-22-2023-2025-ie00001.svg" width="37pt" height="17pt" src="bg-22-2023-2025-ie00001.png"/></svg:svg></span></span>) at the ecosystem–HWP level due to the slow decay of harvested wood products, but ICS was negative (<span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M4" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>-</mo><mn mathvariant="normal">0.59</mn><mo>×</mo><msup><mn mathvariant="normal">10</mn><mn mathvariant="normal">6</mn></msup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="59pt" height="14pt" class="svg-formula" dspmath="mathimg" md5hash="7373506b0fc74b809df7466427be02df"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-22-2023-2025-ie00002.svg" width="59pt" height="14pt" src="bg-22-2023-2025-ie00002.png"/></svg:svg></span></span> <span class="inline-formula"><math xmlns="http://www.w3.org/1998/Math/MathML" id="M5" display="inline" overflow="scroll" dspmath="mathml"><mrow class="unit"><msub><mi mathvariant="normal">g</mi><mi mathvariant="normal">C</mi></msub><mspace linebreak="nobreak" width="0.125em"/><mi mathvariant="normal">yr</mi><mspace linebreak="nobreak" width="0.125em"/><msubsup><mi mathvariant="normal">m</mi><mi mathvariant="normal">soil</mi><mrow><mo>-</mo><mn mathvariant="normal">2</mn></mrow></msubsup></mrow></math><span><svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="47pt" height="17pt" class="svg-formula" dspmath="mathimg" md5hash="51823c91fe35764f0b30cdb8d6a2dadf"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="bg-22-2023-2025-ie00003.svg" width="47pt" height="17pt" src="bg-22-2023-2025-ie00003.png"/></svg:svg></span></span>) due to the large initial carbon losses. This study highlights the importance of system boundary selection and temporal dynamics in assessing the carbon balance of forested drained peatlands.</p>https://bg.copernicus.org/articles/22/2023/2025/bg-22-2023-2025.pdf
spellingShingle D. Escobar
D. Escobar
S. Manzoni
J. Tapasco
P. Vestin
S. Belyazid
Evaluation of long-term carbon dynamics in a drained forested peatland using the ForSAFE-Peat model
Biogeosciences
title Evaluation of long-term carbon dynamics in a drained forested peatland using the ForSAFE-Peat model
title_full Evaluation of long-term carbon dynamics in a drained forested peatland using the ForSAFE-Peat model
title_fullStr Evaluation of long-term carbon dynamics in a drained forested peatland using the ForSAFE-Peat model
title_full_unstemmed Evaluation of long-term carbon dynamics in a drained forested peatland using the ForSAFE-Peat model
title_short Evaluation of long-term carbon dynamics in a drained forested peatland using the ForSAFE-Peat model
title_sort evaluation of long term carbon dynamics in a drained forested peatland using the forsafe peat model
url https://bg.copernicus.org/articles/22/2023/2025/bg-22-2023-2025.pdf
work_keys_str_mv AT descobar evaluationoflongtermcarbondynamicsinadrainedforestedpeatlandusingtheforsafepeatmodel
AT descobar evaluationoflongtermcarbondynamicsinadrainedforestedpeatlandusingtheforsafepeatmodel
AT smanzoni evaluationoflongtermcarbondynamicsinadrainedforestedpeatlandusingtheforsafepeatmodel
AT jtapasco evaluationoflongtermcarbondynamicsinadrainedforestedpeatlandusingtheforsafepeatmodel
AT pvestin evaluationoflongtermcarbondynamicsinadrainedforestedpeatlandusingtheforsafepeatmodel
AT sbelyazid evaluationoflongtermcarbondynamicsinadrainedforestedpeatlandusingtheforsafepeatmodel