Carbon and climate implications of rewetting a raised bog in Ireland

Title: Carbon and climate implications of rewetting a raised bog in Ireland
Authors: Wilson, DavidMackin, FrancisTuovinen, Juha-PekkaMoser, GeraldFarrell, Catherine A.Renou-Wilson, Florence
Permanent link: http://hdl.handle.net/10197/13210
Date: Nov-2022
Online since: 2022-10-20T15:01:12Z
Abstract: Peatland rewetting has been proposed as a vital climate change mitigation tool to reduce greenhouse gas emissions and to generate suitable conditions for the return of carbon (C) sequestration. In this study, we present annual C balances for a 5-year period at a rewetted peatland in Ireland (rewetted at the start of the study) and compare the results with an adjacent drained area (represents business-as-usual). Hydrological modelling of the 230-hectare site was carried out to determine the likely ecotopes (vegetation communities) that will develop post-rewetting and was used to inform a radiative forcing modelling exercise to determine the climate impacts of rewetting this peatland under five high-priority scenarios (SSP1-1.9, SS1-2.6, SSP2-4.5, SSP3-7.0 and SSP5-8.5). The drained area (marginal ecotope) was a net C source throughout the study and emitted 157 ± 25.5 g C m−2 year−1. In contrast, the rewetted area (sub-central ecotope) was a net C sink of 78.0 ± 37.6 g C m−2 year−1, despite relatively large annual methane emissions post-rewetting (average 19.3 ± 5.2 g C m−2 year−1). Hydrological modelling predicted the development of three key ecotopes at the site, with the sub-central ecotope predicted to cover 24% of the site, the sub-marginal predicted to cover 59% and the marginal predicted to cover 16%. Using these areal estimates, our radiative forcing modelling projects that under the SSP1-1.9 scenario, the site will have a warming effect on the climate until 2085 but will then have a strong cooling impact. In contrast, our modelling exercise shows that the site will never have a cooling impact under the SSP5-8.5 scenario. Our results confirm the importance of rapid rewetting of drained peatland sites to (a) achieve strong C emissions reductions, (b) establish optimal conditions for C sequestration and (c) set the site on a climate cooling trajectory.
Funding Details: Environmental Protection Agency
Funding Details: Bord na Móna
Academy of Finland
Open access funding provided by IReL
Type of material: Journal Article
Publisher: Wiley
Journal: Global Change Biology
Volume: 28
Issue: 21
Start page: 6349
End page: 6365
Copyright (published version): 2022 The Authors
Keywords: Carbon dioxideClimate mitigationMethanePeatRadiative forcingRewetting
DOI: 10.1111/gcb.16359
Language: en
Status of Item: Peer reviewed
ISSN: 1354-1013
This item is made available under a Creative Commons License: https://creativecommons.org/licenses/by-nc-nd/3.0/ie/
Appears in Collections:Biology & Environmental Science Research Collection
Climate Change Collection

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