A model of gross primary productivity based on satellite data suggests formerly afforested peatlands undergoing restoration regain full photosynthesis capacity after five to ten years.

Carbon Eddy covariance MODIS Peatland Remote sensing Restoration

Journal

Journal of environmental management
ISSN: 1095-8630
Titre abrégé: J Environ Manage
Pays: England
ID NLM: 0401664

Informations de publication

Date de publication:
15 Sep 2019
Historique:
received: 11 07 2018
revised: 26 02 2019
accepted: 08 03 2019
pubmed: 17 6 2019
medline: 26 9 2019
entrez: 17 6 2019
Statut: ppublish

Résumé

Peatlands are an important terrestrial carbon store, but disturbance has resulted in the degradation of many peatland ecosystems and caused them to act as a net carbon source. Restoration work is being undertaken but monitoring the success of these schemes can be difficult and costly using traditional field-based methods. A landscape-scale alternative is to use satellite data to assess the condition of peatlands and to estimate gaseous carbon fluxes. In this study we used Moderate Resolution Imaging Spectroradiometer (MODIS) products to model Gross Primary Productivity (GPP) over peatland sites at various stages of restoration. We found that the MOD17A2H GPP product overestimates GPP modelled from data collected by eddy covariance towers situated at two ex-forestry sites undergoing restoration towards blanket bog at the Forsinard Flows RSPB reserve, Scotland, UK (one full year of data), and a near-natural Atlantic blanket bog site in Glencar, Ireland (ten-year data series). We calibrated a Temperature and Greenness (TG) model for the Forsinard sites and found it to be more accurate than the MODIS GPP product at local scale. We also found that inclusion of a wetness factor using the Normalised Difference Water Index (NDWI) improved inter-annual accuracy of the model. This TGWa (annual Temperature, Greenness and Wetness) model was then applied to six control sites comprising near-natural bog across the reserve, and to six sites on which restoration began between 1998 and 2006. GPP from 2005 to 2016 was estimated for each site using the model. The resulting modelled trends are positive at all six restored sites, increasing by approximately 5.5 g C/m

Identifiants

pubmed: 31202827
pii: S0301-4797(19)30342-1
doi: 10.1016/j.jenvman.2019.03.040
pii:
doi:

Types de publication

Journal Article

Langues

eng

Sous-ensembles de citation

IM

Pagination

594-604

Informations de copyright

Copyright © 2019 Elsevier Ltd. All rights reserved.

Auteurs

K J Lees (KJ)

Department of Geography and Environmental Science, University of Reading, Whiteknights, RG6 6DW, UK. Electronic address: k.lees@exeter.ac.uk.

T Quaife (T)

National Centre for Earth Observation, Department of Meteorology, University of Reading, Reading, Whiteknights, RG6 6BB, UK.

R R E Artz (RRE)

James Hutton Institute, Craigiebuckler, Aberdeen, AB15 8QH, UK.

M Khomik (M)

University of Waterloo, ON N2L 3G1, Canada.

M Sottocornola (M)

Department of Science, Waterford Institute of Technology, Ireland.

G Kiely (G)

Civil Structural & Environmental Engineering, and Environmental Research Institute, University College Cork, Cork, T12 YN60, Ireland.

G Hambley (G)

University of St Andrews, Fife, KY16 9AJ, Scotland, UK.

T Hill (T)

University of Exeter, EX4 4QD, UK.

M Saunders (M)

Department of Botany, School of Natural Sciences, Trinity College Dublin, College Green, D2, Dublin, Ireland.

N R Cowie (NR)

Royal Society for the Protection of Birds, Centre for Conservation Science, Edinburgh, EH12 9DH, UK.

J Ritson (J)

Imperial College London, SW7 2A7 UK.

J M Clark (JM)

Department of Geography and Environmental Science, University of Reading, Whiteknights, RG6 6DW, UK.

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