Using remote sensing to assess peatland resilience by estimating soil surface moisture and drought recovery

• Published in: The Science of the total environment 2021-03, Vol.761, p.143312, Article 143312
• Main Authors: Lees, K.J., Artz, R.R.E., Chandler, D., Aspinall, T., Boulton, C.A., Buxton, J., Cowie, N.R., Lenton, T.M.
• Format: Article
• Language: English
• Subjects: Blanket bog; Hydrology; SAR; Sentinel-1; Water table dynamics
• ISSN: 0048-9697; 1879-1026
• DOI: 10.1016/j.scitotenv.2020.143312

Peatland areas provide a range of ecosystem services, including biodiversity, carbon storage, clean water, and flood mitigation, but many areas of peatland in the UK have been degraded through human land use including drainage. Here, we explore whether remote sensing can be used to monitor peatland resilience to drought. We take resilience to mean the rate at which a system recovers from perturbation; here measured literally as a recovery timescale of a soil surface moisture proxy from drought lowering. Our objectives were (1) to assess the reliability of Sentinel-1 Synthetic Aperture Radar (SAR) backscatter as a proxy for water table depth (WTD); (2) to develop a method using SAR to estimate below-ground (hydrological) resilience of peatlands; and (3) to apply the developed method to different sites and consider the links between resilience and land management. Our inferences of WTD from Sentinel-1 SAR data gave results with an average Pearson's correlation of 0.77 when compared to measured WTD values. The 2018 summer drought was used to assess resilience across three different UK peatland areas (Dartmoor, the Peak District, and the Flow Country) by considering the timescale of the soil moisture proxy recovery. Results show clear areas of lower resilience within all three study sites, which often correspond to areas of high drainage and may be particularly vulnerable to increasing drought severity/events under climate change. This method is applicable to monitoring peatland resilience elsewhere over larger scales, and could be used to target restoration work towards the most vulnerable areas. [Display omitted] •Many peatlands are degraded, potentially causing low resilience to climate change.•Drought recovery time can be used to assess peatland resilience.•Soil moisture and drought recovery can be estimated from Sentinel-1 SAR data.•Areas of lower resilience are shown to correlate with areas of high drainage.