Abstract

South Patagonian peat bogs are little studied sources of methane (CH4). Since CH4 fluxes can vary greatly on a small scale of meters, high-quality maps are needed to accurately quantify CH4 fluxes from bogs. We used high-resolution color infrared (CIR) images captured by an Unmanned Aerial System (UAS) to investigate potential uncertainties in total ecosystem CH4 fluxes introduced by the classification of the surface area. An object-based approach was used to classify vegetation both on species and microform level. We achieved an overall Kappa Index of Agreement (KIA) of 0.90 for the species- and 0.83 for the microform-level classification, respectively. CH4 fluxes were determined by closed chamber measurements on four predominant microforms of the studied bog. Both classification approaches were employed to up-scale CH4 closed chamber measurements in a total area of around 1.8 hectares. Including proportions of the surface area where no chamber measurements were conducted, we estimated a potential uncertainty in ecosystem CH4 fluxes introduced by the classification of the surface area. This potential uncertainty ranged from 14.2 mg·m−2·day−1 to 26.8 mg·m−2·day−1. Our results show that a simple classification with only few classes potentially leads to pronounced bias in total ecosystem CH4 fluxes when plot-scale fluxes are up-scaled.

Highlights

  • The effects of human activities on the carbon cycle receive much attention worldwide from both research and public perspective

  • Carbon cycling in peatlands is an important feature of the global carbon cycle because these ecosystems are important carbon sinks [1,2], but are main sources of methane (CH4 ) [1,3,4]

  • Southern peat bogs are comparatively little explored [8,9]; this is true of Patagonian peat bogs [10], which have been affected little by human activities [8,10,11]

Read more

Summary

Introduction

The effects of human activities on the carbon cycle receive much attention worldwide from both research and public perspective. Methane fluxes typically vary temporally and on spatial scales from the Remote Sens. 2016, 8, 173 microform to the ecosystem level [4,5,6]. In this context, northern peat bogs have been extensively studied, especially those found in the boreal zone [1,2,4,5,7]. Research in Patagonian peat bogs can enhance our understanding of CH4 fluxes from pristine ecosystems

Methods
Results
Discussion
Conclusion
Full Text
Published version (Free)

Talk to us

Join us for a 30 min session where you can share your feedback and ask us any queries you have

Schedule a call