Mapping Above- and Below-Ground Carbon Pools in Boreal Forests: The Case for Airborne Lidar.

PLoS One

United States Forest Service, United States Department of Agriculture, Grand Rapids, Minnesota, United States of America.

Published: June 2016

AI Article Synopsis

  • Airborne lidar technology is effective for measuring above-ground tree biomass in forests, but its use for assessing carbon stocks in soil and non-tree vegetation is less explored.
  • The study combines lidar data with carbon information to analyze carbon pools in Norway spruce stands, finding that lidar metrics can accurately model carbon in trees and correlate with carbon in field layer vegetation.
  • Results suggest that while tree and understory carbon distributions are influenced by lidar data, mosses and soil carbon stocks are more affected by topographical factors, highlighting the need for higher-resolution topographical data in carbon assessments.

Article Abstract

A large and growing body of evidence has demonstrated that airborne scanning light detection and ranging (lidar) systems can be an effective tool in measuring and monitoring above-ground forest tree biomass. However, the potential of lidar as an all-round tool for assisting in assessment of carbon (C) stocks in soil and non-tree vegetation components of the forest ecosystem has been given much less attention. Here we combine the use airborne small footprint scanning lidar with fine-scale spatial C data relating to vegetation and the soil surface to describe and contrast the size and spatial distribution of C pools within and among multilayered Norway spruce (Picea abies) stands. Predictor variables from lidar derived metrics delivered precise models of above- and below-ground tree C, which comprised the largest C pool in our study stands. We also found evidence that lidar canopy data correlated well with the variation in field layer C stock, consisting mainly of ericaceous dwarf shrubs and herbaceous plants. However, lidar metrics derived directly from understory echoes did not yield significant models. Furthermore, our results indicate that the variation in both the mosses and soil organic layer C stock plots appears less influenced by differences in stand structure properties than topographical gradients. By using topographical models from lidar ground returns we were able to establish a strong correlation between lidar data and the organic layer C stock at a stand level. Increasing the topographical resolution from plot averages (~2000 m2) towards individual grid cells (1 m2) did not yield consistent models. Our study demonstrates a connection between the size and distribution of different forest C pools and models derived from airborne lidar data, providing a foundation for future research concerning the use of lidar for assessing and monitoring boreal forest C.

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Source
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4591287PMC
http://journals.plos.org/plosone/article?id=10.1371/journal.pone.0138450PLOS

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