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

被引:21
|
作者
Kristensen, Terje [1 ,2 ]
Naesset, Erik [1 ]
Ohlson, Mikael [1 ]
Bolstad, Paul V. [2 ]
Kolka, Randall [3 ]
机构
[1] Norwegian Univ Life Sci, Dept Ecol & Nat Resource Management, As, Norway
[2] Univ Minnesota, Dept Forest Resources, St Paul, MN 55108 USA
[3] US Forest Serv, USDA, Grand Rapids, MN USA
来源
PLOS ONE | 2015年 / 10卷 / 10期
关键词
COARSE WOODY DEBRIS; FINE-ROOT BIOMASS; NORWAY SPRUCE; UNDERSTORY VEGETATION; OLD-GROWTH; SCOTS PINE; BIOPHYSICAL PROPERTIES; VACCINIUM-MYRTILLUS; INDIVIDUAL TREES; SOIL PROPERTIES;
D O I
10.1371/journal.pone.0138450
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
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 (similar to 2000 m(2)) towards individual grid cells (1 m(2)) 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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页数:24
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