| Literature DB >> 31774813 |
Lisa A Venier1, Tom Swystun1, Marc J Mazerolle2, David P Kreutzweiser1, Kerrie L Wainio-Keizer1, Ken A McIlwrick1, Murray E Woods3, Xianli Wang1.
Abstract
Forest understory vegetation is an important characteristic of the forest. Predicting and mapping understory is a critical need for forest management and conservation planning, but it has proved difficult with available methods to date. LiDAR has the potential to generate remotely sensed forest understory structure data, but this potential has yet to be fully validated. Our objective was to examine the capacity of LiDAR point cloud data to predict forest understory cover. We modeled ground-based observations of understory structure in three vertical strata (0.5 m to < 1.5 m, 1.5 m to < 2.5 m, 2.5 m to < 3.5 m) as a function of a variety of LiDAR metrics using both mixed-effects and Random Forest models. We compared four understory LiDAR metrics designed to control for the spatial heterogeneity of sampling density. The four metrics were highly correlated and they all produced high values of variance explained in mixed-effects models. The top-ranked model used a voxel-based understory metric along with vertical stratum (Akaike weight = 1, explained variance = 87%, cross-validation error = 15.6%). We found evidence of occlusion of LiDAR pulses in the lowest stratum but no evidence that the occlusion influenced the predictability of understory structure. The Random Forest model results were consistent with those of the mixed-effects models, in that all four understory LiDAR metrics were identified as important, along with vertical stratum. The Random Forest model explained 74.4% of the variance, but had a lower cross-validation error of 12.9%. We conclude that the best approach to predict understory structure is using the mixed-effects model with the voxel-based understory LiDAR metric along with vertical stratum, because it yielded the highest explained variance with the fewest number of variables. However, results show that other understory LiDAR metrics (fractional cover, normalized cover and leaf area density) would still be effective in mixed-effects and Random Forest modelling approaches.Entities:
Mesh:
Year: 2019 PMID: 31774813 PMCID: PMC6881062 DOI: 10.1371/journal.pone.0220096
Source DB: PubMed Journal: PLoS One ISSN: 1932-6203 Impact factor: 3.240
Fig 1Sampling design for field observations of vegetation structure (FIELD).
Measurements around each point on the transects and vertical strata were within a 15 cm-radius (r).
Airborne LiDAR acquisition specifications.
| Parameter | Value |
|---|---|
| Pulse repetition rate | 150 Khz |
| Frequency | 76.67 Hz |
| Scan Angle | ± 20 Degrees |
| FOV | 40 Degrees |
| Line spacing: Cross track | 0.6 m |
| Line spacing: Along track | 0.6 m |
| Line spacing between flight lines | 250 m |
| Laser footprint min: | 0.38 m |
| Laser footprint max | 0.42 m |
| Average point density: All Returns | ~ 15 pts/m2 |
| Average point density: Last Returns | ~ 6 pts/m2 |
Mixed effects model explaining understory cover recorded in the field (FIELD): TYPE = forest type based on overstory composition, STRATUM = vertical 1 m strata, ST1-ST3, and OVERSTORY = a measure of LiDAR vegetation cover in the vertical column above the stratum of interest calculated by classifying canopy cover (CC) into three classes (low, medium, high), see S1 Table.
The plot was treated as a random effect in each model.
| Model Name | Model fixed effects structure | Biological interpretation |
|---|---|---|
| FRAC null | FRAC | Relationship between FRAC and FIELD is constant |
| FRAC * STRATUM | FRAC + STRATUM + FRAC*STRATUM | Relationship between FRAC and FIELD differs among STRATUM |
| FRAC * OVERSTORY | FRAC + OVERSTORY + FRAC*OVERSTORY | Relationship between FRAC and FIELD differs among OVERSTORY |
| FRAC * TYPE | FRAC + TYPE + FRAC*TYPE | Relationship between FRAC and FIELD differs among TYPE |
| NORM null | NORM | Relationship between NORM and FIELD is constant |
| NORM * STRATUM | NORM + STRATUM + NORM*STRATUM | Relationship between NORM and FIELD differs among STRATUM |
| NORM * OVERSTORY | NORM + OVERSTORY + FRAC*OVERSTORY | Relationship between NORM and FIELD differs among OVERSTORY |
| NORM * TYPE | NORM + TYPE + FRAC*TYPE | Relationship between NORM and FIELD differs among TYPE |
| VOX1m null | VOX1m | Relationship between VOX1m and FIELD is constant |
| VOX1m * STRATUM | VOX1m +STRATUM + VOX1m*STRATUM | Relationship between VOX1m and FIELD differs among STRATUM |
| VOX1m * OVERSTORY | VOX1m + OVERSTORY + VOX1m*OVERSTORY | Relationship between VOX1m and FIELD differs among OVERSTORY |
| VOX1m * TYPE | VOX1m + TYPE + VOX1m*TYPE | Relationship between VOX1m and FIELD differs among TYPE |
| LAD (null) | LAD | Relationship between LAD and FIELD is constant |
| LAD * STRATUM | LAD + STRATUM + LAD*STRATUM | Relationship between LAD and FIELD differs among STRATUM |
| LAD * OVERSTORY | LAD + OVERSTORY + LAD*OVERSTORY | Relationship between LAD and FIELD differs among OVERSTORY |
| LAD * TYPE | LAD + TYPE + LAD*TYPE | Relationship between LAD and FIELD differs among TYPE |
Fig 2Scatterplot of FIELD (measured density) against the LiDAR metrics, a) fractional cover (FRAC), b) normalized cover (NORM), c) leaf area density (LAD), and d) voxel cover (VOX1m), including Pearson product-moment correlation coefficients.
Pearson product-moment correlations between pairs of understory cover LiDAR metrics included in analysis (n = 1310).
| Correlation | r | Lower 95% CL | Upper 95% CL |
|---|---|---|---|
| FRAC vs NORM | 0.77 | 0.751 | 0.794 |
| FRAC vs VOX1m | 0.84 | 0.819 | 0.852 |
| FRAC vs LAD | 0.77 | 0.744 | 0.789 |
| NORM vs LAD | 0.81 | 0.79 | 0.827 |
| NORM vs VOX1m | 0.92 | 0.911 | 0.927 |
| VOX1m vs LAD | 0.79 | 0.767 | 0.808 |
R2 and AIC values for sixteen candidate linear mixed-effects models.
Note that marginal R2 denotes the percent variance explained by the fixed effects, whereas the conditional R2 includes both fixed effects and random effects. Delta AIC is the difference between each model relative to the most parsimonious model and Akaike weight indicates the percent support of a given model.
| Model | Marginal R2 | Conditional R2 | AIC | Delta AIC | Akaike weight |
|---|---|---|---|---|---|
| VOX1m * STRATUM | 0.62 | 0.87 | 11868.87 | 0 | 1 |
| FRAC * STRATUM | 0.65 | 0.87 | 11901.00 | 32.13 | 0 |
| LAD * STRATUM | 0.56 | 0.82 | 11998.29 | 129.42 | 0 |
| NORM * STRATUM | 0.52 | 0.83 | 12099.16 | 230.29 | 0 |
| VOX1m * OVERSTORY | 0.60 | 0.82 | 12348.32 | 479.45 | 0 |
| LAD * OVERSTORY | 0.51 | 0.73 | 12384.88 | 516.01 | 0 |
| VOX1m * TYPE | 0.60 | 0.82 | 12384.88 | 516.01 | 0 |
| VOX1m null | 0.60 | 0.82 | 12385.78 | 516.91 | 0 |
| LAD * TYPE | 0.51 | 0.72 | 12396.42 | 527.55 | 0 |
| LAD null | 0.50 | 0.71 | 12407.11 | 538.24 | 0 |
| NORM * OVERSTORY | 0.53 | 0.75 | 12450.66 | 581.79 | 0 |
| NORM * TYPE | 0.51 | 0.75 | 12563.97 | 695.1 | 0 |
| NORM null | 0.49 | 0.75 | 12568.4 | 699.53 | 0 |
| FRAC * OVERSTORY | 0.58 | 0.77 | 12585.04 | 716.17 | 0 |
| FRAC * TYPE | 0.57 | 0.75 | 12613.19 | 744.32 | 0 |
| FRAC null | 0.56 | 0.75 | 12617.05 | 748.18 | 0 |
Fig 3Predicted versus observed scatterplot.
(a) Predictions of FIELD generated from mixed-effects model consisting of VOX1m + STRATUM + interaction, (b) Predictions of FIELD generated from Random Forest model with 59 explanatory variables.
Fig 4Predictions of FIELD for each of three strata based on the mixed-effects model consisting of VOX1m + STRATUM + interaction.
Dashed lines around solid lines denote 95% confidence intervals around predictions.
Estimates of the best supported mixed-effects model consisting of VOX1m + STRATUM + interaction and a random effect of plot.
| Estimate | Lower 95% CL | Upper 95% CL | |
|---|---|---|---|
| intercept | 64.35 | 60.25 | 68.46 |
| LIDAR | 0.03 | 0.29 | 0.32 |
| STRATUM.ST2 | -21.94 | -25.96 | -17.98 |
| STRATUM.ST3 | -29.38 | -33.48 | -25.28 |
| LIDAR*STRATUM.ST2 | -0.016 | -0.039 | 0.008 |
| LIDAR*STRATUM.ST3 | -0.010 | -0.037 | 0.017 |
Ten-fold cross-validation results from top linear mixed-effects model and the selected Random Forest model, based on symmetric mean absolute percentage error (SMAPE).
Note that average values of SMAPE are given for predictions of all STRATUM levels, but also for predictions specific to STRATUM levels.
| Model | SMAPE mean | SMAPE sd (n = 10) | |
|---|---|---|---|
| VOX1m * STRATUM | predictions of all STRATUM levels | 0.156 | 0.014 |
| predictions of STRATUM 1 | 0.107 | 0.016 | |
| predictions of STRATUM 2 | 0.170 | 0.024 | |
| predictions of STRATUM 3 | 0.190 | 0.020 | |
| Random forest (59 predictors) | 0.129 | 0.015 |
Random forest models: Mean squared residuals and percent variance explained.
| Number of Predictors in model | Mean Squared Residuals | Percent variance Explained |
|---|---|---|
| 341 (Base model) | 484 | 74.8 |
| 276 | 485 | 74.7 |
| 223 | 485 | 74.8 |
| 180 | 484 | 74.7 |
| 145 | 476 | 75.2 |
| 116 | 486 | 74.7 |
| 93 | 481 | 75.0 |
| 74 | 492 | 74.3 |
| 59 | 490 | 74.4 |
| 47 | 513 | 73.3 |
| 37 | 508 | 73.5 |
| 29 | 531 | 72.4 |
| 22 | 553 | 71.2 |
| 17 | 528 | 72.5 |
| 13 | 558 | 70.9 |
| 10 | 580 | 69.8 |
| 7 | 569 | 70.4 |
| 5 | 632 | 67.1 |