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Remote Sensing 2013, 5(1), 202-223; doi:10.3390/rs5010202
Published: 10 January 2013
Abstract: The ultimate goal of this multi-article series is to develop a methodology to generate continuous fields of tree height and biomass. The first paper demonstrated the need for Allometric Scaling and Resource Limitation (ASRL) model optimization and its ability to generate spatially continuous fields of tree heights over the continental USA at coarse (1 km) spatial resolution. The objective of this second paper is to provide an assessment of that approach at site scale, specifically at 12 FLUXNET sites where more accurate data are available. Estimates of tree heights from the Geoscience Laser Altimeter System (GLAS) waveform data are used for model optimization. Amongst the five possible GLAS metrics that are representative of tree heights, the best metric is selected based on how closely the metric resembles field-measured and Laser Vegetation Imaging Sensor tree heights. In the optimization process, three parameters of the ASRL model (area of single leaf, α; exponent for canopy radius, η; and root absorption efficiency, γ) are simultaneously adjusted to minimize the difference between model predictions and observations at the study sites (distances to valid GLAS footprints ≤ 10 km). Performance of the optimized ASRL model was evaluated through comparisons to the best GLAS metric of tree height using a two-fold cross validation approach (R2 = 0.85; RMSE = 1.81 m) and a bootstrapping approach (R2 = 0.66; RMSE = 2.60 m). The optimized model satisfactorily performed at the site scale, thus corroborating results presented in part one of this series. Future investigations will focus on generalizing these results and extending the model formulation using similar allometric concepts for the estimation of woody biomass.
Forest height and biomass are important attributes required for quantifying the dynamics of the terrestrial carbon cycle [1–4]. Several recent articles have reported variations in regional and global forest structural attributes  (e.g., under decreasing , increasing [7–9], or relatively steady-state  conditions), but there remains large uncertainty [11–13]. Two conventional methods of mapping tree heights and biomass are the extrapolation methods using field-measured and/or remote sensing altimetry data (e.g., regression tree or random forest algorithms [14–16]) and the physical/physiological model based on allometric scaling laws (e.g., Allometric Scaling and Resource Limitations (ASRL) model ).
The extrapolation methods well estimate forest structural attributes by exploiting advancements in remote sensing. Small footprint lidar, Terrestrial Laser Scanners [18,19] and Laser Vegetation Imaging Sensor (LVIS) [20,21] are key to accurate estimation of tree heights and forest biomass. Global and regional maps of tree heights [14,15] and forest biomass [16,22,23] have been generated using lidar waveform data from the Geoscience Laser Altimeter System (GLAS) instrument onboard the Ice, Cloud and land Elevation Satellite (ICESat). The relatively large footprint and wide spatial coverage of the GLAS instrument have made large-scale mapping of forest heights feasible [24,25]. However, the physical/physiological mechanisms governing plant growth are often neglected in the extrapolation approaches. The ASRL model  alternatively uses allometric scaling rules, which relate tree heights and local energy budgets in the prediction of potential tree growth. Nevertheless, the premises of the ASRL model have an obvious limitation that the balance of internal flows (metabolic flow requirement, available flow, and evaporative flow) is independent of local landscape variations across different eco-climatic regimes and forest types of varying age classes, unlike a non-allometric scaling model (e.g., ). This results in disparities between observations and model predictions.
Therefore, the parametric optimization of the ASRL model possibly brings significant progress in mapping tree heights and biomass by incorporating actual observations (i.e., GLAS waveform data) with the power of physical/physiological laws for scaling purpose. The feasibility of ASRL model optimization with high resolution remotely sensed altimetry data and its ability to predict tree heights are tested in the multi-article series with the ultimate goal of generating accurate spatially continuous fields of tree heights and biomass. Paper one in this series is focused on the application of the optimized ASRL model over the continental USA (CONUS) . The forested lands in the CONUS were delineated into different eco-climatic zones based on dominant forest type, annual total precipitation amount and annual average temperature. The optimization involved finding the appropriate scaling parameters and exponents of the ASRL model in each of the eco-climatic zones using the Powell’s optimization method . A spatially continuous map of tree heights over the CONUS was satisfactorily reproduced in the first paper, but at coarse spatial scales (1 km). The objective of this second article is to test the methodology underlying these large-scale mapping efforts at finer spatial scales, i.e., FLUXNET sites, where more accurate information is available. Future articles in this series will extend the allometric scaling and resource limitation concepts to estimation of woody biomass.
2.1. Field Measurements
In this study, we used four different sources of field-measured tree heights. Data from 82 plots were assembled from seven field sites (Table 1) [20,21,29–35]. These data came from different measurement campaigns, or census, and are comprised of different acquisition dates with varying sizes and numbers of subplots as shown in Section S1 and Figure S1 of the Supplementary Material.
2.2. LVIS Data
LVIS is an airborne laser altimeter sensor that records the intensity of returned signals from a target surface . An LVIS standard data product, RH100, was used in this study (Section S2.1). Lidar tree heights could be influenced by topography and footprint size. Therefore, topographic effects were corrected from LVIS tree heights taking into account its footprint size (∼20 m) .
LVIS datasets used in this study were categorized into two groups. The first dataset was used to compare LVIS heights with concurrent field-measured tree heights in seven different locations (Table 1 and Figure S1). In a separate exercise, the second dataset was used for comparisons between LVIS tree heights and GLAS height metrics. Except for the 2008 Sierra Nevada campaign, acquisition dates of the second dataset mostly overlapped with GLAS waveform acquisition dates (from 2003 to 2006; Table 2 and Figure S2).
2.3. GLAS Data
The latest release of GLAS laser altimetry data (Release 33) available from the National Snow and Ice Data Center was used in this study. GLAS waveform data provide information on land elevation and vegetation cover within its ellipsoidal footprints at ∼170 m spaced intervals [40,41]. We used GLAS Level-2 Land Surface Altimetry (GLA14) product, which includes geolocation of footprints and waveform parameters such as signal beginning and echo energy peaks . It is difficult to estimate the dimension and shape of every single GLAS footprint. Therefore, all GLAS footprints were assumed to have a circular diameter of 70 m  in this study.
Figure 1 depicts the sequential preprocessing/filtering steps for selecting valid GLAS waveforms. Data from May to October of each year were considered, as this period best approximates the growing season. GLAS data were further screened by applying several preprocessing filters, such as atmospheric forward scattering and signal saturation, background noise level correction and landcover mask conditions (Section S2.2, S2.3, S3, and Figure S3 for preprocessing datasets). GLAS footprints have a coarser spatial resolution (70 m) than some preprocessing datasets (e.g., National Land Cover Database is at 30 m spatial resolution). A GLAS footprint is possibly located over heterogeneous forest types and topographic conditions. This study used preprocessing data values of nearest pixels to the center of a GLAS footprint as the normalized lidar intensity of GLAS data peaks at the center of footprint .
2.4. Input Data for the ASRL Model
The ASRL model predicts potential tree heights. The model combines statistical allometric scaling laws with local energy budgets constrained by resource limitations such as water, radiation, wind and air temperature . The model is driven by input climatic variables and tree trait parameters. Input climatic variables are annual incoming solar radiation, annual total precipitation, annual average temperature, annual average wind speed and annual average relative humidity. Additionally, Leaf Area Index (LAI) and Digital Elevation Model (DEM) are required for initializing the model. Table S1 lists the input datasets (climatic and ancillary data).
2.4.1. FLUXNET Data
The analysis in this paper is focused on sites from the FLUXNET network . We chose 12 sites, amongst the 71 sites over the CONUS, based on distance between a site and valid GLAS footprints (≤10 km radius; Figure 2 and Table 3). Annual total precipitation and annual average temperature data (from 2001 to 2006) were obtained from the selected sites.
2.4.2. DAYMET Data
The FLUXNET datasets do not contain all the input climatic variables required by the ASRL model. Annual incoming solar radiation, annual average wind speed and annual average vapor pressure were therefore obtained from the DAYMET database  at a spatial resolution of 1 km. DAYMET climatic values were extracted from pixels nearest to our study sites. Annual vapor pressure was converted into annual relative humidity using a formula provided by the World Meteorological Organization (WMO) .
2.4.3. Ancillary Data for the ASRL Model (LAI and DEM)
The ASRL model requires two ancillary variables: (a) LAI and (b) DEM. Several Landsat TM scenes (Figure 2(a)) were obtained for the period 2003 to 2006 with near-similar acquisition dates (June to September) as the GLAS waveform data. The Landsat Ecosystem Disturbance Adaptive Processing System  and a physically-based algorithm  were used to retrieve LAI values. As with the DAYMET data, we extracted LAI and DEM values of the pixels nearest to the study sites. Neighboring pixels in a 3 × 3 window showed minimal variability in both LAI and DEM at 30 m spatial resolution (absolute variation coefficients <5%).
3.1. GLAS Metric Selection
Prior to the optimization of the ASRL model with GLAS tree heights, we perform an exercise finding the best GLAS metric that closely corresponds to field-measured and LVIS derived tree heights. This analysis is based on two premises: (a) canopy height derived from LVIS data is related to field-measured tree height as reported in previous studies [2,37,48–50] and (b) the best GLAS metric, inferred from comparison of five GLAS metrics with LVIS tree heights, improves model optimization. Several recent articles have evaluated GLAS tree heights directly with field data [14,51–53] and/or with airborne lidar data [37,54–56].
The root mean square error (RMSE) and R2 (from the linear-regression) are used to determine how well tree heights are related to each other in the inter-comparisons among field-measured, LVIS, and GLAS derived tree heights. Systematic errors related to biases in measurements are additionally considered in the interpretation of results.
3.1.1. Comparison between Field-Measured and LVIS Tree Heights
Field-measured datasets used in this study differed in their sampling methodologies and plot designs. Also, the coordinates of individual trees were not recorded in every measurement campaign/census. This precluded a footprint-level comparison between field-measured and LVIS tree heights, unlike in some previous studies [2,48]. Therefore, we performed comparisons at the plot-level by calculating representative tree height values from field measurements and LVIS data, which were defined as the average of the top 25% tree heights in each of the subplots (e.g., Figure S4). This approach minimizes overestimations (e.g., using only three highest values ) or underestimations (e.g., using all values ) if there are large numbers of field-measured trees and LVIS footprints in a subplot. The RMSE is calculated using Equation 1.
3.1.2. Comparison between LVIS Tree Heights and GLAS Height Metrics
Three standard altimetry variables are available from the GLA14 product based on the Gaussian decomposition approach : (a) signal begin range increment, SigBegOff, (b) signal end range increment, SigEndOff and (c) centroid range increment for the last Gaussian Peak, gpCntRngOff 1. Theoretically, gpCntRngOff 1 and SigEndOff are assumed to represent the ground level elevation within a GLAS field-of-view, while SigBegOff refers to the highest point of a surface. In practice, (SigBegOff − SigEndOff) and (SigBegOff − gpCntRngOff 1) may not be identical due to topographic and roughness effects . There are five possible GLAS metrics representative of tree heights based on the Gaussian decomposition approach and topographic effect correction (HA–E in Table 4 and Section S4).
The spatial correspondence between LVIS and GLAS footprints was determined using the maximum distance from the center of a GLAS footprint to any LVIS footprint (within ∼45 m; Figure S5). The RMSEs between LVIS heights and five possible GLAS height metrics were obtained from Equation (2):
The result analyses were stratified into three groups, based on topographic conditions over the GLAS footprint, as low (slope ≤ 5°), intermediate (5° < slope ≤ 10°) and high (10° < slope ≤ 20°). All outliers were removed in this comparison exercise, i.e., only GLAS tree heights within two standard deviations from the mean height were considered (∼95%; 5 m < HA–E ≤ 100 m).
3.2. ASRL Model Optimization
3.2.1. Initial ASRL Model Predictions (Potential Tree Heights)
The initial model runs are driven by input datasets and result in potential tree heights at each study site. Key climate input data (temperature and precipitation) are derived from FLUXNET sites. DAYMET, LAI, and DEM grids nearest to the study sites provide other climatic variables and ancillary data for the model runs. The unoptimized ASRL model predicts only potential tree heights considering hydraulic limits to tree growth. These differ from observations due to the fact that the unoptimized model applies homogeneous steady-state allometric scaling laws across different environmental conditions and forest types with varying age classes .
3.2.2. Optimized ASRL Model Predictions
Remote sensing based altimetry data, which provide actual tree heights, can alleviate the limitation of the unoptimized ASRL model related to different growing conditions and forest types with varying age classes. The model optimization is detailed in the first paper of this series . Model optimization is aimed at minimizing the difference between GLAS tree heights and model predictions (Figure 3) based on the Powell’s optimization methodology . A merit function was formulated and implemented from Press et al. and Kuusk and Nilson . It finds the maximum likelihood estimates of each parameter that result in minimizing the merit function. Amongst the five GLAS height metrics, the model optimization uses the best GLAS metric that is closest to the field-measured and LVIS tree heights.
Three model parameters are iteratively adjusted during optimization: (a) area of single leaf, α, (b) exponent for canopy radius, η, and (c) root absorption efficiency, γ. The respective initial values are 13 cm2, 1.14, and 0.33 . α is related to the collection of solar radiation for plant growth, and it is used to calculate the coefficients for canopy transmissions. In the ASRL model, energy budget in a single leaf is accumulated to a canopy-level budget . The geometry of canopy is associated with η controlling the scaling of canopy radius with tree height. This derives the rate of absorbed solar radiation in the ASRL model . γ determines the available flow rate given the incoming rate of precipitation within the root capture area. Local γ varies depending on soil type and hydrology . To achieve convergence, the following ranges were used: 1 cm2 ≤ α < 100 cm2, 0.8 ≤ η < 1.5, and 0.1 ≤ γ < 0.8 (as in the TRY database ). Kempes et al. tested η and γ individually in a sensitivity analysis. This study added α to the optimization scheme because the area of a leaf significantly varies across different eco-climatic regimes and forest types [64,65]. Also, α is an important parameter determining net radiation and fluxes of sensible and latent heat (e.g., ).
Our approach has constraints due to a limited number of scaling parameters (α, η, and γ) explored in the model optimization and an assumption that allometric scaling laws at individual tree level are applicable at larger scales. In addition, a limitation of this study is that the model does not directly account for variation in forest stand age in the optimization process. Tree heights and growth rates are clearly related to forest stand ages [67,68], varying across different forest types and growing conditions. However, it does not necessarily mean that our methodology neglects forest stand ages in the estimation of tree heights. GLAS waveform data indirectly brings age information of forests into the ASRL model for the parametric optimization, as actual heights are associated with forest stand ages.
3.3. Evaluation of the Optimized ASRL Model Predictions
3.3.1. Two-Fold Cross Validation Approach
The performance of the optimized ASRL model is evaluated through comparisons against GLAS tree heights in this study. The two-fold cross validation technique is a common statistical approach that randomly divides original samples into two equal sets of training and test data. The first half of GLAS tree heights was used as a training dataset to optimize the model at a site. The test dataset was prepared by averaging the remaining half of GLAS tree heights at the same site. Training and test GLAS data are completely separated in the cross validation (i.e., no overlapping each other). The RMSE is estimated to interpret the relationship between GLAS tree heights and optimized model predictions (Equation (3)) along with R2 from the linear regression.
3.3.2. Bootstrapping Approach
A second evaluation of the optimized ASRL model was performed at the eco-climatic zone scale . Individual FLUXNET sites were grouped into eco-climatic zones (Figure S6). Each zone consisted of 1 to 2 FLUXNET sites at the most. We neglected zones where GLAS footprints were less than 50 based on the need for model optimization. Selected sites include Harvard Forest EMS Tower (US-Ha1), Howland Forest Main Tower (US-Ho1), Howland Forest West Tower (US-Ho2), Harvard Forest Hemlock Site (US-Ha2), Missouri Ozark Site (US-MOz), and Little Prospect Hill (US-LPH) within a total of five eco-climatic zones (Table S2).
A bootstrapping approach  was applied to evaluate the optimized model predictions for the five zones. Corresponding GLAS footprints were randomly divided into two groups (training and test datasets). The bootstrapping generated extra comparison sets (subsamples, N = 100) to examine the stability of the results. Training subsamples of the GLAS tree heights were used for model optimization. The optimized ASRL model predictions were then compared to the average of tree heights derived from test subsamples by calculating the RMSE (Equation 4). R2 from the linear regression is additionally provided for the interpretation. Two groups of subsamples (training and test) also have no overlaps in each other.
4. Results and Discussion
4.1. Best GLAS Height Metric from Inter-Comparisons with Field-Measured and LVIS Tree Heights
We first performed a plot-level comparison between LVIS tree heights and field measurements (Figure 4). The statistical significance of this relationship (R2 = 0.76 and RMSE = 4.13 m) is comparable to previous reports (footprint-level comparison  and plot-level comparison ). Some disagreements are due to differences in data acquisition times. For example, field measurements for the Penobscot Experimental Forest (Maine, USA) were conducted in 2009, while the LVIS data were acquired in 2003. Similarly, the LVIS acquisition date is six years prior to field measurements of the 2009 New England Campaign (Table 1).
The average tree growth rates in study regions can be approximated using an equation of Shugart et al.. The map of forest age distribution in North America  shows that forest stands are aged from 41 to 80 in New England (Maine, Massachusetts, and New Hampshire). We expect that tree growths in New England can be made roughly up to 1.3 m for 6 years.
Relatively large deviation is found in the results of Barro-Colorado Island. Two plausible reasons are associated with (a) tree growth rates of tropical forest and (b) terrain features and densely vegetated environment of the study area. Tropical forests increase more in size  compared to USA forests for a similar period. This explains that field measured tree heights (year 2000) are larger than LVIS tree heights (year 1998). Another plausible reason for disagreements is that the LVIS is a large-footprint lidar (20 m), which is significantly affected by the topography and denseness of vegetation over the ground . Especially, Barro Colorado Island consists of dense tropical forest and some plots are located over steep terrains. This possibly decreases the measurement accuracy of LVIS data, inflating deviations.
Subsequent analysis was focused on comparison of five metrics derived from GLAS waveform data (HA–E; Table 4) with LVIS tree heights, at six sites with terrain slope condition ≤5°(Figure 5). Results for other slope categories are shown in Figure S7 and S8. We observed an overestimation of GLAS tree heights relative to LVIS tree heights, similar to previous studies [37,56]. Among the five GLAS height metrics, HC was best correlated to LVIS tree heights (R2 of 0.70 and RMSE of 4.42 m (P < 0.01)). This metric was derived from the distance between the last Gaussian peak and signal beginning of the GLAS waveform and incorporated topographic effect correction. Overestimations are related to both topographic gradient effects and GLAS waveform parameters. The bias increased with increasing tree heights (HA and HB; Figure 5(a,b)), as previously noted in Lee et al.. Also, significant biases were generated for taller trees from use of the full GLAS waveform extents (HB and HD; Figure 5(b,d)). As shown in Figures 5e, a relatively low correlation with LVIS tree heights was obtained from the metric using all three GLAS waveform parameters (i.e., signal begin, end, and the last Gaussian peak).
Similarly, for regions with intermediate slope condition (Figure S7) HC was best correlated with LVIS tree height but with a lower R2 and larger RMSE as compared to the low slope condition. In the case of high topographic gradients (Figure S8), HD showed better correspondence with LVIS heights, however, the correlations were significantly lower for all five metrics.
4.2. Optimized ASRL Model Predictions and Evaluations
The ASRL model was optimized using tree heights derived from the best GLAS height metric (i.e., HC; Section 4.1) for all the 12 FLUXNET sites. The number of sample GLAS tree heights in the two-fold cross validation varied from 5 to 34 depending on the site (Table S3). A statistically significant relationship (R2 = 0.85; RMSE = 1.81 m; P < 0.01) was obtained when comparing the optimized model predictions with the average of test GLAS tree heights (Figure 6). Kempes et al. similarly tested the adjustment of individual allometric parameters of the ASRL model (e.g., stomatal density and root absorption efficiency) but reported less variation in model errors from the sensitivity analysis.
The optimized values of allometric parameters for the study sites are listed in Table S3. There were notable adjustments in the optimized values of leaf size, α (initial value: 13.0 cm2). It varied from 14.0 cm2 for the US-MMS site to 56.0 cm2 for the US-Ha2 site. This supports the relative significance of selecting α as an additional allometric parameter in model optimization. The other two allometric parameters, exponent for canopy radius, η (initial value: 1.14) and root absorption efficiency, γ (initial value: 0.33), were also adjusted in the optimization with η values ranging from 0.94 for the US-MOz site to 1.24 for the US-Ha1 site and γ ranging from 0.19 for the US-Ho1 site to 0.38 for the US-SP3 site. These parameters were relatively stable compared to α, as previously reported by Kempes et al..
Optimizing three parameters clearly improved model performance. Figure 7 shows the distribution of tree heights over 12 FLUXNET sites. Compared to the unoptimized ASRL model predictions (Figure 7(b)), tree heights from the optimized ASRL model (Figure 7(c)) better resemble GLAS tree heights (Figure 7(a)). As shown in Figure S9, the variance of model errors to the actual observation, “(GLAS tree heights—Predicted tree heights)/GLAS tree heights” , decreased from 0.53 (without optimization) to 0.01 (after optimization).
We performed a second evaluation of the optimized ASRL model at the eco-climatic zone scale (Table S2). Cold and drier regions are characterized by the zone ID 2, while zone ID 1, 3 and 5 represent cold and wetter regions. Zone ID 4 is located in the relatively warm and dry region. This definition of eco-climatic zones is comparable to the traditional eco-climatic zones (e.g., Holdridge life zones )—zone ID 1, 3 and 5 are related to the Cool Temperate Wet Forest, while ID 2 and 4 represent the Cool Temperate Moist Forest and Warm Temperate Dry Forest, respectively.
As shown by the bootstrapping evaluation approach (Figure 8), the optimized model satisfactorily predicted tree heights (R2 = 0.66; RMSE = 2.60 m; P < 0.01). The model’s error variance decreased from 0.60 to 0.02 after optimization (Figure S10). Overall, the optimization successfully alleviated the effect of different environmental conditions and forest types and thus generated a more robust prediction of tree heights at a local scale, as indicated by the results of the two evaluation approaches. However, our approach did not consider the error propagation related to uncertainties in such input climatic variables and the GLAS waveform data, which are critical inputs to the optimized ASRL model. Input climate data may have produced large uncertainties due to the interpolation of climatic variables that are sensitive to terrain conditions (e.g., [74,75]). Model predictions and evaluations carry certain constraints that GLAS tree heights are taken as true values of tree heights in spite of inherent uncertainties in GLAS waveform data: topographic effects  might not be completely corrected from GLAS data. In addition, GLAS undersampling for some of the climatic zones results in fewer comparison sets in the optimization process, that is, increasing uncertainties.
5. Concluding Remarks
The Allometric Scaling and Resource Limitations (ASRL) model optimized with the Geoscience Laser Altimeter System (GLAS) waveform data was tested at site scale (12 FLUXNET sites over the continental USA) in this second of a multi-article series. The model predicts potential tree heights based on local energy budgets limited by water, radiation, wind and air temperature. Predicted potential tree heights differ from observations due to homogeneous scaling parameters and exponents across different eco-climatic zones and forest types with varying age classes. Model optimization in this study is aimed at minimizing the difference between model predictions and observations (i.e., GLAS tree heights). This study considered three allometric parameters (area of single leaf, α; exponent for canopy radius, η; and root absorption efficiency, γ) for model optimization.
Amongst the five GLAS metrics (HA–E) indicative of tree heights, the best GLAS metric (HC) was used in model optimization. We conducted comparisons showing the closeness between: (a) Laser Vegetation Imaging Sensor (LVIS) tree heights and field measurements (R2 = 0.76; RMSE = 4.13 m) and (b) the five GLAS metrics of tree heights and LVIS tree heights (R2 = 0.70; RMSE = 4.42 m for HC). This best GLAS metric (HC) was retrieved from the distance between the last Gaussian peak and signal beginning of the GLAS waveform and incorporated topographic effect correction.
The optimized model prediction was evaluated using two-fold cross validation and bootstrapping exercises. Predicted tree heights explained 85% of the variability in GLAS tree heights and on average showed an estimation error of 1.81 units of height from the two-fold cross validation approach at the studied sites. The variance of model errors to observation decreased from 0.53 to 0.01 after model optimization. In the case of bootstrapping, the study sites were stratified into five eco-climatic zones based on dominant forest type, annual total precipitation and annual average temperature. This exercise also resulted in a satisfactory prediction of GLAS tree heights by the optimized model (R2 = 0.66; RMSE = 2.60 m) and a decrease in model error variance from 0.60 to 0.02 after optimization.
This investigation at site scale provides evidence corroborating our initial study  to the need for optimization and utility of the ASRL model with the ultimate goal of generating spatially continuous maps of tree heights and biomass. Optimization with remote sensing altimetry data successfully takes into account the external effect imposed by different eco-climatic regimes and forest types. The ASRL model was clearly improved by the parametric optimization showing the potential of the model in mapping tree heights. Nevertheless, the results from this site-specific analysis cannot be generalized due to the limited number of study sites and available GLAS waveform data. The studied sites did not cover the full range of precipitation, temperature and forest types prevalent across the continental USA. The optimized ASRL model has certain limitations due to (a) uncertainties of input climate and GLAS data and (b) a limited number of parameters explored in the optimization. Also, forest stand ages were not directly involved in the model optimization.
Forthcoming investigations will focus on extending the model formulation using similar concepts for the estimation of woody biomass (next two articles in preparation). Also, our approach will be tested over different study locations (e.g., China and Amazon Basin) to generalize the results for mapping global tree heights and biomass. A future research will be conducted over Amazon Basin where eco-climatic regimes and forest types are quite different from the CONUS. The availability of input climate data with good quality is certainly a challenge in this study region. Additionally, eco-climatic regimes and forest types of some regions in China may resemble those of the CONUS, but scaling parameters of the ASRL model are not necessarily identical. Hence, we will investigate the feasibility of the ASRL model in various regions by obtaining the appropriate scaling parameters.
This study was partially funded by the National Natural Science Foundation of China (grants no. 40801139 and 41175077), China Scholarship Council and the Fulbright Foundation.
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|Table 1. Datasets for inter-comparisons between field measured and Laser Vegetation Imaging Sensor (LVIS) waveform derived heights. There are 82 measurement plots spanning seven field sites in this study.|
|Sites||Field Measured Data||LVIS Data|
|Subplots||Acquisition Year||Plot Size (m)||References||Acquisition Year|
|La Selva Biological Station, Costa Rica||30||2006||10 × 100||[20,21]||2005|
|Barro Colorado Island, Panama||20||2000||100 × 100||[29–31]||1998|
|Penobscot Experimental Forest, Maine, USA||12||2009||50 × 200||[32,33]||2003|
|Sierra National Forest, California, USA||8||2008||100 × 100||[34,35]||2008|
|Harvard Forest, Massachusetts, USA||2||2007||100 × 100||2003|
|2||2009||50 × 50|
|Howland Research Forest, Maine, USA||2||2007||100 × 100||2003|
|2||2009||50 × 50|
|Bartlett Experimental Forest, New Hampshire, USA||2||2007||100 × 100||2003|
|2||2009||50 × 50|
|Table 2. Datasets for inter-comparisons between LVIS derived heights and Geoscience Laser Altimeter System (GLAS) height metrics (six different sites used in this study).|
|Sites||LVIS Data||GLAS Data|
|White River Wildlife Refuge, AR, USA||2006||2003–2006|
|Sierra Nevada, CA, USA||2008||2003–2006|
|Harvard Forest, MA, USA||2003||2003–2006|
|Patapsco Forest, MD, USA||2003||2003–2006|
|Howland Research Forest and Penobscot Experimental Forest, ME, USA||2003||2003–2006|
|Bartlett Experimental Forest, NH, USA||2003||2003–2006|
|Table 3. The 12 FLUXNET sites selected for analysis in this study based on the distance between a site and valid GLAS footprints (≤10 km radius). The three dominant forest types at these sites are Evergreen Needleleaf Forest (ENF), Deciduous Broadleaf Forest (DBF), and Mixed Forests (MF). Percent tree cover values were derived from the MODIS VCF product.|
|FLUXNET SITE ID||Site Name||Location||Temporal Range of Data||Forest Types||% Tree Cover||Valid GLAS Footprints|
|US-Me1||Metolius Eyerly Burn||OR, USA||2004–2005||ENF||63||29|
|US-Syv||Sylvania Wilderness Area||MI, USA||2001–2006||MF||52||33|
|US-Ha1||Harvard Forest EMS Tower||MA, USA||1992–2006||DBF||74||68|
|US-Ho1||Howland Forest (main tower)||ME, USA||1996–2004||ENF||73||33|
|US-MMS||Morgan Monroe State Forest||IN, USA||1999–2006||DBF||70||18|
|US-Bar||Bartlett Experimental Forest||NH, USA||2004–2006||DBF||93||12|
|US-Ha2||Harvard Forest Hemlock Site||MA, USA||2004||ENF||74||67|
|US-MOz||Missouri Ozark Site||MO, USA||2004–2007||DBF||51||64|
|US-Ho2||Howland Forest (west tower)||ME, USA||1999–2004||ENF||74||31|
|US-LPH||Little Prospect Hill||MA, USA||2003–2005||DBF||73||68|
|US-WCr||Willow Creek||WI, USA||1999–2006||DBF||51||9|
|Table 4. Five possible GLAS height metrics based on Gaussian decomposition approach and topographic effect correction. Statistical analysis examining the full GLAS waveform extents [24,55,58,59] is beyond the scope of this study.|
|GLAS Height Metrics||Applied GLAS Waveform Parameters||Topographic Effect Correction||References|
|HA||SigBegOff − gpCntRngOff 1||No||[22,51,60]|
|HB||SigBegOff − SigEndOff||No|||
|HC||SigBegOff − gpCntRngOff 1||Yes||[14,37,56]|
|HD||SigBegOff − SigEndOff||Yes||-|
|HE||SigBegOff − 2 × gpCntRngOff 1 + SigEndOff||No||-|