ABSTRACT
Leaf area index (LAI) is defined as one half of the total green leaf area per unit ground surface area. Its vertical profile is critical for understanding the remote sensing radiative transfer processes. LAI profile has been derived from airborne and spaceborne LiDAR data, such as the Global Ecosystem Dynamics Investigation (GEDI) installed on the International Space Station. However, the capability of various algorithms for the LAI profile estimation with airborne LiDAR is not clearly evaluated, and the estimated LAI profiles, including the GEDI LAI products, are not been fully validated. This study conducted a quantitative retrieval and validation of the LAI profiles using terrestrial and airborne laser scanning (TLS and ALS) and spaceborne GEDI data over a deciduous needleleaf forest site in northern China. The vertical LAI profile was estimated in the field using an upward digital hemispherical photography (DHP) attached to a portable measurement system in 2020 and 2021. A suite of new LiDAR indices combining both LiDAR return number and return intensity was explored for the LAI profile estimation. All LAI profiles obtained from the DHP, TLS, ALS, and GEDI during the leaf-on season and leaf-off season were compared. The DHP shows a good agreement with the TLS LAI profiles (R2 = 0.97). The LAI profile derived from the ALS data using the combined light penetration index (LPIRI) agrees well (R2 ≥0.86) with the DHP, TLS, and GEDI estimates. In general, the LPIRI is advantageous for regional LAI profile mapping from ALS. The GEDI cumulative LAI corresponds well with the DHP during the leaf-on season (R2 = 0.90, RMSE = 0.23), but underestimates during the leaf-off season (R2 = 0.70, RMSE = 0.14, bias=−0.13). The underestimation is attributed to the higher canopy and ground reflectance ratio (ρv/ρg) assigned in the algorithm and the height discrepancy between the GEDI and field measurements. For the GEDI LAI profile product, further validation and improvement are necessary for other biome types and landscape conditions, especially during the leaf-off season.
Highlights
A portable field measurement system was developed to measure the LAI profile.
The combined light penetration index (LPIRI) is recommended for the LAI profile estimation from ALS.
GEDI cumulative LAI performs well during the leaf-on season.
GEDI cumulative LAI shows an underestimation during the leaf-off season.
Nomenclature
θ | = | Zenith angle |
z | = | Height in the canopy |
= | Leaf projection function | |
J0 | = | Transmitted laser pulse energy |
= | Gap fraction at zenith angle θ | |
= | Gap fraction at height z | |
Iraw | = | The raw return intensity |
Icorrected | = | The corrected return intensity |
R0 | = | The range between the ALS instrument and the return |
Rs | = | The standard range (the average flying altitude) |
ρg | = | The ground reflectance |
ρv | = | The canopy reflectance |
Rg | = | The laser energies from the ground return |
Rv(0) | = | The laser energies from the canopy top to bottom |
Rv(z) | = | The laser energies from the canopy top to height z |
Rv1 and Rv2 | = | The canopy return energies from two adjacent footprints |
Rg1 and Rg2 | = | The ground return energies from two adjacent footprints |
R2 | = | Coefficient of determination |
ALS | = | Airborne Laser Scanning |
DEM | = | Digital Elevation Model |
DHP | = | Digital Hemispherical Photography |
GEDI | = | Global Ecosystem Dynamics Investigation |
GLAS | = | Geoscience Laser Altimeter System |
LAI | = | Leaf Area Index |
LAIcum | = | Cumulative Leaf Area Index |
LAIi | = | Leaf Area Index for layer i |
LiDAR | = | Light Detection and Ranging |
PAI | = | Plant Area Index |
RMSE | = | Root Mean Square Error |
SNFP | = | Saihanba National Forest Park |
TLS | = | Terrestrial Laser Scanning |
VSP | = | Vertical Sampling Point |
WAI | = | Woody Area Index |
ABRI | = | Above and Below Ratio Index |
ABRIR | = | Above and Below Ratio Index from Returns |
ABRIInt | = | Above and Below Ratio Index from return Intensity |
ABRIRI | = | Above and Below Ratio Index combining Returns and Intensity |
FCI | = | canopy Fractional Cover Index |
FCIR | = | canopy Fractional Cover Index from Returns |
FCIInt | = | canopy Fractional Cover Index from return Intensity |
FCIRI | = | canopy Fractional Cover Index combining Returns and Intensity |
LPI | = | Light Penetration Index |
LPIR | = | Light Penetration Index from Returns |
LPIInt | = | Light Penetration Index from return Intensity |
LPIRI | = | Light Penetration Index combining Returns and Intensity |
Acknowledgments
This study was mainly supported by the National Natural Science Foundation of China (42171358) and the National Key Research and Development Program of China (2016YFA0600201) to H.F. The TLS data were provided by Dr. Jie Zou, Fuzhou University. The GEDI data are available from the NASA’s Land Processes Distributed Active Archive Center (LP DAAC). Drs. Lu Xu and Lixia Ma helped with the field data collection and the TLS data, respectively. The insightful comments provided by the anonymous reviewers helped improve the manuscript.
Disclosure statement
No potential conflict of interest was reported by the authors.
Data availability statement
The field measurement data in this study are available from the corresponding author, Y.W., upon reasonable request.
Supplementary Material
Supplemental data for this article can be accessed online at https://doi.org/10.1080/15481603.2023.2214987