Abstract
Radiative transfer models (RTMs) of vegetation canopies can be applied for the retrieval of numerical values of vegetation properties from satellite data. For such retrieval, it is necessary first to apply atmospheric correction to translate the top-of-atmosphere (TOA) satellite data into top-of-canopy (TOC) values. This atmospheric correction typically assumes a Lambertian surface reflection, which introduces errors if the real surface is non-Lambertian. Furthermore, atmospheric correction requires atmospheric characterization as input, which is not always available. In this study, we present an RTM for soil-plant-atmosphere systems to model TOC and TOA reflectance as observed by sensors, and to retrieve vegetation properties directly from TOA reflectance skipping the atmosphere correction processes with the inversion mode of the RTM. The model uses three computationally efficient RTMs for soil (BSM), vegetation canopies (PROSAIL) and atmosphere (SMAC), respectively. The sub-models are coupled by using the four-stream theory and the adding method. The resulting ‘Soil-Plant-Atmosphere Radiative Transfer model’ (SPART) simulates directional TOA spectral observations, with all major effects included, such as sun-observer geometries and non-Lambertian reflectance of the land surface. A sensitivity anaylsis of the model shows that neglecting anisotropic reflection of the surface in coupling the surface with atmosphere causes considerable errors in TOA reflectance. The model was validated by comparing TOC and TOA reflectance simulations with those simulated with the atmosphere-included version of the DART RTM model. We show that the differences between DART and SPART are less than 7% for simulating TOC reflectance, and are less than 20% (less than 10% at most bands) for simulating TOA reflectance. The model performance in retrieving key vegetation and atmospheric properties was evaluted by using a synthetic dataset and a satellite dataset. The inversion mode allows estimating vegetation properties along with atmospheric properties and TOC reflectance with reasonable accuracy directly from TOA observations, and remarkable accuracy can be achieved if prior information is used in the model inversion. The model can be used to investigate the sensitivity of surface and atmospheric properties on TOC and TOA reflectance and for the simulation of synthetic data of existing and forthcoming satellite missions. More importantly, it facilitates a quantitative use of remote sensing data from satellites directly without the need for atmospheric correction.
Highlights
Earth observation satellites in the optical domain enable monitoring of the status of vegetation canopies
The overall objective of this study is to develop an invertible Radiative transfer models (RTMs) for the combined system of a soil surface, a vegetation layer and an atmosphere layer, that can facilitate the operational retrieval of surface properties from TOA radiance without knowing atmospheric properties
Compared to the difference in the simulated TOC reflectance, the TOA reflectance simulated by DART and Soil-PlantAtmosphere Radiative Transfer model’ (SPART) show larger differences (Fig. 10), in particular at the blue bands and the oxygen absorption feature
Summary
Earth observation satellites in the optical domain enable monitoring of the status of vegetation canopies. Spectroradiometer (MODIS) since 1999 (Justice et al, 1998) and the Sentinel missions since 2010s (Drusch et al, 2012; Donlon et al, 2012) This development has stimulated the development of operational methods for the quantification of vegetation and atmosphere characteristics from top-of-atmosphere (TOA) radiance or reflectance observations by satellites. Radiative transfer problems in the canopy can be solved numerically using techniques like Monte Carlo ray tracing (North, 1996; Disney et al, 2000) or analytically using techniques like the four-stream theory (Verhoef, 1985) and discrete ordinates (Knyazikhin et al, 1992) These have resulted a number of vegetation RTMs, such as the Suits model (Suits, 1971), the SAIL model (Verhoef, 1984), the DART model (Gastellu-Etchegorry et al, 1996, 2015) and the FLIGHT model (North, 1996). Among all atmospheric RTMs, MODTRAN (MODerate resolution atmospheric TRANsmission, Berk et al, 2005) and 6S (Second Simulation of a Satellite Signal in the Solar Spectrum, Vermote et al, 1997) have found a wide application in the field of remote sensing due to their reasonable compromise between model simplicity and realism
Sign-in/Register to view highlights & summary Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
