Simulating Global Dynamic Surface Reflectances for Imaging Spectroscopy Spaceborne Missions: LPJ-PROSAIL
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Author
Poulter, B.
Currey, B.
Calle, L.
Shiklomanov, A.N.
Amaral, C.H.
Brookshire, E.N.J.
Campbell, P.
Chlus, A.
Cawse-Nicholson, K.
Huemmrich, F.
Miller, C.E.
Miner, K.
Pierrat, Z.
Raiho, A.M.
Schimel, D.
Serbin, S.
Smith, W.K.
Stavros, N.
Stutz, J.
Townsend, P.
Thompson, D.R.
Zhang, Z.
Affiliation
School of Natural Resources and the Environment, University of ArizonaIssue Date
2023-01-16Keywords
dynamic global vegetation modelimaging spectroscopy
radiative transfer model
Surface Biology and Geology (SBG)
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John Wiley and Sons IncCitation
Poulter, B., Currey, B., Calle, L., Shiklomanov, A. N., Amaral, C. H., Brookshire, E. N. J., et al. (2023). Simulating global dynamic surface reflectances for imaging spectroscopy spaceborne missions: LPJ-PROSAIL. Journal of Geophysical Research: Biogeosciences, 128, e2022JG006935. https://doi.org/10.1029/2022JG006935Rights
© 2023. American Geophysical Union. All Rights Reserved. This article has been contributed to by U.S. Government employees and their work is in the public domain in the USA.Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
Spectroscopic reflectance data provide novel information on the properties of the Earth's terrestrial and aquatic surfaces. Until recently, imaging spectroscopy missions were dependent mainly on airborne instruments, such as the Next Generation Airborne Visible InfraRed Imaging Spectrometer (AVIRIS-NG), providing limited spatial and temporal observations. Currently, there is an emergence of spaceborne imaging spectroscopy missions, which require advances in end-to-end model support for traceability studies. To provide this support, the LPJ-wsl dynamic global vegetation model is coupled with the canopy radiative transfer model, PROSAIL, to generate global, gridded, daily visible to shortwave infrared (VSWIR) spectra (400–2,500 nm). LPJ-wsl variables are cross-walked to meet required PROSAIL parameters, which include leaf structure, chlorophyll a + b, brown pigment, equivalent water thickness, and dry matter content. Simulated spectra are compared to a boreal forest site, a temperate forest, managed grassland, a dryland and a tropical forest site using reflectance data from tower-mounted, aircraft, and spaceborne imagers. We find that canopy nitrogen and leaf-area index are the most uncertain variables in translating LPJ-wsl to PROSAIL parameters but at first order, LPJ-PROSAIL successfully simulates surface reflectance dynamics. Future work will optimize functional relationships required for improving PROSAIL parameters and include the development of the LPJ-model to represent improvements in leaf water content and canopy nitrogen. The LPJ-PROSAIL model is intended to support missions such as NASA's Surface Biology and Geology and subsequent modeled products related to the carbon cycle and hydrology. © 2023 The Authors. This article has been contributed to by U.S. Government employees and their work is in the public domain in the USA.Note
Public domain articleISSN
2169-8953Version
Final Published Versionae974a485f413a2113503eed53cd6c53
10.1029/2022JG006935
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Except where otherwise noted, this item's license is described as © 2023. American Geophysical Union. All Rights Reserved. This article has been contributed to by U.S. Government employees and their work is in the public domain in the USA.