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Simulating global dynamic surface reflectances for imaging spectroscopy spaceborne missions - LPJ-PROSAIL
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  • Benjamin Poulter,
  • Bryce Currey,
  • Leonardo Calle,
  • Jack Brookshire,
  • Petya Campbell,
  • Adam Chlus,
  • Kerry Cawse-Nicholson,
  • Karl Fred Huemmrich,
  • Charles E. Miller,
  • Kimberley Miner,
  • Zoe Amie Pierrat,
  • David Schimel,
  • Shawn Paul Serbin,
  • Alexey N Shiklomanov,
  • E. Natasha Stavros,
  • Philip A Townsend,
  • David Ray Thompson,
  • Zhen Zhang,
  • Cibele Amaral,
  • Ann Raiho,
  • Jochen Stutz
Benjamin Poulter
NASA

Corresponding Author:[email protected]

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Bryce Currey
Montana State University
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Leonardo Calle
Montana State University
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Jack Brookshire
Montana State University
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Petya Campbell
University of Maryland, Joint Center for Environmental Technology (UMBC-JCET)
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Adam Chlus
Jet Propulsion Laboratory
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Kerry Cawse-Nicholson
Jet Propulsion Laboratory, California Institute of Technology
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Karl Fred Huemmrich
University of Maryland, Baltimore County
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Charles E. Miller
Jet Propulsion Laboratory
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Kimberley Miner
Jet Propulsion Laboratory
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Zoe Amie Pierrat
UCLA
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David Schimel
Jet Propulsion Laboratory
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Shawn Paul Serbin
Brookhaven National Laboratory (DOE)
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Alexey N Shiklomanov
NASA Goddard Space Flight Center
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E. Natasha Stavros
University of Colorado Boulder
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Philip A Townsend
University of Wisconsin–Madison
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David Ray Thompson
Jet Propulsion Laboratory, California Institute of Technology
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Zhen Zhang
University of Maryland
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Cibele Amaral
CU Boulder
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Ann Raiho
NASA
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Jochen Stutz
University of California Los Angeles
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Abstract

Imaging spectroscopy is a remote-sensing technique that retrieves reflectances across visible to shortwave infrared wavelengths at high spectral resolution (<10 nm). Spectroscopic reflectance data provide novel information on the properties of the Earth’s terrestrial and aquatic surfaces. Until recently, imaging spectroscopy missions were limited spatially and temporally using airborne instruments, such as the Next Generation Airborne Visible InfraRed Imaging Spectrometer (AVIRIS-NG), providing the main source of observations. Here, we present a land-surface modeling framework to help support end-to-end traceability of emerging imaging spectroscopy spaceborne missions. 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. 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, and a tropical forest site using reflectance data from canopy imagers mounted on towers and from air and spaceborne platforms. 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 can support missions such as NASA’s Surface Biology and Geology (SBG) and higher-level modeled products.