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Journal Article

Atmospheric Lengthscales for Global VSWIR Imaging Spectroscopy

Authors

Thompson,  David R.
External Organizations;

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Bohn,  Niklas
1.4 Remote Sensing, 1.0 Geodesy, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Brodrick,  Philip G.
External Organizations;

Carmon,  Nimrod
External Organizations;

Eastwood,  Michael L.
External Organizations;

Eckert,  Regina
External Organizations;

Fichot,  Cédric G.
External Organizations;

Harringmeyer,  Joshua P.
External Organizations;

Nguyen,  Hai M.
External Organizations;

Simard,  Marc
External Organizations;

Thorpe,  Andrew K.
External Organizations;

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Fulltext (public)

5012589.pdf
(Publisher version), 2MB

Supplementary Material (public)
There is no public supplementary material available
Citation

Thompson, D. R., Bohn, N., Brodrick, P. G., Carmon, N., Eastwood, M. L., Eckert, R., Fichot, C. G., Harringmeyer, J. P., Nguyen, H. M., Simard, M., Thorpe, A. K. (2022): Atmospheric Lengthscales for Global VSWIR Imaging Spectroscopy. - Journal of Geophysical Research: Biogeosciences, 127, 6, e2021JG006711.
https://doi.org/10.1029/2021JG006711


Cite as: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5012589
Abstract
Future global Visible Shortwave Infrared Imaging Spectrometers, such as the Surface Biology and Geology (SBG) mission, will regularly cover the Earth's entire terrestrial land area. These missions need high fidelity atmospheric correction to produce consistent maps of terrestrial and aquatic ecosystem traits. However, estimation of surface reflectance and atmospheric state is computationally challenging, and the terabyte data volumes of global missions will exceed available processing capacity. This article describes how missions can overcome this bottleneck using the spatial continuity of atmospheric fields. Contemporary imaging spectrometers oversample atmospheric spatial variability, so it is not necessary to invert every pixel. Spatially sparse solutions can train local linear emulators that provide fast, exact inversions in their vicinity. We find that estimating the atmosphere at 200 m scales can outperform traditional atmospheric correction, improving speed by one to two orders of magnitude with no measurable penalty to accuracy. We validate performance with an airborne field campaign, showing reflectance accuracies with RMSE of 1.1% or better compared to ground measurements of diverse targets. These errors are statistically consistent with retrieval uncertainty budgets. Local emulators can close the efficiency gap and make rigorous model inversion algorithms feasible for global missions such as SBG.