Unraveling plant phenotype to genotype associations with daily hyperspectral traits in <i>Populus trichocarpa</i>. [PDF]
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Net Primary Productivity Retrieval Based on ESTARFM Fusion and an Improved CASA Model. [PDF]
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Integrating Multi-Source and Multi-Temporal UAV Observations to Improve Wheat Yield Prediction Using Machine Learning. [PDF]
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Satellite remote sensing enables monitoring of soil organic carbon decline in croplands of Jilin China. [PDF]
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An Integrated Pixel-Level Reflectance Adjustment (IPRA) for Harmonizing GF-1/6 WFV and Sentinel-2 MSI Data. [PDF]
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Model for the interpretation of hyperspectral remote-sensing reflectance
Applied Optics, 1994Remote-sensing reflectance is easier to interpret for the open ocean than for coastal regions because the optical signals are highly coupled to the phytoplankton (e.g., chlorophyll) concentrations. For estuarine or coastal waters, variable terrigenous colored dissolved organic matter (CDOM), suspended sediments, and bottom reflectance, all factors that
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Errors in the remotely sensed ocean reflectance
Advances in Space Research, 1987Abstract An approximate method has been described to determine optical properties of the ocean surface from the reflected short-wave radiance at the top of the atmosphere. The non-scattered and singly scattered components of the radiation field have been taken into account exactly, the multiply scattered components - approximately.
S. Keevallik, A. Heinlo
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Remote sensing reflectance anomalies in the ocean
Remote Sensing of Environment, 2016Small spectral differences from the mean remote sensing reflectance (Rrs) of the ocean – anomalies – can provide unique environmental information from ocean color satellite data. First, we describe the average relationship between three input spectral bands and an output band by developing a look-up table (LUT) based on the fully normalized Rrs from ...
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Modeling the remote-sensing reflectance of highly turbid waters
Applied Optics, 2019In ocean-color remote sensing, subsurface remote-sensing reflectance (r r s ) of optically deep waters can be linked to its absorption (a) and backscattering coefficients (b b ) by various models. The use of such models allows for quick calculations r r s from such coefficients, eliminating the need to solve the radiative transfer equation.
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