Response to Temperature of a Class of In Situ Hyperspectral Radiometers
The response to temperature of sample hyperspectral radiometers commonly used to support the validation
of satellite ocean color data was characterized in the 400–800-nm spectral range. Measurements performed in the
10–40C interval at 5C increments showed mean temperature coefficients varying from -0.04x10-2 (C)-1 at
400 nm to +0.33x10-2 (C)-1 at 800 nm, which are largely explained by the temperature coefficient of the
photodetector array constituting the core of the sensor. Overall, the results indicate the possibility of applying
temperature corrections with an uncertainty of approximately 0.03x10-2 (C)-1 for the class of hyperspectral
radiometers investigated in the study.
ZIBORDI Giuseppe;
TALONE Marco;
JANKOWSKI Lukasz;
2017-08-24
AMER METEOROLOGICAL SOC
JRC106262
0739-0572,
http://journals.ametsoc.org/doi/10.1175/JTECH-D-17-0048.1,
https://publications.jrc.ec.europa.eu/repository/handle/JRC106262,
10.1175/JTECH-D-17-0048.1,
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