Dependence of refractive index (RI) of seawater on salinity, temperature and wavelength n (S, T, λ) in infrared band is required.However, almost all the existing empirical formulas of the RI of seawater are suitable for the visible waveband (400 nm - 700 nm). There is little report on developing the RI expression of seawater in infrared band, especially the most commonly used 1200 nm - 1650 nm waveband.

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[1] Shan-Shan Wang, "All 500 sets of data used in theoretical fitting", IEEE Dataport, 2023. [Online]. Available: http://dx.doi.org/10.21227/ke54-bm18. Accessed: May. 23, 2024.
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doi = {10.21227/ke54-bm18},
url = {http://dx.doi.org/10.21227/ke54-bm18},
author = {Shan-Shan Wang },
publisher = {IEEE Dataport},
title = {All 500 sets of data used in theoretical fitting},
year = {2023} }
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T1 - All 500 sets of data used in theoretical fitting
AU - Shan-Shan Wang
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Shan-Shan Wang. (2023). All 500 sets of data used in theoretical fitting. IEEE Dataport. http://dx.doi.org/10.21227/ke54-bm18
Shan-Shan Wang, 2023. All 500 sets of data used in theoretical fitting. Available at: http://dx.doi.org/10.21227/ke54-bm18.
Shan-Shan Wang. (2023). "All 500 sets of data used in theoretical fitting." Web.
1. Shan-Shan Wang. All 500 sets of data used in theoretical fitting [Internet]. IEEE Dataport; 2023. Available from : http://dx.doi.org/10.21227/ke54-bm18
Shan-Shan Wang. "All 500 sets of data used in theoretical fitting." doi: 10.21227/ke54-bm18