Related Experiment Video
Updated: Jan 8, 2026

09:25
Agarose-based Tissue Mimicking Optical Phantoms for Diffuse Reflectance Spectroscopy
Published on: August 22, 2018
13.1K
Robust spectral optimization algorithms for retrieving inherent optical properties of global oceans
Optics Express
|December 19, 2025
Summary
This study introduces new correlation regularization models to improve ocean color remote sensing accuracy. The developed algorithms enhance spectral optimization by addressing errors in inherent optical properties (IOPs) and atmospheric correction.
Area of Science:
- Oceanography
- Remote Sensing
- Optical Physics
Background:
- Ocean color remote sensing is crucial for global monitoring.
- Spectral optimization methods are key algorithms but sensitive to model and inherent optical property (IOP) errors.
- Existing methods struggle with accuracy due to inherent optical property (IOP) uncertainties.
Purpose of the Study:
- To improve the accuracy of ocean color remote sensing by developing error post-correction methods.
- To explore correlation patterns among inherent optical properties (IOPs) for enhanced inversion.
- To introduce novel correlation regularization models for spectral optimization algorithms.
Main Methods:
- Established cross-regression models for IOP magnitude parameters using in situ data.
- Developed global correlation regularization (G-CoReg) and locally weighted correlation regularization (L-CoReg) models.
- Reformulated semianalytical inversion as a spectral optimization task with correlation constraints.
Main Results:
- G-CoReg and L-CoReg algorithms showed superior accuracy over existing methods on NOMAD and SeaWiFS datasets.
- The new algorithms demonstrated improved robustness against atmospheric correction errors.
- Reduced accuracy degradation was observed with the proposed correlation regularization models.
Conclusions:
- The proposed G-CoReg and L-CoReg models significantly enhance ocean color remote sensing accuracy and robustness.
- Correlation regularization effectively mitigates errors from semianalytical models and atmospheric correction.
- These advancements offer more reliable ocean color data for scientific applications.
Related Concept Videos
Ultraviolet and Visible (UV–Vis) Spectroscopy: Overview
4.4K
Ultraviolet–visible (UV–visible or UV–Vis) spectroscopy is an analytical technique that investigates the interaction between matter and UV–Vis light within the electromagnetic spectrum. This method is widely used for its versatility, simplicity, and relatively quick data acquisition, making it valuable for both qualitative and quantitative analysis. When UV–Vis radiation passes through a material, molecules absorb light depending on the energy required for...
4.4K
Spectrophotometry: Introduction
6.6K
Spectrophotometry is the quantitative measurement of the absorption, reflection, diffraction, or transmission of electromagnetic radiation through a material as a function of the intensity and wavelength of the radiation. A spectrophotometer is a device used to measure the change in the radiation intensity caused by its interaction with the material.
The essential components of a spectrophotometer include a source of electromagnetic radiation, a slot for placing a material to be analyzed, and a...
The essential components of a spectrophotometer include a source of electromagnetic radiation, a slot for placing a material to be analyzed, and a...
6.6K
UV–Vis Spectroscopy: Beer–Lambert Law
6.5K
The Beer-Lambert law describes the relationship between absorbance and concentration, which combines the principles established by scientists Johann Heinrich Lambert and August Beer. Lambert's law states that when light passes through a medium, the loss in intensity is directly proportional to the original intensity and the path length of the light. Beer's law proposed that the transmittance of a solution remains constant if the product of concentration and path length is constant. The modern...
6.5K
UV–Vis Spectroscopy: Woodward–Fieser Rules
28.0K
UV–Visible absorption spectra of conjugated dienes arise from the lowest energy π → π* transitions. The light-absorbing part of the molecule is called the chromophore, and the substituents directly attached to the chromophore are called auxochromes. A strong correlation exists between the absorption maxima, λmax, and the structure of a conjugated π system. The Woodward–Fieser rules predict the value of λmax for a given structure by adding the...
28.0K
Estimation of the Physical Quantities
7.2K
On many occasions, physicists, other scientists, and engineers need to make estimates of a particular quantity. These are sometimes referred to as guesstimates, order-of-magnitude approximations, back-of-the-envelope calculations, or Fermi calculations. The physicist Enrico Fermi was famous for his ability to estimate various kinds of data with surprising precision. Estimating does not mean guessing a number or a formula at random. Instead, estimation means using prior experience and sound...
7.2K
Methods of Obtaining Topography
260
Topography involves measuring and mapping land elevations, natural features, and artificial structures to create accurate representations of the terrain. Topographic surveying relies on traditional and modern methods, each with distinct advantages and limitations.Traditional Surveying Methods:Transit stadia surveys and plane table surveys were widely used traditional surveying methods. These techniques relied on instruments like theodolites and stadia rods for measuring distances and angles,...
260

