Sensors that can be used for the observation of ocean color in NASA's Earth Observing
System era (SeaWiFS, MODIS, and MISR) have been designed with 2–4 times the …

By validation of atmospheric correction, we mean quantification of the uncertainty expected
to be associated with the retrieval of the water‐leaving radiance from the measurement of …

A radiative transfer code termed OSOA for the ocean–atmosphere system that is able to
predict the total and the polarized signals has been developed. The successive-orders-of …

To recover the ocean water-leaving radiance and derive biophysical parameters from
observations of space-borne ocean color sensors, the required uncertainty in the measured …

We simulate vicarious calibration (VC) of a Sea-viewing Wide Field-of-view Sensor
(SeaWiFS)-like ocean color sensor relative to its longer near infrared (NIR) spectral band …

Synchronous observations with similar illumination-observation and meteorological
conditions are critical components of cross-calibration analysis. This study outlines data …

Radiometric vicarious calibration of ocean color (OC) satellite sensors is carried out through
the full sunlight path radiative transfer (RT) simulations of the coupled ocean–atmosphere …

Comparing inter-mission space instrument performance is crucial to accurate satellite
measurements which guarantees the quality of ocean color products. However, comparing …

The single‐scattering albedo and phase function of African mineral dust are retrieved at 14
wavelengths across the visible spectrum from ground‐based measurements of the aerosol …

The variability of phase functions of submicrometer atmospheric aerosols was studied using
Mie theory. In the analyzed statistical ensemble of phase functions, the effective radii of …