Related Experiment Video
Updated: Jan 25, 2026

10:28
Investigating the Relationship between Sea Surface Chlorophyll and Major Features of the South China Sea with Satellite Information
Published on: June 13, 2020
6.3K
Optimal satellite orbit configuration for global ocean color product coverage
Optics Express
|May 5, 2019
Summary
Optimizing satellite orbits is key for daily ocean color data. A 90° phase shift for the next Joint Polar Satellite System (JPSS) satellite can maximize global ocean color retrievals, minimizing coverage gaps.
Area of Science:
- Earth Observation Science
- Satellite Remote Sensing
- Oceanography
Background:
- The Visible Infrared Imaging Radiometer Suite (VIIRS) is crucial for monitoring ocean color.
- Current satellite constellations (SNPP, NOAA-20) face limitations in daily global coverage.
- Optimizing orbital configurations is necessary for enhanced data acquisition.
Purpose of the Study:
- To develop a methodology for evaluating current and future VIIRS orbital configurations.
- To maximize global daily ocean color retrievals from polar-orbiting satellites.
- To identify optimal orbital phasing for the Joint Polar Satellite System (JPSS) series.
Main Methods:
- Evaluating orbital configurations of SNPP and NOAA-20 VIIRS.
- Analyzing coverage losses due to sensor-zenith angles and sun glint.
- Simulating various orbital scenarios for future JPSS satellites.
Main Results:
- Two current sensors (SNPP, NOAA-20) cannot achieve complete daily global coverage.
- High sensor-zenith angles and sun glint significantly reduce ocean color data.
- A 90° phase shift for the JPSS-2 satellite relative to SNPP and NOAA-20 maximizes daily retrievals.
Conclusions:
- Complete daily global ocean color coverage is unachievable with the current two-satellite configuration.
- Strategic orbital phasing, specifically a 90° shift for JPSS-2, is essential for maximizing ocean color data.
- Future satellite mission planning must consider orbital dynamics to enhance Earth observation capabilities.
Related Concept Videos
Energy of a Satellite in a Circular Orbit
3.0K
Thousands of artificial satellites orbit the Earth every day at various distances from the Earth. Satellites that orbit the Earth below an altitude of 1,600 km are considered to be orbiting in low-Earth orbit (LEO). Research satellites and Earth observation satellites are usually placed in LEO, and mostly orbit the Earth in elliptical orbits. Navigation satellites are placed in medium-Earth orbit (MEO), ranging from 2,000 km to 36,000 km from the surface of the Earth. Meanwhile, communication...
3.0K
Circular Orbits and Critical Velocity for Satellites
5.5K
The Moon orbits around the Earth. In turn, the Earth (and other planets) orbit the Sun. The space directly above our atmosphere is filled with artificial satellites in orbit. One can examine the circular orbit, the simplest kind of orbit, to understand the relationship between the speed and the period of planets and satellites with respect to their positions and the bodies that they orbit.
Nicolaus Copernicus (1473-1543) first suggested that the Earth and all other planets orbit the Sun in...
Nicolaus Copernicus (1473-1543) first suggested that the Earth and all other planets orbit the Sun in...
5.5K
Electron Orbital Model
72.0K
Orbitals are the areas outside of the atomic nucleus where electrons are most likely to reside. They are characterized by different energy levels, shapes, and three-dimensional orientations. The location of electrons is described most generally by a shell or principal energy level, then by a subshell within each shell, and finally, by individual orbitals found within the subshells.
The first shell is closest to the nucleus, and it has only one subshell with a single spherical orbital called the...
The first shell is closest to the nucleus, and it has only one subshell with a single spherical orbital called the...
72.0K
Electron Configuration of Multielectron Atoms
64.7K
The alkali metal sodium (atomic number 11) has one more electron than the neon atom. This electron must go into the lowest-energy subshell available, the 3s orbital, giving a 1s22s22p63s1 configuration. The electrons occupying the outermost shell orbital(s) (highest value of n) are called valence electrons, and those occupying the inner shell orbitals are called core electrons. Since the core electron shells correspond to noble gas electron configurations, we can abbreviate electron...
64.7K
Colors and Magnetism
14.0K
Color in Coordination Complexes
When atoms or molecules absorb light at the proper frequency, their electrons are excited to higher-energy orbitals. For many main group atoms and molecules, the absorbed photons are in the ultraviolet range of the electromagnetic spectrum, which cannot be detected by the human eye. For coordination compounds, the energy difference between the d orbitals often allows photons in the visible range to be absorbed and emitted, which is seen as colors by the human...
When atoms or molecules absorb light at the proper frequency, their electrons are excited to higher-energy orbitals. For many main group atoms and molecules, the absorbed photons are in the ultraviolet range of the electromagnetic spectrum, which cannot be detected by the human eye. For coordination compounds, the energy difference between the d orbitals often allows photons in the visible range to be absorbed and emitted, which is seen as colors by the human...
14.0K
Atomic Orbitals
43.5K
An atomic orbital represents the three-dimensional regions in an atom where an electron has the highest probability to reside. The radial distribution function indicates the total probability of finding an electron within the thin shell at a distance r from the nucleus. The atomic orbitals have distinct shapes which are determined by l, the angular momentum quantum number. The orbitals are often drawn with a boundary surface, enclosing densest regions of the cloud.
43.5K

