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Both heliographic and heliocentric coordinates are discussed.
Accepted assumptions concerning the dependence of the diffusion coefficients on the coordinates are discussed.
In addition the geometrical contributions to the mass transfer coefficient for spherical and cylindrical coordinates are discussed.
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The effects of particles size distribution on spectral reflectivity, optimization parameter, and color coordinates were discussed.
The convenience offered by the body-fixed coordinates is discussed across various fields.
The concept of absolute natural coordinates is discussed to model rigid bodies in order to satisfy the constraints of modularity.
The possibility of using the data to refine the unit cell parameters and the atomic coordinates is discussed.
Properties of sections of coordinate maps are discussed in [21, Section 3].
Detailed descriptions about coordinate transformations are discussed by Hartley and Zisserman (2003).
The interactive features of the parallel coordinate representations are discussed, with particular emphasis on their ability to facilitate geographic data exploration and understanding.
The technical details of specifying the orthonormal coordinates forming ζ are discussed in Appendix A.
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