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One of these coordinates is based on the radial flow behaviour.
A formal system for incorporation of these coordinates into FITS files, based on the FITS World Coordinate System, is described.
A subset of these coordinates is then taken as the design variables for a nonlinear optimization problem where new target physical properties are sought.
The estimation of these coordinates and the iso-p VLE by the UNIFAC method are acceptable but do not give good predictions of the hE even less so for the LLE of the methyl methanoate + pentane system.
On the basis of these coordinates, it is possible to identify a series of anthropometric measurements and angles that can provide a guide and tool for surgeons and orthodontists involved in the reevaluation of female faces.
A comparison of these coordinates with results of recent landing site investigations using visual and radar images of the Cassini VIMS instrument shows excellent agreement of the two independently derived landing coordinates, i.e., longitude and latitude residuals of respectively 0.035 deg and 0.007 deg.
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We use a combination of these coordinate systems to represent the magnetic field.
The extension of these coordinate systems to observations made from non-terrestial viewpoints, such as STEREO and Solar Probe, is discussed.
The first of these, coordinated by Wehmiller (this edition), used homogeneous hydrolysates of Pleistocene mollusc and eggshell materials and focused on the agreement of analytical measurements between laboratories, without interference from differing sample preparation procedures.
The choice of these coordinate axes was motivated by a previous modeling study [19] that suggested that the (o+i) pool of ERG potassium channels was the appropriate slow variable for a fast/slow analysis.
Work is ongoing to clarify the putative tandem activity of these coordinate sRNAs.
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