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Only coefficients with order ǀmǀ ≤ 1 are used, since we are fitting a latitudinal profile sampled over a partial orbit, with a limited variation of longitude and altitude, and will use quasi-dipole coordinates (see below) to reduce the number of required coefficients.
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The justification for choosing such variables are that latitude is expected to affect the spatial variation of surface temperature, whereas longitude may capture the influence of winds.
For the strong control of the neutral wind, east west electric field has only a small effect on the longitude variation of the ionospheric asymmetry.
Less-direct results have been obtained by examining the variations in TEC as a function of longitude.
We did not observe any spatial variation in the fractal dimension with latitude; however we do report significant spatial variation of the fractal dimension with longitude.
For a direct comparison of variations in longitude, we also show the mean airglow intensity (solid red line) around the latitude of Jicamarca for each time.
This wind effect varies significantly with longitude, due to the variation of magnetic declination and inclination.
According to this idea, we plotted latitudinal variation of NmF2 which was measured in the longitude of Japan.
The Commissioners of Longitude were not known as the Board of Longitude until around the 1760s.
Analysis of temporal variations of neutron flux between summer and winter seasons allowed the creation of multidimensional model of CO2 deposition describing behavior of CO2 condensed mass as a function of longitude, latitude and time.
The longitude convention for Mercury puts the zero of longitude at one of the two hottest points on the surface, as described above.
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