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North and south of the equatorial strip the dry season increases in severity with latitude.
The equatorial strip that extends from the Atlantic Ocean to the Western Rift Valley is influenced throughout the year by the intertropical convergence zone (ITCZ), resulting in intense, heavy precipitation.
However, the eye as a whole is divided into three distinct parts: a dorsal region, a ventral region, and an equatorial strip of ommatidia (see Fig. 5).
Ommatidia in the equatorial strip, typically arranged into six rows (but sometimes only two or three rows), have visual fields that sample only a planar slice through visual space, placed about midway within the overlapping fields of the surrounding ommatidia.
This set of nuclei is distributed in an equatorial strip.
If an equatorial strip encircles with the whole equator, we obtain a parallelepiped with circular topology on the equatorial coordinate and can apply the circular version of SSA [ 39].
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The equatorial strips of ommatidia are specialized for high-quality color vision and for analyzing the polarization of light.
Equatorial strips can be nonconvex and of varying width; hence we need more sophisticated processing than above.
Due to the small number of nuclei in the equatorial strips, we do not estimate the noise model.
For data in equatorial strips, we use the equidistant cylindrical projection [ 38, Section 12], maintaining distances of points to the equator (i.e., latitudes) and distances between points on the equator.
The African sector, in general, has the largest landmass under the equatorial anomaly strip, with an ionosphere that is characterized with complex electrodynamic structures that are not yet well understood.
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