The statement that should describe the temperature of the region at the equator is that it can be associated with perpendicular solar radiation.
The Equator line at zero (0) latitude is an imaginary line that divides the Earth's planet into two equal parts composed of South latitudes and North latitudes.
Temperatures at low latitudes, i.e., near the Equator line, are warmer because this region receives perpendicular solar rays all the year, thereby the energy of solar radiation is distributed to the Earth's surface.
In conclusion, the statement that should describe the temperature of the region at the equator is that it can be associated with perpendicular solar radiation.
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