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The primary TLE ozone layer is also characterised by altitude variations (Fig. 4c, d), which are present in both the day side and the night side, but are much less pronounced compared to the PDE (Fig. 4a, b).
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This is due to the transport of odd oxygen from the day side to the night side through both the horizontal and vertical circulation, where it recombines to form ozone.
The day side ionosphere is driven by photoionization.
Therefore, the TLE mesospheric day night side variation is (sim 43 % with respect to the day side.
A tidally locked planet can be divided into the day side and the night side.
The day side ionosphere will be broader with larger densities than the night side ionosphere.
On the day side, potential is around 5 V and on the night side it reaches up to −82 V.
Shades of red indicate high incoming solar radiation and define the day side of the planet.
Shades of red indicate high temperatures and define the day side of the planet.
On the TLE, ozone is only generated on the day side.
The day side is the permanently illuminated hemisphere that is always facing the parent star.
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