Table 5 Comparison of the difference between the \(\mathrm TOC_{HM(PDE)}\) and \(\mathrm TOC_{HM(TLE)}\) hemisphere means for different phases of the planet
From: Characterising the three-dimensional ozone distribution of a tidally locked Earth-like planet
Phase \(\varphi\) | \(\Delta \mathrm{TOC}_{\mathrm{HM(PDE,TLE)}}\) (DU) | \(\Delta \mathrm{TOC}_{\mathrm{HM(PDE,TLE)}}\) (%) | \(\Delta \mathrm{TOC}_{\mathrm{HM(TLE,TLE)}}\) (%) | \(\Delta \mathrm{TOC}_{\mathrm{HM(PDE,PDE)}}\) (%) |
|---|---|---|---|---|
\(0\)° | \(-\)56 | 23 | 0 | 0 |
\(90\)° | \(-\)51 | 22 | 2.2 | 3.5 |
\(180\)° | \(-\)39 | 16 | \(-\)3.8 | 2.7 |
\(270\)° | \(-\)13 | 12 | \(-\)8.1 | 1.4 |