Fig. 3From: The middle atmospheric circulation of a tidally locked Earth-like planet and the role of the sea surface temperatureCTLE, WTLE and PDE atmospheric temporal evolution. a TOC. b HW. c Ω. d T. The CTLE and WTLE TOC, HW, and T are exponentially decaying to their steady-state value with an e-folding time of 30, 20, and 40 days, respectively. The CTLE and WTLE vertical winds are exponentially increasing to their steady-state value with an e-folding time of 15 daysBack to article page