An individual simulation from Set A showing the annual latitudinal climate of Gl 514 b (ε = 3﹩\mathop{.}\limits^{{\unicode{x000b0}}}﹩0, ψ = 90°, and pCO₂ = 8.375 bar). Top left: insolation received by the planet. Top right: surface temperature. Bottom left: ice mass balance. A positive value represents ice accumulation while a negative value represents ice melting. Bottom right: outgoing longwave radiation.