Time evolution of the midplane thermal and turbulent pressures (a) and the thermal and turbulent velocity dispersions (b) of the diffuse component for model QA10x2. In (a), P _th initially decreases as the gas cools, while P _turb increases rapidly after the gas falls toward midplane and is stirred up by SN explosions. After a few cloud formation and feedback cycles (a few 10 s of Myr), P _th and P _turb reach saturation values of P _th/ k _B ~ 1680 cm ⁻³ K and P _turb/ k _B ~ 5440 cm ⁻³ K, respectively, with a relative fluctuation amplitudes of 0.21 and 0.52. In (b), the velocity dispersions saturate at v _{th, diff} = 3.7 km s ⁻¹ and v _{z, diff} = 6.8 km s ⁻¹, respectively, with relative fluctuation amplitudes of 5% and 30%.