Solution
= Solution
<Methane> reaching the <stratosphere> is oxidized and is an important source of stratospheric <water vapor>. That <water> can feed <HOx radical family> chemistry and alter <radiative cooling> and polar-cloud conditions. <Methane> also converts <chlorine> atoms into <hydrogen chloride>, opposing some chlorine-driven <ozone> loss. These effects compete: increasing <methane> does not have one universal <ozone> sign at every altitude and latitude.