As the CO2 and CH4 (methane) level goes up, H2O
vapour in the atmosphere falls which — because H2O is 30 times more important
than CO2 as a «greenhouse gas» offsets the effect of CO2 on temperature, while cloud cover and albedo increases because
warmed moist
air rises to form clouds, further cooling the world.
Air containing water in vapour form will rise higher than dry air because it is lighter so when the vapour is removed it must fall back to its «correct» height but because of the air around it becoming warmer as it descends it will remain too dense for its height until it reaches the ground and receives more energy from the irradiated surfa
Air containing water in
vapour form will rise higher
than dry
air because it is lighter so when the vapour is removed it must fall back to its «correct» height but because of the air around it becoming warmer as it descends it will remain too dense for its height until it reaches the ground and receives more energy from the irradiated surfa
air because it is lighter so when the
vapour is removed it must fall back to its «correct» height but because of the
air around it becoming warmer as it descends it will remain too dense for its height until it reaches the ground and receives more energy from the irradiated surfa
air around it becoming
warmer as it descends it will remain too dense for its height until it reaches the ground and receives more energy from the irradiated surface.