Stratosphere
		Standard Atmosphere				q  The reasons for the inversion in the stratosphere is due to the ozone absorption of ultraviolet solar energy. q  Although maximum ozone concentration occurs at 25km, the lower air density at 50km allows solar energy to heat up temperature there at a much greater degree. q  Also, much solar energy is absorbed in the upper stratosphere and can not reach the level of ozone maximum.
	lapse rate = 6.5 C/km