Normally, temperatures decrease with height in the troposphere , because the earth absorbs solar radiation and acts as a heating element for the air above. Occasionally, temperatures will increase with height in a small layer of the tropopause. We call this a temperature inversion . From about 20-50 km above earth's surface. The zone of ozone concentration.
Temperatures increase with height.
From 50-80 km above earth's surface. Temperatures decrease with height. Topped by mesopause. Temperatures increase with height, individual molecules are rare, but bombarded by unfiltered solar radiation.