Well the altitde in <span>the atmosphere in which the stratospheric ozone can be found is 82 km. So the closest would be 70 km.</span>
Major conflict Against the background of the clash between the poor greasers and the rich Socs, the greaser Ponyboy struggles to mature. rising action Johnny kills a Soc; Johnny and Ponyboy flee; tension mounts between the greasers and Socs.
IamSugarBee
The <span>narrow belts of fast-moving air at the higher levels of the troposphere are called jet streams. The paths of the jet streams can be best described as meandering. Jet streams can start or stop or split or move in the reverse direction at any time. I hope that the answer has come to your great help.</span>
Answer: A) Ocean instability due to the vertical temperature profile of the top 100 meters
Explanation:
Ocean instability are due to the vertical temperature profile of the top 100 meter are not main drivers for the surface ocean current as, the surface ocean currents are derived by the velocity of the wind and the coriolis effects. Deep water current and the circulations current are driven by the changes in the salinity and the temperature which is also known as density currents.