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Atmosphere

Across
The number of particle in the air.
The natural rain barriers.
The layer of atmosphere that ranges from 10 to 50 km up.
The currant temperature/precipitation.
The natural conveyor belt of air.
The area of land on the leeward side of of a mountain that gets little to no rain.
The higher air pressure over the ocean causes this.
Down
The layer of atmosphere that ranges from 50 to 85 km up.
When the air pressure is higher over the land this happens.
The lowest layer of atmosphere.
The layer of atmosphere that contains the most ozone.
The average temperature/precipitation.
The outermost layer of the atmosphere.
The time when the air pressure in the western pacific ocean decreases, and the air pressure in the eastern pacific ocean increases.
An effect every 2 to 7 years that causes Peru, north, and south America's air pressure over the coast to decrease.