6.4.7—Ozone depletion effects

Syllabus
First assessment 2026
Objective
6.4.7
Level
HL

Define an Ozone Hole by Concentration and Season

An ozone hole is a seasonal region of unusually low stratospheric ozone, especially over polar areas—not a literal opening in the atmosphere.

Polar stratospheric clouds support reactions that activate chlorine; spring sunlight drives rapid catalytic loss. The reduced shield raises surface UV and can affect health and ecosystems.

Antarctic spring measurements show a seasonal low-ozone area that expands and contracts rather than remaining a permanent hole.

A measured regional concentration anomaly over time, not a photograph or one day’s UV reading.

The ozone hole is not uniform global ozone disappearance; location and season are essential.