Polar stratospheric clouds and ozone depletion

• Main Authors: Toon, Owen B., Turco, Richard P.
• Format: Other/Unknown Material
• Language: unknown
• Published: 1991
• Subjects: 46; Antarctic; Austral; The Antarctic; Antarc*; Antarctica
• Online Access: http://ntrs.nasa.gov/search.jsp?R=19910052350

A review is presented of investigations into the correlation between the depletion of ozone and the formation of polar stratospheric clouds (PSCs). Satellite measurements from Nimbus 7 showed that over the years the depletion from austral spring to austral spring has generally worsened. Approximately 70 percent of the ozone above Antarctica, which equals about 3 percent of the earth's ozone, is lost during September and October. Various hypotheses for ozone depletion are discussed including the theory suggesting that chlorine compounds might be responsible for the ozone hole, whereby chlorine enters the atmosphere as a component of chlorofluorocarbons produced by humans. The three types of PSCs, nitric acid trihydrate, slowly cooling water-ice, and rapidly cooling water-ice clouds act as important components of the Antarctic ozone depletion. It is indicated that destruction of the ozone will be more severe each year for the next few decades, leading to a doubling in area of the Antarctic ozone hole.