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The Great Salinity Anomaly (GSA) originally referred to an event in the late 1960s to early 1970s where a large influx of freshwater from the Arctic Ocean led to a salinity anomaly in the northern North Atlantic Ocean, which affected the Atlantic meridional overturning circulation. Since then, the term "Great Salinity Anomaly" has been applied to successive occurrences of the same phenomenon, including the Great Salinity Anomaly of the 1980s and the Great Salinity Anomaly of the 1990s. The Great Salinity Anomalies were advective events, propagating to different sea basins and areas of the North Atlantic, and is on the decadal-scale for the anomalies in the 1970s, 1980s, and 1990s.

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  • The Great Salinity Anomaly (GSA) originally referred to an event in the late 1960s to early 1970s where a large influx of freshwater from the Arctic Ocean led to a salinity anomaly in the northern North Atlantic Ocean, which affected the Atlantic meridional overturning circulation. Since then, the term "Great Salinity Anomaly" has been applied to successive occurrences of the same phenomenon, including the Great Salinity Anomaly of the 1980s and the Great Salinity Anomaly of the 1990s. The Great Salinity Anomalies were advective events, propagating to different sea basins and areas of the North Atlantic, and is on the decadal-scale for the anomalies in the 1970s, 1980s, and 1990s. (en)
  • Великая солёностная аномалия (ВСА, англ. Great Salinity Anomaly) — наблюдавшееся в северной части Атлантического океана в конце 1960-х годов явление, заключавшееся в существенном (до 1 промилле) уменьшении солёности морской воды в прилегающем к поверхности 200-метровом слое. (ru)
  • Велика солонісна аномалія (ВСА, англ. Great Salinity Anomaly) — явище, що спостерігалося в північній частині Атлантичного океану наприкінці 1960-х років і полягало в істотному (до 1 проміле) зменшенні солоності морської води у прилеглому до поверхні 200-метровому шарі. (uk)
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  • The Great Salinity Anomaly (GSA) originally referred to an event in the late 1960s to early 1970s where a large influx of freshwater from the Arctic Ocean led to a salinity anomaly in the northern North Atlantic Ocean, which affected the Atlantic meridional overturning circulation. Since then, the term "Great Salinity Anomaly" has been applied to successive occurrences of the same phenomenon, including the Great Salinity Anomaly of the 1980s and the Great Salinity Anomaly of the 1990s. The Great Salinity Anomalies were advective events, propagating to different sea basins and areas of the North Atlantic, and is on the decadal-scale for the anomalies in the 1970s, 1980s, and 1990s. (en)
  • Великая солёностная аномалия (ВСА, англ. Great Salinity Anomaly) — наблюдавшееся в северной части Атлантического океана в конце 1960-х годов явление, заключавшееся в существенном (до 1 промилле) уменьшении солёности морской воды в прилегающем к поверхности 200-метровом слое. (ru)
  • Велика солонісна аномалія (ВСА, англ. Great Salinity Anomaly) — явище, що спостерігалося в північній частині Атлантичного океану наприкінці 1960-х років і полягало в істотному (до 1 проміле) зменшенні солоності морської води у прилеглому до поверхні 200-метровому шарі. (uk)
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  • Great Salinity Anomaly (en)
  • Великая солёностная аномалия (ru)
  • Велика солонісна аномалія (uk)
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