Significant disturbance caused by a major pulse of freshwater input to the Nordic Seas
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.[1] 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[2] and the Great Salinity Anomaly of the 1990s.[3] 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.
^Dima, Mihai; Lohmann, Gerrit. Causes and Consequences of the Late 1960s Great Salinity Anomaly, Planet Earth 2011 - Global Warming Challenges and Opportunities for Policy and Practice. InTech. ISBN 978-953-307-733-8.
^Belkin, Igor M (1998). ""Great Salinity Anomalies" in the North Atlantic". Progress in Oceanography. 41 (1): 1–68. Bibcode:1998PrOce..41....1B. doi:10.1016/S0079-6611(98)00015-9.
^Belkin, Igor M (2004). "Propagation of the "Great Salinity Anomaly" of the 1990s around the northern North Atlantic". Geophysical Research Letters. 31 (8). Bibcode:2004GeoRL..31.8306B. doi:10.1029/2003GL019334. S2CID 128813097.
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the water quality around the Great Barrier Reef. Another consequence of land clearing is dryland salinity. Dryland salinity is the movement of salt to the...
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increase in salinity shows that evaporation is increasing even more. The same goes for regions of low salinity that are becoming less saline, which indicates...
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wavelengths reveal larger scale surface information, e.g. regional thermal anomalies, surface roughness, etc. Such techniques are particularly beneficial for...
cycles accompanied by salinity changes, estuaries for example, may see vertical migration in some species of zooplankton. Salinity has also been proposed...
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