Long-term comparative study reveals parallels between time series from Florida and Newfoundland
Researchers from the University of Bremen and the Federal Maritime and Hydrographic Agency have compared long-term data on the Atlantic Meridional Overturning Circulation from two different latitudes and discovered a statistical correlation. Their aim was to investigate how the Atlantic Meridional Overturning Circulation has developed over a period of 25 years, based on moored observation stations. These data will help to refine climate models in the future. The study has been published in the journal Geophysical Research Letters.
In addition to wind, temperature and salinity are the driving forces of ocean currents in the North Atlantic. They transport warm, salty water from the subtropical regions northward to the colder, lower-salinity areas. Like the wind-driven Gulf Stream, these currents are components of the Atlantic Meridional Overturning Circulation (AMOC). Because of the immense amount of heat it transports, the AMOC is an important part of the global climate system. For example, it influences regional precipitation as well as strong tropical storms, and acts as a remote heating system for Europe’s climate.
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