Upper Ocean Mixing and Oxygen Utilization Rates in the Changing Sargasso Sea with Development of an Improved Beryllium-7 Sampling System
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Oceanographers often use radioactive elements coming from the atmosphere to estimate how quickly the ocean circulates. For example, radiocarbon, which decays over thousands of years, can be used to determine that ocean currents travel from the surface to the deep sea in about 300 to 1000 years, depending on where you are. Radiocarbon decay is…
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