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Award ID contains: 1459563

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  1. ; ; ; ; ; (, Science)
    The high rate of biological productivity in the North Atlantic is stimulated by the advective supply of nutrients into the region via the Gulf Stream (nutrient stream). It has been proposed that the projected future decline in the Atlantic Meridional Overturning Circulation (AMOC) will cause a reduction in nutrient supply and resulting productivity. In this work, we examine how the nutrient stream changed over the Younger Dryas climate reversal that marked the transition out of the last ice age. Gulf Stream nutrient content decreased, and oxygen content increased at the Florida Straits during this time of weakened AMOC. The decreased nutrient stream was accompanied by a reduction in biological productivity at higher latitudes in the North Atlantic, which supports the link postulated in theoretical and modeling studies. 
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  2. ; ; ; (, Paleoceanography and Paleoclimatology)
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  3. ; ; ; (, NOAA National Centers for Environmental Information)
    This archived Paleoclimatology Study is available from the NOAA National Centers for Environmental Information (NCEI), under the World Data Service (WDS) for Paleoclimatology. The associated NCEI study type is Climate Reconstruction. The data include parameters of paleoceanography with a geographic location of North Atlantic Ocean. The time period coverage is from 1930 to -52 in calendar years before present (BP). See metadata information for parameter and study location details. Please cite this study when using the data. 
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