Rapid 20th-Century Increase in Coastal Upwelling off Northwest Africa

Near-shore waters along the northwest African margin are characterized by coastal upwelling and represent one of the world's major upwelling regions. Sea surface temperature (SST) records from Moroccan sediment cores, extending back 2500 years, reveal anomalous and unprecedented cooling during...

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Veröffentlicht in:Science (American Association for the Advancement of Science) 2007-02, Vol.315 (5812), p.637-639
Hauptverfasser: McGregor, H.V, Dima, M, Fischer, H.W, Mulitza, S
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container_title Science (American Association for the Advancement of Science)
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creator McGregor, H.V
Dima, M
Fischer, H.W
Mulitza, S
description Near-shore waters along the northwest African margin are characterized by coastal upwelling and represent one of the world's major upwelling regions. Sea surface temperature (SST) records from Moroccan sediment cores, extending back 2500 years, reveal anomalous and unprecedented cooling during the 20th century, which is consistent with increased upwelling. Upwelling-driven SSTs also vary out of phase with millennial-scale changes in Northern Hemisphere temperature anomalies (NHTAs) and show relatively warm conditions during the Little Ice Age and relatively cool conditions during the Medieval Warm Period. Together, these results suggest that coastal upwelling varies with NHTAs and that upwelling off northwest Africa may continue to intensify as global warming and atmospheric CO₂ levels increase.
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source American Association for the Advancement of Science; Jstor Complete Legacy
subjects Atmospherics
Carbon dioxide
Coasts
Cooling
Datasets
Earth sciences
Earth, ocean, space
Exact sciences and technology
Geophysics
Global warming
Marine
Marine and continental quaternary
Marine geology
Oceanography
Oceans
Proxy reporting
Proxy statements
Sea water
Surface water
Surficial geology
Upwelling water
Water temperature
title Rapid 20th-Century Increase in Coastal Upwelling off Northwest Africa
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