Unidad Océano y Clima, Instituto de Oceanografía y Cambio Global, IOCAG, Universidad de Las Palmas de Gran Canaria, ULPGC, Unidad Asociada ULPGC-CSIC, Canary Islands, Spain
Centro Oceanográfico de Canarias, Instituto Español de Oceanografía – Consejo Superior de Investigaciones Científicas (IEO-CSIC), Santa Cruz de Tenerife, Canary Islands, Spain
Unidad Océano y Clima, Instituto de Oceanografía y Cambio Global, IOCAG, Universidad de Las Palmas de Gran Canaria, ULPGC, Unidad Asociada ULPGC-CSIC, Canary Islands, Spain
Centro Oceanográfico de Canarias, Instituto Español de Oceanografía – Consejo Superior de Investigaciones Científicas (IEO-CSIC), Santa Cruz de Tenerife, Canary Islands, Spain
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1,703
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Cumulative views and downloads
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Total article views: 1,925 (including HTML, PDF, and XML)
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1,332
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1,925
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PDF: 306
XML: 287
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Supplement: 98
BibTeX: 73
EndNote: 75
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371
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Total article views: 2,419 (including HTML, PDF, and XML)
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Total article views: 1,925 (including HTML, PDF, and XML)
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Total article views: 494 (including HTML, PDF, and XML)
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Eastern boundary upwelling systems (EBUSs) are crucial for resources, but climate change poses uncertainties for their future. To assess global warming's impact, we examine Andrew Bakun's 1990 hypothesis of intensified upwelling using deseasonalized sea surface temperature data. A new index, αUI, normalizes upwelling trends against non-upwelling processes, confirming intensification in all EBUSs and supporting Bakun's hypothesis.
Eastern boundary upwelling systems (EBUSs) are crucial for resources, but climate change poses...
