Climate change and wind intensification in coastal upwelling ecosystems-Reference-Cited by-同舟云学术

Climate change and wind intensification in coastal upwelling ecosystems

Published:2014-07-04 Issue:6192 Volume:345 Page:77-80
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Sydeman W. J.¹,García-Reyes M.¹,Schoeman D. S.²,Rykaczewski R. R.³,Thompson S. A.¹⁴,Black B. A.⁵,Bograd S. J.⁶

Affiliation:

1. Farallon Institute for Advanced Ecosystem Research, Suite Q, 101 H Street, Petaluma, CA 94952, USA.

2. Faculty of Science, Health, Education and Engineering, University of the Sunshine Coast, Locked Bag 4, Maroochydore DC, Queensland 4558, Australia.

3. Department of Biological Sciences and Marine Science Program, University of South Carolina, 701 Sumter Street, Columbia, SC 29208, USA.

4. Climate Impacts Group, University of Washington, Box 355674, Seattle, WA 98195, USA.

5. Marine Science Institute, University of Texas, 750 Channel View Drive, Port Aransas, TX 78373, USA.

6. Environmental Research Division, National Oceanic and Atmospheric Administration (NOAA) Southwest Fisheries Science Center, 1352 Lighthouse Avenue, Pacific Grove, CA 93950-2097, USA.

Abstract

Strong winds, upwelling, and teeming shores Climate warming has produced stronger winds along some coasts, a result of growing differences in temperature and pressure between land and sea. These winds cause cold nutrient-rich seawater to rise to the surface, affecting climate and fueling marine productivity. Sydeman et al. examined data from the five major world regions where upwelling is occurring. Particularly in the California, Humboldt, and Benguela upwelling systems, winds have become stronger over the past 60 years. These regions represent up to a fifth of wild marine fish catches and are hot spots of biodiversity. Science , this issue p. 77

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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