Under Pressure: Climate Change, Upwelling, and Eastern Boundary Upwelling Ecosystems
Open accessAbstract
The IPCC AR5 provided an overview of the likely effects of climate change on Eastern Boundary Upwelling Systems (EBUS), stimulating increased interest in research examining the issue. We use these recent studies to develop a new synthesis describing climate change impacts on EBUS. We find that model and observational data suggest coastal upwelling-favorable winds in poleward portions of EBUS have intensified and will continue to do so in the future. Although evidence is weak in data that are presently available, future projections show that this pattern might be driven by changes in the positioning of the oceanic high-pressure systems rather than by deepening of the continental low-pressure systems, as previously proposed. There is low confidence regarding the future effects of climate change on coastal temperatures and biogeochemistry due to uncertainty in the countervailing responses to increasing upwelling and coastal warming, the latter of which could increase thermal stratification and render upwelling less effective in lifting nutrient-rich deep waters into the photic zone. Although predictions of ecosystem responses are uncertain, EBUS experience considerable natural variability and may be inherently resilient. However, multi-trophic level, end-to-end (i.e., “winds to whales”) studies are needed to resolve the resilience of EBUS to climate change, especially their response to long-term trends or extremes that exceed pre-industrial ranges.
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Equatorward upwelling-favorable winds have been observed to increase in strength in most EBUS.
“Moreover, equatorward upwelling-favorable winds were observed to be increasing their strength in most EBUS (Bakun, 1990;García-Reyes et al., 2015;Sydeman et al., 2014).”
From Recent Trends in SST, Chl‐<i>a</i>, Productivity and Wind Stress in Upwelling and Open Ocean Areas in the Upper Eastern North Atlantic Subtropical Gyre (2021) · cites this paper as García-Reyes et al., 2015
The Trends in Upwelling-Favorable Winds section reports intensifying winds in three EBUS—the Humboldt and California systems during the warm season, and the Benguela system in annual data. That supports the claim's 'most EBUS' count, but the sentence omits the seasonal qualification and the paper's finding that Canary trends are equivocal. (LLM, conf=0.84)
Experimental — accuracy not yet measuredWarming in coastal areas increases stratification and inhibits vertical nutrient exchange, limiting productivity.
“Warming in coastal areas increases the stratification and inhibits the vertical nutrient exchange limiting the productivity (Brady et al., 2019;Di Lorenzo et al., 2005;Garcia-Reyes et al., 2015).”
From Recent Trends in SST, Chl‐<i>a</i>, Productivity and Wind Stress in Upwelling and Open Ocean Areas in the Upper Eastern North Atlantic Subtropical Gyre (2021) · cites this paper as Garcia-Reyes et al., 2015
The ‘Water Temperatures and the Counteracting Roles of Upwelling and Stratification’ section says surface warming increases stratification, which can reduce the nutrients brought into the euphotic zone and thereby affect productivity. But the paper discusses this mechanism in eastern boundary upwelling systems and says its productivity effects depend on upwelling winds; it does not establish the claim as an unqualified outcome across coastal areas. No page number is supplied in our copy. (LLM, conf=0.82)
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Warming up, turning sour, losing breath: ocean biogeochemistry under global change
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Barton, E. D., Field, D. B., & Roy, C. (2013) · Progress in Oceanography · doi:10.1016/j.pocean.2013.07.007 · Cited by 134 · cited 5× · see citing works
“In part, this is a result of the substantial spatial heterogeneity in physical characteristics within EBUS, which emphasizes the role of local processes and resultant local biotic effects (Nelson and Hutchings, 1983; Dorman and Winant, 1995; Barton et al., 2013; Bakun et al., 2015).”
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- Authors
- García-Reyes, M., Sydeman, W. J., Schoeman, D. S., Rykaczewski, R. R., Black, B. A., Smit, A. J., & Bograd, S. J.
- Affiliations
- Farallon Institute (US)
- University of the Sunshine Coast (AU)
- University of South Carolina (US)
- University of Texas at Austin Marine Science Institute (US)
- University of the Western Cape (ZA)
- NOAA National Marine Fisheries Service Southwest Fisheries Science Center (US)
- ORCID
- Venue
- Frontiers in Marine Science
- Publisher
- Frontiers Media SA
- Published
- 2015-12-16
- Volume
- 2
- ISSN
- 2296-7745 (ISSN-L)
- OpenAlex
- W2216244657
- Cited by
- 272
- References
- 5
- Citations by year
- 2026: 23 · 2025: 27 · 2024: 35 · 2023: 34 · 2022: 34 · 2021: 33 · 2020: 27 · 2019: 24 · 2018: 20 · 2017: 9 · 2016: 4
- FWCI
- 9.16
- Type
- journal article
- Language
- en
- Open access
- gold
- dx.doi.org
- Licence
- cc-by
- Locations
- Frontiers in Marine Science (publishedVersion, cc-by)
- DOAJ (DOAJ: Directory of Open Access Journals) (submittedVersion, cc-by-sa)
- NOAA Institutional Repository (submittedVersion, cc-by)
- Funders
- National Science Foundation (1434732)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and coastal ecosystems
- Physical Sciences › Environmental Science › Global and Planetary Change › Marine and fisheries research
- Keywords
- climate change impacts, eastern boundary upwelling systems, coastal upwelling, upwelling-favorable winds, coastal warming, thermal stratification, nutrient upwelling, biogeochemistry, ecosystem resilience, IPCC AR5, natural variation
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