Cited by 315Oceanographic and Atmospheric ProcessesClimate variability and modelsMarine and fisheries research

Phenology of coastal upwelling in the California Current

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Bograd, Steven J., Schroeder, Isaac, Sarkar, Nandita, Qiu, Xuemei, Sydeman, William J., Schwing, Franklin B.·2009·Geophysical Research Letters

Abstract

Changes in the amplitude and phasing of seasonal events (phenology) can affect the functioning of marine ecosystems. Phenology plays a particularly critical role in eastern boundary ecosystems, which are driven largely by the seasonal cycle of coastal upwelling. Here we develop and describe a set of indicators that quantify the timing, evolution, intensity, and duration of coastal upwelling in the California Current large marine ecosystem (CCLME). There is significant interannual variability in upwelling characteristics during 1967–2007, with extended periods of high (1970s, 1998–2004) and low (1980–1995) seasonally‐integrated upwelling and a trend towards a later and shorter upwelling season in the northern CCLME. El Niño years were characterized by delayed and weak upwelling in the central CCLME. Understanding the causes and ecosystem consequences of phenological changes in coastal upwelling is critical, as climate models project significant variability in the amplitude and phase of coastal upwelling under varying climate change scenarios.

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References 31 · Cited by 315

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  1. Barth, J. A., B. A. Menge, J. Lubchenco, F. Chan, J. M. Bane, A. R. Kirincich, M. A. McManus, K. J. Nielsen, S. D. Pierce, and L. Washburn (2007), Delayed upwelling alters nearshore coastal ecosystems in the northern California Current, Proc. Natl. Acad. Sci. U. S. A., 104(10), 3719 -3724.
  2. Bograd, S., F. Schwing, R. Mendelssohn, and P. Green-Jessen (2002), On the changing seasonality over the North Pacific, Geophys. Res. Lett., 29(9), 1333, doi:10.1029/2001GL013790. · DOI
  3. Brodeur, R. D., S. Ralston, R. L. Emmett, M. Trudel, T. D. Auth, and A. J. Phillips (2006), Anomalous pelagic nekton abundance, distribution, and apparent recruitment in the northern California Current in 2004 and 2005, Geophys. Res. Lett., 33, L22S08, doi:10.1029/2006GL026614. · DOI
  4. Diffenbaugh, N. S. (2005), Response of large-scale eastern boundary current forcing in the 21st century, Geophys. Res. Lett., 32, L19718, doi:10.1029/2005GL023905. · DOI
  5. Diffenbaugh, N. S., M. A. Snyder, and L. C. Sloan (2004), Could CO 2 - induced land-cover feedbacks alter nearshore upwelling regimes?, Proc. Natl. Acad. Sci. U. S. A., 101(1), 27 -32.
  6. Durant, J. M., D. O. Hjermann, G. Ottersen, and N. C. Stenseth (2007), Climate and the match or mismatch between predator requirements and resource availability, Clim. Res., 33(2), 271 -283.
  7. Kosro, P. M., W. T. Peterson, B. M. Hickey, R. K. Shearman, and S. D. Pierce (2006), Physical versus biological spring transition: 2005, Geo- phys. Res. Lett., 33, L22S03, doi:10.1029/2006GL027072. · DOI
  8. Lenarz, W. H., D. A. VenTresca, W. M. Graham, F. B. Schwing, and F. Chavez (1995), Explorations of El Nin ˜o events and associated biological population dynamics off central California, CalCOFI Rep. 36, pp. 106 - 119, Cal. Coop. Oceanic Fish. Invest., La Jolla, Calif.
  9. Mackas, D. L., W. T. Peterson, M. D. Ohman, and B. E. Lavaniegos (2006), Zooplankton anomalies in the California Current system before and dur- ing the warm ocean conditions of 2005, Geophys. Res. Lett., 33, L22S07, doi:10.1029/2006GL027930. · DOI · Paper page
  10. Mote, P. W., and N. J. Mantua (2002), Coastal upwelling in a warmer future, Geophys. Res. Lett., 29(23), 2138, doi:10.1029/2002GL016086. · DOI · Paper page
  11. Pierce, S. D., J. A. Barth, R. E. Thomas, and G. W. Fleischer (2006), Anomalously warm July 2005 in the northern California Current: Histor- ical context and the significance of cumulative wind stress, Geophys. Res. Lett., 33, L22S04, doi:10.1029/2006GL027149. · DOI
  12. Rykaczewski, R. R., and D. M. Checkley Jr. (2008), Influence of ocean winds on the pelagic ecosystem in upwelling regions, Proc. Natl. Acad. Sci. U. S. A., 105(6), 1965 -1970.
  13. Schwing, F. B., N. A. Bond, S. J. Bograd, T. Mitchell, M. A. Alexander, and N. Mantua (2006), Delayed coastal upwelling along the U.S. West Coast in 2005: A historical perspective, Geophys. Res. Lett., 33, L22S01, doi:10.1029/2006GL026911. · DOI · Paper page
  14. Snyder, M. A., L. C. Sloan, N. S. Diffenbaugh, and J. L. Bell (2003), Future climate change and upwelling in the California Current, Geophys. Res. Lett., 30(15), 1823, doi:10.1029/2003GL017647. · DOI · Paper page
  15. Stenseth, N. C., and A. Mysterud (2002), Climate, changing phenology, and other life history traits: Nonlinearity and match-mismatch to the environ- ment, Proc. Natl. Acad. Sci. U. S. A., 99(21), 13,379 -13,381.
  16. Thomas, A. C., and P. Brickley (2006), Satellite measurements of chloro- phyll distribution during spring 2005 in the California Current, Geophys. Res. Lett., 33, L22S05, doi:10.1029/2006GL026588. · DOI · Paper page
  17. Weise, M. J., D. P. Costa, and R. M. Kudela (2006), Movement and diving behavior of male California sea lion (Zalophus californianus) during anomalous oceanographic conditions of 2005 compared to those of 2004, Geophys. Res. Lett., 33, L22S10, doi:10.1029/2006GL027113. · DOI

Authors
Bograd, S. J., Schroeder, I., Sarkar, N., Qiu, X., Sydeman, W. J., & Schwing, F. B.
Affiliations
  • National Oceanic and Atmospheric Administration (US)
  • Farallon Institute (US)
Venue
Geophysical Research Letters
Published
2009-01
Volume
36
Issue
1
ISSN
  • 0094-8276 (ISSN-L)
  • 1944-8007
OpenAlex
W2029036899
Cited by
315
References
31
Citations by year
2026: 12 · 2025: 22 · 2024: 25 · 2023: 29 · 2022: 15 · 2021: 20 · 2020: 14 · 2019: 12 · 2018: 15 · 2017: 24 · 2016: 17 · 2015: 21 · 2014: 19 · 2013: 30 · 2012: 10
FWCI
6.93
Type
journal article
Language
en
Open access
Locations
Geophysical Research Letters (publishedVersion)
Funders
National Oceanic and Atmospheric Administration
Topics
  • Physical Sciences › Earth and Planetary Sciences › Oceanography › Oceanographic and Atmospheric Processes
  • Physical Sciences › Environmental Science › Global and Planetary Change › Climate variability and models
  • Physical Sciences › Environmental Science › Global and Planetary Change › Marine and fisheries research
Keywords
coastal upwelling, phenology, California Current, eastern boundary upwelling systems, interannual variability, El Niño, upwelling intensity, climate change projections

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