Inorganic carbon dynamics during northern California coastal upwelling

Andrea J. Fassbender, Christopher L. Sabine, Richard A. Feely, Chris Langdon, Calvin W. Mordy

Research output: Contribution to journalArticle

29 Citations (Scopus)

Abstract

Coastal upwelling events in the California Current System can transport subsurface waters with high levels of carbon dioxide (CO2) to the sea surface near shore. As these waters age and are advected offshore, CO2 levels decrease dramatically, falling well below the atmospheric concentration beyond the continental shelf break. In May 2007 we observed an upwelling event off the coast of northern California. During the upwelling event subsurface respiration along the upwelling path added ~35γmolkg-1 of dissolved inorganic carbon (DIC) to the water as it transited toward shore causing the waters to become undersaturated with respect to Aragonite. Within the mixed layer, pCO2 levels were reduced by the biological uptake of DIC (up to 70%), gas exchange (up to 44%), and the addition of total alkalinity through CaCO3 dissolution in the undersaturated waters (up to 23%). The percentage contribution of each of these processes was dependent on distance from shore. At the time of measurement, a phytoplankton bloom was just beginning to develop over the continental shelf. A box model was used to project the evolution of the water chemistry as the bloom developed. The biological utilization of available nitrate resulted in a DIC decrease of ~200γmolkg-1, sea surface pCO2 near ~200ppm, and an aragonite saturation state of ~3. These results suggest that respiration processes along the upwelling path generally increase the acidification of the waters that are being upwelled, but once the waters reach the surface biological productivity and gas exchange reduce that acidification over time.

Original languageEnglish
Pages (from-to)1180-1192
Number of pages13
JournalContinental Shelf Research
Volume31
Issue number11
DOIs
StatePublished - Aug 1 2011

Fingerprint

inorganic carbon
upwelling
carbon dioxide
acidification
gas exchange
carbon
dissolved inorganic carbon
hydrochemistry
alkalinity
algal blooms
water
aragonite
continental shelf
nitrates
sea surface
algal bloom
respiration
coasts
biological uptake
shelf break

Keywords

  • Acidification
  • California
  • Carbon
  • Continental shelf
  • Phytoplankton
  • Upwelling

ASJC Scopus subject areas

  • Aquatic Science
  • Geology
  • Oceanography

Cite this

Inorganic carbon dynamics during northern California coastal upwelling. / Fassbender, Andrea J.; Sabine, Christopher L.; Feely, Richard A.; Langdon, Chris; Mordy, Calvin W.

In: Continental Shelf Research, Vol. 31, No. 11, 01.08.2011, p. 1180-1192.

Research output: Contribution to journalArticle

Fassbender, Andrea J. ; Sabine, Christopher L. ; Feely, Richard A. ; Langdon, Chris ; Mordy, Calvin W. / Inorganic carbon dynamics during northern California coastal upwelling. In: Continental Shelf Research. 2011 ; Vol. 31, No. 11. pp. 1180-1192.
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