Spatiotemporal variability and long-term trends of ocean acidification in the California Current System

C. Hauri, N. Gruber, M. Vogt, S. C. Doney, R. A. Feely, Zouhair Lachkhar, A. Leinweber, A. M.P. McDonnell, M. Munnich

Research output: Contribution to journalArticle

Abstract

Due to seasonal upwelling, the upper ocean waters of the California Current System (CCS) have a naturally low pH and aragonite saturation state (Ωarag), making this region particularly prone to the effects of ocean acidification. Here, we use the Regional Oceanic Modeling System (ROMS) to conduct preindustrial and transient (1995-2050) simulations of ocean biogeochemistry in the CCS. The transient simulations were forced with increasing atmospheric CO2 and increasing oceanic dissolved inorganic carbon concentrations at the lateral boundaries, as projected by the NCAR CSM 1.4 model for the IPCC SRES A2 scenario. Our results show a large seasonal variability in pH (range of ∼ 0.14) and Ωarag (∼ 0.2) for the nearshore areas (50 km from shore). This variability is created by the interplay of physical and biogeochemical processes. Despite this large variability, we find that present-day pH and Ωarag have already moved outside of their simulated preindustrial variability envelopes (defined by ±1 temporal standard deviation) due to the rapidly increasing concentrations of atmospheric CO2. The nearshore surface pH of the northern and central CCS are simulated to move outside of their present-day variability envelopes by the mid-2040s and late 2030s, respectively. This transition may occur even earlier for nearshore surface Ωarag, which is projected to depart from its present-day variability envelope by the early-to mid-2030s. The aragonite saturation horizon of the central CCS is projected to shoal into the upper 75 m within the next 25 yr, causing near-permanent undersaturation in subsurface waters. Due to the model's overestimation of Ωarag, this transition may occur even earlier than simulated by the model. Overall, our study shows that the CCS joins the Arctic and Southern oceans as one of only a few known ocean regions presently approaching the dual threshold of widespread and near-permanent undersaturation with respect to aragonite and a departure from its variability envelope. In these regions, organisms may be forced to rapidly adjust to conditions that are both inherently chemically challenging and also substantially different from past conditions.

Original languageEnglish (US)
Pages (from-to)193-216
Number of pages24
JournalBiogeosciences
Volume10
Issue number1
DOIs
StatePublished - Jan 28 2013

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aragonite
ocean
saturation
oceans
dissolved inorganic carbon
upper ocean
biogeochemistry
simulation
upwelling
water
modeling
long-term trend
ocean acidification
Arctic region
seawater
seasonal variation
carbon
organisms

ASJC Scopus subject areas

  • Ecology, Evolution, Behavior and Systematics
  • Earth-Surface Processes

Cite this

Spatiotemporal variability and long-term trends of ocean acidification in the California Current System. / Hauri, C.; Gruber, N.; Vogt, M.; Doney, S. C.; Feely, R. A.; Lachkhar, Zouhair; Leinweber, A.; McDonnell, A. M.P.; Munnich, M.

In: Biogeosciences, Vol. 10, No. 1, 28.01.2013, p. 193-216.

Research output: Contribution to journalArticle

Hauri, C, Gruber, N, Vogt, M, Doney, SC, Feely, RA, Lachkhar, Z, Leinweber, A, McDonnell, AMP & Munnich, M 2013, 'Spatiotemporal variability and long-term trends of ocean acidification in the California Current System', Biogeosciences, vol. 10, no. 1, pp. 193-216. https://doi.org/10.5194/bg-10-193-2013
Hauri, C. ; Gruber, N. ; Vogt, M. ; Doney, S. C. ; Feely, R. A. ; Lachkhar, Zouhair ; Leinweber, A. ; McDonnell, A. M.P. ; Munnich, M. / Spatiotemporal variability and long-term trends of ocean acidification in the California Current System. In: Biogeosciences. 2013 ; Vol. 10, No. 1. pp. 193-216.
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