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A novel method for determination of aragonite saturation state on the continental shelf of central Oregon using multi-parameter relationships with hydrographic data

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Title A novel method for determination of aragonite saturation state on the continental shelf of central Oregon using multi-parameter relationships with hydrographic data
Names Juranek, L. W. (creator)
Freely, R. A. (creator)
Peterson, W. T. (creator)
Alin, S. R. (creator)
Hales, Burke (creator)
Lee, K. (creator)
Sabine, C. L. (creator)
Peterson, J. (creator)
Date Issued 2009-12-31 (iso8601)
Note Copyrighted by American Geophysical Union.
Abstract We developed a multiple linear regression model to
robustly determine aragonite saturation state (Ωarag) from
observations of temperature and oxygen (R² = 0.987, RMS
error 0.053), using data collected in the Pacific Northwest
region in late May 2007. The seasonal evolution of Ωarag near
central Oregon was evaluated by applying the regression
model to a monthly (winter)/bi-weekly (summer) watercolumn
hydrographic time-series collected over the shelf and
slope in 2007. The Ωarag predicted by the regression model
was less than 1, the thermodynamic calcification/dissolution
threshold, over shelf/slope bottom waters throughout the
entire 2007 upwelling season (May–November), with the
Ωarag = 1 horizon shoaling to 30 m by late summer. The
persistence of water with Ωarag < 1 on the continental shelf
has not been previously noted and could have notable
ecological consequences for benthic and pelagic calcifying
organisms such as mussels, oysters, abalone, echinoderms,
and pteropods.
Genre Article
Topic aragonite saturation state
Identifier Juranek , L. W., R. A. Feely, W. T. Peterson, S. R. Alin, B. Hales, K. Lee, C. L. Sabine, and J. Peterson (2009), A novel method for determination of aragonite saturation state on the continental shelf of central Oregon using multi‐parameter relationships with hydrographic data, Geophys. Res. Lett., 36, L24601.

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