An inland sea high nitrate‐low chlorophyll (HNLC) region with naturally high pCO 2

• Published in: Limnology and Oceanography
• Main Authors: Murray, James W., Roberts, Emily, Howard, Evan, O'Donnell, Michael, Bantam, Cory, Carrington, Emily, Foy, Mike, Paul, Barbara, Fay, Amanda
• Other Authors: The Educational Foundation of America (EFA, National Science Foundation Field Station Marine Lab Program
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2015
• Subjects: Pacific; Ocean acidification
• Online Access: http://dx.doi.org/10.1002/lno.10062; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Flno.10062; https://onlinelibrary.wiley.com/doi/pdf/10.1002/lno.10062; https://onlinelibrary.wiley.com/doi/full-xml/10.1002/lno.10062; https://aslopubs.onlinelibrary.wiley.com/doi/pdf/10.1002/lno.10062

Abstract We present a time series of data for temperature, salinity, nitrate, and carbonate chemistry from September 2011 to July 2013 at the University of Washington's Friday Harbor Laboratories. Samples were collected at the Friday Harbor dock and pump house. Seawater conditions at Friday Harbor were high nitrate‐low chlorophyll, with average nitrate and pCO 2 concentrations of ∼ 25 ± 5 μ mol L −1 and ∼ 700 ± 103 μ atm (pH 7.80 ± 0.06). Transient decreases in surface water nitrate and pCO 2 corresponded with the timing of a spring bloom (April through June). The high nitrate and pCO 2 originate from the high values for these parameters in the source waters to the Salish Sea from the California Undercurrent (CU). These properties are due to natural aerobic respiration in the region where the CU originates, which is the oxygen minimum zone in the eastern tropical North Pacific. Alkalinity varies little so the increase in pCO 2 is due to inputs of dissolved inorganic carbon (DIC). This increase in DIC can come from both natural aerobic respiration within the ocean and input of anthropogenic CO 2 from the atmosphere when the water was last at the sea surface. We calculated that the anthropogenic “ocean acidification” contribution to DIC in the source waters of the CU was 36 μ mol L −1 . This contribution ranged from 13% to 22% of the total increase in DIC, depending on which stoichiometry was used for C/O 2 ratio (Redfield vs. Hedges). The remaining increase in DIC was due to natural aerobic respiration.