Storm-induced upwelling of high pCO2 waters onto the continental shelf of the western Arctic Ocean and implications for carbonate mineral saturation states
Text S1: Description of several different methods used to collect that data presented in the paper, including how samples were collected, the analytical procedures use to analyze TA, pH and the partial pressure of carbon dioxide as well as the constants use to calculate carbonate parameters. (30Kb)
Text S1: Description of several different methods used to collect that data presented in the paper, including how samples were collected, the analytical procedures use to analyze TA, pH and the partial pressure of carbon dioxide as well as the constants use to calculate carbonate parameters. (4.574Kb)
Mathis, Jeremy T.
Pickart, Robert S.
Byrne, Robert H.
McNeil, Craig L.
Moore, G. W. K.
Juranek, Laurie W.
Easley, Regina A.
Elliot, Matthew M.
Cross, Jessica N.
Reisdorph, Stacey C.
Bahr, Frank B.
Morison, James H.
Feely, Richard A.
MetadataShow full item record
The carbon system of the western Arctic Ocean is undergoing a rapid transition as sea ice extent and thickness decline. These processes are dynamically forcing the region, with unknown consequences for CO2 fluxes and carbonate mineral saturation states, particularly in the coastal regions where sensitive ecosystems are already under threat from multiple stressors. In October 2011, persistent wind-driven upwelling occurred in open water along the continental shelf of the Beaufort Sea in the western Arctic Ocean. During this time, cold (<−1.2°C), salty (>32.4) halocline water—supersaturated with respect to atmospheric CO2 (pCO2 > 550 μatm) and undersaturated in aragonite (Ωaragonite < 1.0) was transported onto the Beaufort shelf. A single 10-day event led to the outgassing of 0.18–0.54 Tg-C and caused aragonite undersaturations throughout the water column over the shelf. If we assume a conservative estimate of four such upwelling events each year, then the annual flux to the atmosphere would be 0.72–2.16 Tg-C, which is approximately the total annual sink of CO2 in the Beaufort Sea from primary production. Although a natural process, these upwelling events have likely been exacerbated in recent years by declining sea ice cover and changing atmospheric conditions in the region, and could have significant impacts on regional carbon budgets. As sea ice retreat continues and storms increase in frequency and intensity, further outgassing events and the expansion of waters that are undersaturated in carbonate minerals over the shelf are probable.
Author Posting. © American Geophysical Union, 2012. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 39 (2012): L07606, doi:10.1029/2012GL051574.
Suggested CitationArticle: Mathis, Jeremy T., Pickart, Robert S., Byrne, Robert H., McNeil, Craig L., Moore, G. W. K., Juranek, Laurie W., Liu, Xuewu, Ma, Jian, Easley, Regina A., Elliot, Matthew M., Cross, Jessica N., Reisdorph, Stacey C., Bahr, Frank B., Morison, James H., Lichendorf, Trina, Feely, Richard A., "Storm-induced upwelling of high pCO2 waters onto the continental shelf of the western Arctic Ocean and implications for carbonate mineral saturation states", Geophysical Research Letters 39 (2012): L07606, DOI:10.1029/2012GL051574, https://hdl.handle.net/1912/5187
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