Storm-induced Upwelling of High p CO 2 Waters Onto the Continental Shelf of the Western Arctic Ocean and Implications for Carbonate Mineral Saturation States

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 sens...

Full description

Bibliographic Details
Published in:Geophysical Research Letters
Main Authors: Mathis, Jeremy T., Pickart, Robert S., Byrne, Robert H., McNeil, Craig L., Moore, G. W., Juranek, Laurie W., Liu, Xuewu, Ma, Jian, Easley, Regina A., Elliot, Matthew M., Cross, Jessica N., Reisdorph, Stacey C., Bahr, Frank, Morison, Jamie, Lichendorf, Trina, Feely, Richard A.
Format: Article in Journal/Newspaper
Language:unknown
Published: Digital Commons @ University of South Florida 2012
Subjects:
Online Access:https://digitalcommons.usf.edu/msc_facpub/1589
https://doi.org/10.1029/2012GL051574
https://digitalcommons.usf.edu/context/msc_facpub/article/2632/viewcontent/2012GL051574.pdf