Increase in acidifying water in the western Arctic Ocean

Di Qi, Liqi Chen (), Baoshan Chen, Zhongyong Gao, Wenli Zhong, Richard A. Feely, Leif G. Anderson, Heng Sun, Jianfang Chen, Min Chen, Liyang Zhan, Yuanhui Zhang and Wei-Jun Cai ()
Additional contact information
Di Qi: Key Laboratory of Global Change and Marine-Atmospheric Chemistry of State Oceanic Administration (SOA), Third Institute of Oceanography, SOA
Liqi Chen: Key Laboratory of Global Change and Marine-Atmospheric Chemistry of State Oceanic Administration (SOA), Third Institute of Oceanography, SOA
Baoshan Chen: School of Marine Science and Policy, University of Delaware, Newark
Zhongyong Gao: Key Laboratory of Global Change and Marine-Atmospheric Chemistry of State Oceanic Administration (SOA), Third Institute of Oceanography, SOA
Wenli Zhong: Key Lab of Physical Oceanography, Ocean University of China
Richard A. Feely: Pacific Marine Environmental Laboratory/NOAA Seattle
Leif G. Anderson: University of Gothenburg
Heng Sun: Key Laboratory of Global Change and Marine-Atmospheric Chemistry of State Oceanic Administration (SOA), Third Institute of Oceanography, SOA
Jianfang Chen: Second Institute of Oceanography, SOA
Min Chen: College of Ocean and Earth Sciences, Xiamen University
Liyang Zhan: Key Laboratory of Global Change and Marine-Atmospheric Chemistry of State Oceanic Administration (SOA), Third Institute of Oceanography, SOA
Yuanhui Zhang: Key Laboratory of Global Change and Marine-Atmospheric Chemistry of State Oceanic Administration (SOA), Third Institute of Oceanography, SOA
Wei-Jun Cai: School of Marine Science and Policy, University of Delaware, Newark

Nature Climate Change, 2017, vol. 7, issue 3, 195-199

Abstract: Ocean acidification has expanded in the western Arctic Ocean. Observations from the 1990s to 2010 show that aragonite saturation levels have decreased, with low saturation water deepening to 250 m and increasing in area more rapidly than seen in other oceans.

Date: 2017
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DOI: 10.1038/nclimate3228

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