Article ID Journal Published Year Pages File Type
7699748 Marine Chemistry 2012 9 Pages PDF
Abstract
► Halocarbon distributions in the Amundsen and Ross Seas were mainly governed by sea ice. ► High salinity shelf water in the Ross Sea retained a biogenic halocarbon signal. ► Sea ice was shown to be a major contributor to atmospheric halogens. ► Air-sea halocarbon saturation anomalies varied considerably on short time scales.
Related Topics
Physical Sciences and Engineering Chemistry Chemistry (General)
Authors
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