Assessing the potential for dimethylsulfide enrichment at the sea surface and its influence on air–sea flux
The flux of dimethylsulfide (DMS) to the atmosphere is generally inferred using water sampled at or below 2 m depth, thereby excluding any concentration anomalies at the air–sea interface. Two independent techniques were used to assess the potential for near-surface DMS enrichment to influence DMS e...
Main Authors: | C. F. Walker, M. J. Harvey, M. J. Smith, T. G. Bell, E. S. Saltzman, A. S. Marriner, J. A. McGregor, C. S. Law |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2016-09-01
|
Series: | Ocean Science |
Online Access: | http://www.ocean-sci.net/12/1033/2016/os-12-1033-2016.pdf |
Similar Items
-
Determining the sea-air flux of dimethylsulfide by eddy correlation using mass spectrometry
by: B. W. Blomquist, et al.
Published: (2010-01-01) -
Gradient flux measurements of sea–air DMS transfer during the Surface Ocean Aerosol Production (SOAP) experiment
by: M. J. Smith, et al.
Published: (2018-04-01) -
Dimethylsulfide gas transfer coefficients from algal blooms in the Southern Ocean
by: T. G. Bell, et al.
Published: (2015-02-01) -
Constraining the concentration of the hydroxyl radical in a stratocumulus-topped marine boundary layer from sea-to-air eddy covariance flux measurements of dimethylsulfide
by: B. J. Huebert, et al.
Published: (2009-12-01) -
Sea-surface dimethylsulfide (DMS) concentration from satellite data at global and regional scales
by: M. Galí, et al.
Published: (2018-06-01)