CORE
🇺🇦
make metadata, not war
Services
Services overview
Explore all CORE services
Access to raw data
API
Dataset
FastSync
Content discovery
Recommender
Discovery
OAI identifiers
OAI Resolver
Managing content
Dashboard
Bespoke contracts
Consultancy services
Support us
Support us
Membership
Sponsorship
Community governance
Advisory Board
Board of supporters
Research network
About
About us
Our mission
Team
Blog
FAQs
Contact us
unknown
Dissolved methane distributions and air-sea flux in the plume of a massive seep field, Coal Oil Point, California
Authors
Bassin
Beckenbach
+31 more
Clark
Clark
Cline
Cynar
David L. Valentine
Emery
Fischer
Frew
Harms
Ho
Hornafius
Hovland
Jordan F. Clark
Justin Reed
Kinnaman
Kraus
Kraus
Leifer
Libe Washburn
McGillis
Nightingale
Nishimoto
Quigley
Ramaswamy
Reeburgh
Rehder
Richard Camilli
Susan Mau
Valentine
Wanninkhof
Wiesenburg
Publication date
24 November 2007
Publisher
'American Geophysical Union (AGU)'
Doi
Cite
Abstract
Author Posting. © American Geophysical Union, 2007. 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 34 (2007): L22603, doi:10.1029/2007GL031344.Large quantities of natural gas are emitted from the seafloor into the stratified coastal ocean near Coal Oil Point, Santa Barbara Channel, California. Methane was quantified in the down current surface water at 79 stations in a 280 km2 study area. The methane plume spread over an area of ~70 km2 and emitted on the order of 5 × 104 mol d−1 to the atmosphere. A monthly time series at 14 stations showed variable methane concentrations which were correlated with changing sub-mesoscale surface currents. Air-sea fluxes estimated from the time series indicate that the air-sea flux derived for the 280 km2 area is representative of the daily mean flux from this area. Only 1% of the dissolved methane originating from Coal Oil Point enters the atmosphere within the study area. Most of it appears to be transported below the surface and oxidized by microbial activity.The research was supported by the University of California Energy Institute and the National Science Foundation (OCE 0447395)
Similar works
Full text
Open in the Core reader
Download PDF
Available Versions
Sustaining member
eScholarship - University of California
See this paper in CORE
Go to the repository landing page
Download from data provider
oai:escholarship.org:ark:/1303...
Last time updated on 25/12/2021
Crossref
See this paper in CORE
Go to the repository landing page
Download from data provider
Last time updated on 05/06/2019
Woods Hole Open Access Server
See this paper in CORE
Go to the repository landing page
Download from data provider
oai:darchive.mblwhoilibrary.or...
Last time updated on 08/06/2012