Please use this identifier to cite or link to this item: http://hdl.handle.net/10553/49808
Title: Carbon dioxide fluxes in the Benguela upwelling system during winter and spring: A comparison between 2005 and 2006
Authors: Santana-Casiano, J. Magdalena 
González-Dávila, Melchor 
Ucha, Ivan R.
UNESCO Clasification: 251002 Oceanografía química
Keywords: CO2 fluxes
Upwelling
Benguela
South Atlantic
Carbon dioxide
Issue Date: 2009
Publisher: 0967-0645
Project: Marine Carbon Sources And Sinks Assessment (Carboocean) 
Journal: Deep-Sea Research Part II: Topical Studies in Oceanography 
Abstract: The distributions of fCO2 in surface seawater and in the atmosphere were studied in the Benguela Province (14–33°S) during the austral winter and spring 2005 and 2006. High fCO2sw variability was observed due to the effect of upwelled and derived meso-scale structures such as filament water. The complexity of the system, dominated by the upwelling dynamics, produces both a general decrease in fCO2sw with temperature (16 μatm/°C) and negative temperature–fCO2sw relationship due to the presence of upwelling, filaments, and frontal zones. Multiple linear regressions are unable to capture the resulting variability in fCO2 in the area. CO2 fluxes over the cruise track varied from Northern Namibia to the Southern Benguela regions. The northern system (14–20°S) is oversaturated in CO2 relative to the atmosphere, and presents an average flux of 0.56 mol m−2 yr−1. The southern part (20°S–33°S) of the Benguela system is undersaturated in CO2, and the average flux is −1.62 mol m−2 yr−1. This study describes an intensive upwelling area, acting as a sink for CO2 in winter and spring.
URI: http://hdl.handle.net/10553/49808
ISSN: 0967-0645
DOI: 10.1016/j.dsr2.2008.12.010
Source: Deep-Sea Research Part II: Topical Studies in Oceanography [ISSN 0967-0645], v. 56, p. 533-541
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