2014
DOI: 10.5194/bgd-11-12255-2014
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Remote sensing algorithm for sea surface CO<sub>2</sub> in the Baltic Sea

Abstract: Abstract. Studies of coastal seas in Europe have brought forth the high variability in the CO2 system. This high variability, generated by the complex mechanisms driving the CO2 fluxes makes their accurate estimation an arduous task. This is more pronounced in the Baltic Sea, where the mechanisms driving the fluxes have not been as highly detailed as in the open oceans. In adition, the joint availability of in-situ measurements of CO2 and of sea-surface satellite data is limited in the area. In this paper, a c… Show more

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Cited by 7 publications
(16 citation statements)
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“…The outputs of this research have a horizontal resolution of 4 km and cover the 1998–2011 period. We continue the work of Parard et al [] by estimating p CO 2 variability in time and space over the Baltic Sea.…”
Section: Introductionmentioning
confidence: 82%
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“…The outputs of this research have a horizontal resolution of 4 km and cover the 1998–2011 period. We continue the work of Parard et al [] by estimating p CO 2 variability in time and space over the Baltic Sea.…”
Section: Introductionmentioning
confidence: 82%
“…To reconstruct the sea surface p CO 2 concentrations, we employed the SOMLO methodology [ Sasse et al , ] in a similar way to that applied by Parard et al []. The SOMLO methodology combines two statistical approaches: self‐organizing maps (SOMs) [ Kohonen , ] and linear regression .…”
Section: Methodsmentioning
confidence: 99%
See 1 more Smart Citation
“…1994 to 2008), the CB acts as a source of 1.64 mol m −2 yr −1 for the atmosphere. As we explain in Parard et al (2014), the pCO 2 data do not reproduce the spring-summer bloom in the eastern Gotland Sea described in Schneider et al (2015). The data used for the computation contain the voluntary observing ships (VOSs) ship line, but we calculated a monthly average.…”
Section: Discussionmentioning
confidence: 99%
“…Potential benefits of these methods include filling data gaps caused by cloud cover, inferring vertical distributions of biogeochemical variables observed at sea surface, emulate models of the upper ocean dynamics at high spatial resolution and developing relationships between environmental variables [9][10][11][12]. Further applications can be found in carbon dynamics [13][14][15], coastal turbidity [16,17], phytoplankton blooms [18][19][20][21], harmful algal blooms [22,23], and primary production [24].…”
Section: Introductionmentioning
confidence: 99%