dc.contributor.author | Yasunaka, Sayaka | |
dc.contributor.author | Siswanto, Eko | |
dc.contributor.author | Olsen, Are | |
dc.contributor.author | Hoppema, Mario | |
dc.contributor.author | Watanabe, Eiji | |
dc.contributor.author | Fransson, Agneta Ingrid | |
dc.contributor.author | Chierici, Melissa | |
dc.contributor.author | Murata, Akihiko | |
dc.contributor.author | Lauvset, Siv Kari | |
dc.contributor.author | Wanninkhof, Rik | |
dc.contributor.author | Takahashi, Taro | |
dc.contributor.author | Kosugi, Naohiro | |
dc.contributor.author | Omar, Abdirahman | |
dc.contributor.author | van Heuven, Steven | |
dc.contributor.author | Mathis, Jeremy T. | |
dc.date.accessioned | 2019-02-01T16:12:27Z | |
dc.date.available | 2019-02-01T16:12:27Z | |
dc.date.issued | 2018-03-22 | |
dc.Published | Yasunaka S, Siswanto, Olsen A, Hoppema M, Watanabe E, Fransson AI, Chierici M, Murata A, Lauvset SK, Wanninkhof R, Takahashi T, Kosugi N, Omar A, van Heuven S, Mathis JT. Arctic Ocean CO2 uptake: An improved multiyear estimate of the air-sea CO2 flux incorporating chlorophyll a concentrations. Biogeosciences. 2018;15(6):1643-1661 | eng |
dc.identifier.issn | 1726-4170 | en_US |
dc.identifier.issn | 1726-4189 | en_US |
dc.identifier.uri | https://hdl.handle.net/1956/19045 | |
dc.description.abstract | We estimated monthly air–sea CO2 fluxes in the Arctic Ocean and its adjacent seas north of 60∘ N from 1997 to 2014. This was done by mapping partial pressure of CO2 in the surface water (pCO2w) using a self-organizing map (SOM) technique incorporating chlorophyll a concentration (Chl a), sea surface temperature, sea surface salinity, sea ice concentration, atmospheric CO2 mixing ratio, and geographical position. We applied new algorithms for extracting Chl a from satellite remote sensing reflectance with close examination of uncertainty of the obtained Chl a values. The overall relationship between pCO2w and Chl a was negative, whereas the relationship varied among seasons and regions. The addition of Chl a as a parameter in the SOM process enabled us to improve the estimate of pCO2w, particularly via better representation of its decline in spring, which resulted from biologically mediated pCO2w reduction. As a result of the inclusion of Chl a, the uncertainty in the CO2 flux estimate was reduced, with a net annual Arctic Ocean CO2 uptake of 180 ± 130 Tg C yr−1. Seasonal to interannual variation in the CO2 influx was also calculated. | en_US |
dc.language.iso | eng | eng |
dc.publisher | EGU | en_US |
dc.rights | Attribution CC BY | eng |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/ | eng |
dc.title | Arctic Ocean CO2 uptake: An improved multiyear estimate of the air-sea CO2 flux incorporating chlorophyll a concentrations | en_US |
dc.type | Peer reviewed | |
dc.type | Journal article | |
dc.date.updated | 2018-08-24T08:33:30Z | |
dc.description.version | publishedVersion | en_US |
dc.rights.holder | Copyright The Author(s) 2018 | en_US |
dc.identifier.doi | https://doi.org/10.5194/bg-15-1643-2018 | |
dc.identifier.cristin | 1592041 | |
dc.source.journal | Biogeosciences | |