Abstract
The seawater fugacity of carbon dioxide (CO2; fCO2SW) was investigated over four seasons in the southeastern Yellow Sea (YS). The seasonal variation in sea surface temperature (SST)-normalized fCO2SW in the study area was largely explained by sea surface concentrations of dissolved inorganic carbon modulated by the water column stability in association with biological carbon fixation and remineralization. Overall, our study area acted as a sink for atmospheric CO2, absorbing a regional average of ~2.8 mmol C m−2 day−1. This result contrasts sharply with the large CO2 effluxes reported in other parts of the YS, implying considerable spatiotemporal variations in fCO2SW in this region. Since the YS is significantly influenced by human activity, our data will serve as a baseline to record the human impact on ocean carbon cycles in the future.
Original language | English |
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Article number | 110550 |
Journal | Marine Pollution Bulletin |
Volume | 149 |
DOIs | |
Publication status | Published - 2019 Dec |
Bibliographical note
Funding Information:This work was supported by a project ( PE99712 ) supported by the Korea Institute of Ocean Science and Technology , and by projects funded by Ministry of Oceans and Fisheries , Korea, titled “Construction of ocean research stations and their application studies” and “Study on air-sea interaction and process of rapidly intensifying typhoon in the northwestern Pacific”.
Publisher Copyright:
© 2019 Elsevier Ltd
Keywords
- Air-sea CO flux
- Carbon cycle
- East Asian marginal sea
- Korean coastal water
- Yellow Sea
ASJC Scopus subject areas
- Oceanography
- Aquatic Science
- Pollution