Elevated particulate organic carbon export flux induced by internal waves in the oligotrophic northern South China Sea

Dewang Li; Wen-Chen Chou; Yung-Yen Shih; Guan-Yu Chen; Yi Chang; Chun Hoe Chow; Tsang-Yuh Lin; Chin-Chang Hung

doi:10.1038/s41598-018-20184-9

Elevated particulate organic carbon export flux induced by internal waves in the oligotrophic northern South China Sea

Sci Rep. 2018 Feb 1;8(1):2042. doi: 10.1038/s41598-018-20184-9.

Authors

Dewang Li^{1

2}, Wen-Chen Chou³, Yung-Yen Shih^{1

4}, Guan-Yu Chen¹, Yi Chang⁵, Chun Hoe Chow⁶, Tsang-Yuh Lin^{1

5}, Chin-Chang Hung⁷

Affiliations

¹ Department of Oceanography, National Sun Yat-sen University, Kaohsiung, 804, Taiwan.
² Key Laboratory of Marine Ecosystem and Biogeochemistry, Second Institute of Oceanography, State Oceanic Administration, Hangzhou, 310012, PR China.
³ Institute of Marine Environment and Ecology, National Taiwan Ocean University, Keelung, 202, Taiwan.
⁴ Department of Applied Science, R.O.C Naval Academy, Kaohsiung, 813, Taiwan.
⁵ Institute of Ocean Technology and Marine Affair, National Cheng Kung University, Tainan, 701, Taiwan.
⁶ Department of Marine Environmental Informatics, National Taiwan Ocean University, Keelung, 202, Taiwan.
⁷ Department of Oceanography, National Sun Yat-sen University, Kaohsiung, 804, Taiwan. cchung@mail.nsysu.edu.tw.

Abstract

To understand the biogeochemical response to internal waves in the deep basin of the northern South China Sea (NSCS), particulate organic carbon (POC) export fluxes were quantified for the first time during the passage of large internal waves using drifting sediment traps attached with hydrographic sensors. Results revealed large variations in temperature, nitrate and chlorophyll a (Chl a) concentrations during and after internal waves, suggesting that cold nutrient-replete waters may be brought to the euphotic zone in the dissipation zone during and after the passage of internal wave packets, resulted in phytoplankton flourished. Most importantly, POC export fluxes (110.9 ± 10.7 mg C m^-2 d^-1) were significantly enhanced after internal waves compared to non-internal wave area (32.6-73.0 mg C m^-2 d^-1) in the NSCS. Such elevated POC fluxes may be induced by downward flourished biogenic particles, particle aggregation or converged particles from mixed layer triggered by internal waves.

Publication types

Research Support, Non-U.S. Gov't