Journal
CONTINENTAL SHELF RESEARCH
Volume 230, Issue -, Pages -Publisher
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.csr.2021.104570
Keywords
Net community production; O-2/Ar; Biological pump; East China Sea; Yellow sea; Continental shelf
Categories
Funding
- Ministry of Oceans and Fisheries, Korea [20160040]
- Basic Science Research Program through the National Research Foundation of Korea (NRF) - Ministry of Education [NRF-2016R1D1A1B03931205]
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The East China Sea and Yellow Sea have high biological productivities, with the Yellow Sea Cold Water area having significantly higher net community production compared to the Eastern Kuroshio Branch Water and Southern Coast Water areas. Vertical mixing and horizontal advection play significant roles in influencing the estimates of biological pump activity in these regions.
The East China Sea (ECS) and Yellow Sea (YS) are East Asian marginal seas and mainly cover shallow continental shelves with depths of <200 m. These seas have high biological productivities with large spatial and temporal variabilities. Nevertheless, there are a limited number of studies on the biological pump in the ECS and YS. We observed net community production (NCP) for the first time in this region based on high resolution O-2/Ar measurements, which act as a measure of biological pump activity. Observations were conducted underway using an equilibrator inlet mass spectrometer in April 2018. Three distinct water masses were identified in the study area: a cold and less saline water mass in the southern YS (Yellow Sea Cold Water; YSCW); a warm and saline water mass along a branch of the Kuroshio current (Eastern Kuroshio Branch Water; EKBW); and a water mass near the southern coast of the Korean Peninsula (Southern Coast Water; SCW). The average NCP of 49 +/- 19 mmol O-2 m(-2) d(-1) in the YSCW was almost twice as high as that of 26 +/- 13 and 23 +/- 12 mmol O-2 m(-2) d(-1) in the EKBW and SCW, respectively. Vertical mixing between the surface mixed layer and subsurface layers was assessed using vertical measurements of microscale turbulence and discrete O-2/Ar values and appeared to bias the NCP estimates by similar to 2%. In contrast, horizontal advection, which was assessed using the horizontal O-2/Ar gradient and current speeds, could be a major source of uncertainty up to 38% in the estimates. The spatial variability of the NCP, shown in the standard deviations (39-52% of the three averages), may largely be ascribed to the horizontal advection in the region, which is affected by strong surface currents.
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