AI Article Synopsis
- Studying the impacts of climate change on oceanic carbon cycling is crucial for improving carbon sequestration efforts, particularly in the Ulleung Basin.
- From 2011 to 2017, research showed that particulate organic carbon (POC) flux increased significantly during the El Niño years, with rises of 37%, 56%, and 43%.
- Analysis of water current data indicated that current variability plays a key role in enhancing particle transport, influencing the increased flux of sinking particles during the El Niño phase.
Article Abstract
Understanding the impacts of climate change on oceanic carbon cycling is important from a carbon sequestration perspective. A sediment trap study focused on the biological carbon pump system in the Ulleung Basin (UB) in the southwestern part of the East Sea (Japan Sea) was conducted from 2011 to 2017. Particulate organic carbon (POC) flux significantly increased by 37, 56, and 43% from 2014 to 2016 during the El Niño phase. We examined data related to water current variability, such as sea surface height, current velocity, and eddy frequency to understand their roles in particle transport. In addition, a Martin curve was employed to analyze the rate of vertical attenuation of POC flux in the UB. Current variability could be the most important factor influencing the increase in sinking-particle flux during the El Niño phase.
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| http://www.ncbi.nlm.nih.gov/pmc/articles/PMC11535021 | PMC |
| http://dx.doi.org/10.1038/s41598-024-74818-2 | DOI Listing |
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