A5059461339- Marine and coastal ecosystems
- Oceanographic and Atmospheric Processes
- Marine Biology and Ecology Research
- Ocean Acidification Effects and Responses
- Methane Hydrates and Related Phenomena
- Microbial Community Ecology and Physiology
- Arctic and Antarctic ice dynamics
- Coastal and Marine Management
- Geology and Paleoclimatology Research
- Coastal wetland ecosystem dynamics
- Marine and coastal plant biology
- Marine Bivalve and Aquaculture Studies
- Geological Studies and Exploration
- Marine and fisheries research
- Isotope Analysis in Ecology
- Hydrocarbon exploration and reservoir analysis
- Environmental Changes in China
- Groundwater and Isotope Geochemistry
- Global Energy and Sustainability Research
- Aquatic Ecosystems and Phytoplankton Dynamics
- Peatlands and Wetlands Ecology
- Land Use and Ecosystem Services
- Marine Ecology and Invasive Species
- Environmental Quality and Pollution
- Marine and environmental studies
First Institute of Oceanography
2015-2025
Ministry of Natural Resources
2011-2025
Qingdao National Laboratory for Marine Science and Technology
2018-2025
Laoshan Laboratory
2024
Ocean University of China
2015-2018
Abstract As China's only continental sea, the Bohai Sea is a relatively closed environment and vulnerable to natural changes human activities. In this paper, long‐term variations in nutrients potential influencing factors were analyzed based on historical summer winter data from 1978 2016. The results showed that concentrations of dissolved inorganic nitrogen (DIN) continuously increased 1990 rapidly after 2002, phosphate (PO 4 ‐P) concentration exhibited decreasing trend, silicate (SiO 3...
To better understand the relationship between subsurface seasonal deoxygenation and acidification in Yellow Sea northern East China (ECS), we examined carbonate system parameters dissolved oxygen (DO) of seven field surveys conducted 2017–2018, spanning all four seasons. Low pHT values 7.71‒7.80 critically low aragonite saturation state (Ωarag) 1.07‒1.40 along with undersaturated DO mostly higher than 150 μmol O2 kg–1 occurred Cold Water Mass area summer autumn, while hypoxic 49‒63 extremely...
Abstract The Changjiang (Yangtze River) Estuary (CE) and adjacent inner East China Sea (ECS) shelf are among the most well‐known hypoxic aquatic environments. However, coupled effects of coastal upwelling river plume on dynamics in this region rarely examined. Based observations off CE Zhejiang coast summer 2018, dynamic mechanisms were revealed by highlighting combined role regulating hypoxia. bottom water formed steep slope ECS expands upward seaward. Coastal combine to regulate primary...
Abstract Oceanic emission is a primary source of brominated very short‐lived substances (BrVSLs) to the atmosphere, which have important effects on stratospheric ozone chemistry. Marine biogeochemical processes regulating BrVSLs are often sensitive ocean acidification. Yet, response production acidification remains poorly understood. Herein, two main BrVSLs, dibromomethane (CH 2 Br ) and tribromomethane (CHBr 3 ), were studied by ship‐based incubation experiments at three stations in South...
Abstract As two most important metrics for ocean acidification (OA), both pH and calcium carbonate mineral saturation states (Ω) respond sensitively to anthropogenic carbon dioxide (CO 2 ). However, contrary intuition, they are often out of phase in the global surface ocean, spatially seasonally. For example, during warm seasons, Ω is lowest at high‐latitude seas where there very high values, challenging our understanding that a bellwether OA. To explain this phenomenon, we separate spatial...
Abstract Deoxygenation is a global problem in open oceans and coastal regions has led to the expansion of oxygen minimum zones hypoxia. Here, using time series observations northern Yellow Sea, we illustrate seasonality deoxygenation associated mechanisms this semienclosed shelf ecosystem explore linkage dissolved (DO) declines with seawater warming anthropogenic eutrophication. Our results show that DO concentration displayed decreasing trend winter, rates ~0.76 ~0.78 μmol kg −1 yr surface...