Publications
As part of the Copernicus Marine Service, the annual Copernicus Ocean State Report (OSR) launched in 2015 is the key tool of its ocean reporting framework. The OSR reports on the state, variability, and ongoing changes in the marine environment of the global ocean and the European regional seas over the past decades up to close to real time. Using observation-based (remote sensing, in situ) and ocean reanalysis data, the OSR provides a comprehensive 4-dimensional (latitude, longitude, depth, and time) analysis of the Blue, Green, and White Ocean. The OSR is intended to act as a reference, providing a unique ocean monitoring dashboard for the scientific community and for policy makers and others with decision making responsibilities.
von Schuckmann, K., Moreira, L., Grégoire, M., Marcos, M., Staneva, J., Brasseur, P., Garric, G., Lionello, P., Karstensen, J., & Neukermans, G. (eds.): 8th edition of the Copernicus Ocean State Report (OSR8). Copernicus Publications, State Planet, 4-osr8, 2024, doi:10.5194/sp-4-osr8, open access
It includes following contribution of our colleagues from the Hereon Institute of Coastal Systems – Analysis and Modeling:
Chen, W., & Staneva, J. (2024): Characteristics and trends of marine heatwaves in the northwest European Shelf and the impacts on density stratification. doi:10.5194/sp-4-osr8-7-2024
Abstract:
Marine heatwaves (MHWs) are characterized by anomalous and prolonged increases in sea surface temperatures driven by atmospheric and oceanic factors. The intensification of MHWs is an evident consequence of ongoing global climate change. The question of whether the northwest European Shelf (NWES) is experiencing increased stratification in recent decades is of significant interest with respect to understanding the impacts of these extreme events. In this study, we leverage ocean physics reanalysis data obtained from the Copernicus Marine Environment Monitoring Service (CMEMS) covering the temporal span from 1993 to 2023 to conduct a rigorous examination of the NWES domain. The focus centers on the assessment of potential energy anomaly (PEA) and its role in shaping stratification dynamics.
Our findings reveal an increase in both the frequency and duration of MHWs in the NWES area, especially in coastal areas, where the duration of MHWs is increasing the fastest, generally by more than 2 d yr−1 over the study period. However, despite the intensified MHWs, thermal stratification in the NWES is weakening, particularly in the middle and northern North Sea. This suggests that the warming effect due to MHWs is insufficient to counteract the overall decline in thermal stratification caused by global warming. Additionally, our study highlights the significance of seawater salinity in driving the trend of density stratification. Specifically, the discharge from the Baltic Sea plays a crucial role in influencing the stratification patterns in the North Sea region.
