Progress in Oceanography最新文献

{"title":"Presence of two eddies in close proximity drives large spatial and temporal heterogeneity in the euphotic zone","authors":"Simon Ramondenc ,&nbsp;Richard S. Lampitt ,&nbsp;Maria Fredrika Norrbin ,&nbsp;Anna Belcher ,&nbsp;Wilken-Jon von Appen ,&nbsp;Morten H. Iversen","doi":"10.1016/j.pocean.2025.103476","DOIUrl":"10.1016/j.pocean.2025.103476","url":null,"abstract":"<div><div>Oceanic mesoscale structures, such as eddies, play a fundamental role in ocean circulation, ocean biogeochemical cycles and plankton ecology. They cause lateral and vertical advection, as well as interact with vertical mixing, which is predicted to promote episodic fluxes of macronutrients to the surface ocean. However, the interactions between mesoscale eddies can generate submesoscale fronts and filaments occurring over short temporal and spatial scales and thus their impact on ocean biogeochemistry has been difficult to characterize. During an expedition to the Porcupine Abyssal Plain (PAP) site in the Northeast Atlantic in June 2013, we studied the interface between a cyclonic and an anticyclonic eddy, measuring nutrient and chlorophyll-a concentrations, zooplankton abundance and community structure, and marine snow aggregate abundance and sinking velocities. We observed that eddy rotation and a storm event induced, respectively, lateral stirring and vertical mixing of the two distinct water masses, driving spatial and temporal biogeochemical heterogeneity at the PAP site. Furthermore, we observe that diel and vertical variations in aggregate type and abundance were closely linked to the vertical distribution and abundance of zooplankton, suggesting that zooplankton were the main gatekeepers of carbon flux. Our findings suggest that the interactions between mesoscale structures could significantly modify organic carbon export, as well as provide sustenance for higher trophic levels, processes that have implications for fisheries and global climate.</div></div>","PeriodicalId":20620,"journal":{"name":"Progress in Oceanography","volume":"235 ","pages":"Article 103476"},"PeriodicalIF":3.8,"publicationDate":"2025-04-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143868956","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Significance of temperature and salinity in the dynamics of diatoms and dinoflagellates along the coastal Yellow Sea","authors":"Chenshi Weng ,&nbsp;Dongsheng Ding ,&nbsp;Qian Yang ,&nbsp;Lin Zhu ,&nbsp;Jun Sun ,&nbsp;Keming Qu ,&nbsp;Zhengguo Cui ,&nbsp;Yuqiu Wei","doi":"10.1016/j.pocean.2025.103478","DOIUrl":"10.1016/j.pocean.2025.103478","url":null,"abstract":"<div><div>Diatoms and dinoflagellates are two typical functional groups of phytoplankton, which account for a major part of global primary production and play an important role in ecosystem processes and biogeochemical cycles. It is well known that the dynamics of diatoms and dinoflagellates in the ocean are mainly driven by changes in hydrological conditions related to climate change and human activities. However, little is known about their ability to adapt to changing ocean environments, making it difficult to predict whether and how they will adapt. Analysis of field data from the coastal Yellow Sea (2021–2023) showed that temperature and salinity changes, driven by seasonal variations, notably affected the dynamics of diatoms and dinoflagellates. Moreover, the seasonal dynamics of these two groups exhibited distinct responses to temperature, salinity, and their interactions. Specifically, diatoms exhibited greater heat resistance than dinoflagellates, but were more sensitive to salinity changes, often dominating during the warmer, less saline summer and autumn seasons. In contrast, dinoflagellates, due to their nutritional strategies, showed greater tolerance to salinity changes and often co-dominated with diatoms under high salinity conditions. Overall, changes in temperature and salinity had a large impact on diatoms and dinoflagellates in coastal Yellow Sea, albeit with different relationships. Therefore, future research should focus on the long-term effects of combined temperature and salinity changes, as well as the potential influence of other environmental variables such as nutrient availability.</div></div>","PeriodicalId":20620,"journal":{"name":"Progress in Oceanography","volume":"234 ","pages":"Article 103478"},"PeriodicalIF":3.8,"publicationDate":"2025-04-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143854840","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"A stable-carbon-isotope-based constraint of bulk particulate organic carbon dynamics and budgets in the Yellow Sea: Combining field surveys and isotope fractionation modeling","authors":"Cong-cong Guo ,&nbsp;Shu Yang ,&nbsp;Qing-shan Luan ,&nbsp;Qian-qian Liu ,&nbsp;Zi-chen Liu ,&nbsp;Wei-dong Zhai","doi":"10.1016/j.pocean.2025.103477","DOIUrl":"10.1016/j.pocean.2025.103477","url":null,"abstract":"<div><div>The isotopic composition of POC (δ¹³C_POC) serves as a critical tracer for marine carbon dynamics. Its traditional applications usually assume a fixed δ¹³C value for marine phytoplankton (δ¹³C_phyto) of − 20 ± 1 ‰, overlooking spatiotemporal variabilities in phytoplankton carbon isotope fractionation (<em>ε</em>_P). This study quantifies <em>ε</em>_P-mediated δ¹³C_POC variations in the Yellow Sea – a temperate shelf sea characterized by seasonal stratification, intense diatom blooms, and terrestrial inputs – by coupling isotope fractionation models (passive CO₂aq diffusion vs. active HCO₃^– transport) with multi-season δ¹³C measurements of Dissolved Inorganic Carbon (DIC) and δ¹³C_POC. During algal bloom periods, δ¹³C_POC values were relatively heavier (−20 ± 1 ‰), driven by active HCO₃^– uptake under low CO₂aq concentrations ([CO₂aq]). Strong agreement between δ¹³C_POC and modeled δ¹³C_phyto values confirmed compositional similarity between POC and algal biomass, with <span><math><mrow><msub><mrow><mi>ε</mi></mrow><mrow><mi>P</mi></mrow></msub></mrow></math></span> exhibiting significant covariation with [CO₂aq]. In non-bloom periods, lighter δ¹³C_POC values (from − 26 to − 24 ‰) dominated surface layers, with even more depleted signatures (&lt;−26 ‰) occurred in the Deep Chlorophyll Maximum (DCM) and middle layers. Although detritus inputs caused deviations of δ¹³C_POC from modeled δ¹³C_phyto values, temperature-dependent correlations still revealed <span><math><mrow><msub><mrow><mi>ε</mi></mrow><mrow><mi>P</mi></mrow></msub></mrow></math></span>-related isotopic dynamics in POC. This research underscores the necessity of using environment-specific δ¹³C_phyto values to refine POC budget estimates, reducing flux uncertainties by 20–30 % and minimizing isotopic errors to &lt; 1 ‰ across different timescales. This work establishes a framework for incorporating δ¹³C_phyto plasticity into coastal carbon models, resolving long-standing paradoxes of isotopically light POC (&lt;−26 ‰) in marine-dominated systems and advancing high-resolution carbon flux estimates in marginal seas.</div></div>","PeriodicalId":20620,"journal":{"name":"Progress in Oceanography","volume":"236 ","pages":"Article 103477"},"PeriodicalIF":3.8,"publicationDate":"2025-04-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144071858","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Seasonal dissolved oxygen gas exchange in the California Current Upwelling System","authors":"A.S. Ren ,&nbsp;D.L. Rudnick ,&nbsp;D.P. Nicholson","doi":"10.1016/j.pocean.2025.103473","DOIUrl":"10.1016/j.pocean.2025.103473","url":null,"abstract":"<div><div>Eastern boundary current systems are known for seasonal upwelling that brings water from below the mixed layer to the surface. The process deoxygenates the water column by bringing lower-dissolved oxygen water closer to the surface and oxygenates the water column by driving primary productivity due to the injection of nutrients from deep waters. Here, an observational dataset of 5 years of dissolved oxygen, temperature, and salinity measured to 500 m and from the coast to around 400 km offshore is used to study the seasonal evolution of air-sea exchange of oxygen in an upwelling region. The data were collected as part of the California Underwater Glider Network (CUGN) which monitors transect line 66.7 off of Monterey Bay, CA, transect line 80.0 off of Point Conception, CA, and transect line 90.0 off of Dana Point, CA year-round. A narrow band of coastal oxygen undersaturation drives dissolved oxygen uptake by the ocean in spring and summer, while in winter dissolved oxygen uptake predominates due to more widespread but less intense oxygen undersaturation. Oxygen outgassing occurs offshore of the nearshore uptake band in spring and summer, driven by warming and primary productivity, such that the cumulative net oxygen gas exchange integrated seaward from shore reaches zero once around one hundred kilometers from the coast. Ventilation of the upper ocean is observed as a result of shoaling isopycnals in the upwelling season. The balance between outgassing and uptake is such that the central and southern California Current System is a region of net outgassing of oxygen for a region from the coast to 400 km, 365 km, and 530 km for lines 66.7, 80.0, and 90.0 respectively. Competing factors causing uptake and outgassing and the seaward extent of the domain determine whether an upwelling zone is a net source or sink of oxygen gas.</div></div><div><h3>Plain Language Summary</h3><div>The oceanography of coastal California is such that a seasonal vertical and offshore movement of water in the nearshore 50 km reduces the dissolved oxygen concentration of the water. The dissolved oxygen changes in the ocean were observed with autonomous underwater vehicles that allowed scientists to observe seasonal changes. Dissolved oxygen gas was found to enter the ocean in the coastal region during times of upwelling while it was released from the ocean further offshore. Some dissolved oxygen that entered the ocean surface layer found its way to deeper waters. The amount of dissolved oxygen gas released from the surface ocean compensated for the amount of oxygen uptake that occurred. The region from the coast to around 400 km from shore released oxygen gas to the atmosphere overall.</div></div>","PeriodicalId":20620,"journal":{"name":"Progress in Oceanography","volume":"236 ","pages":"Article 103473"},"PeriodicalIF":3.8,"publicationDate":"2025-04-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"144099777","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"The role of the Atlantic-Ionian stream in the long-term variability of the surface circulation in the Northern Ionian Sea: Results from a hindcast simulation","authors":"E. Napolitano ,&nbsp;A. Carillo ,&nbsp;M.V. Struglia ,&nbsp;R. Iacono ,&nbsp;M. Palma ,&nbsp;G.L. Eusebi Borzelli ,&nbsp;G. Sannino","doi":"10.1016/j.pocean.2025.103472","DOIUrl":"10.1016/j.pocean.2025.103472","url":null,"abstract":"<div><div>We examine the long-term variability of the near-surface circulation of the Ionian Sea. Our analysis primarily focuses on a high-resolution hindcast simulation of the Mediterranean dynamics from 1981 to 2010. This time period is significant as it includes a notable near-surface circulation reversal in the Northern Ionian Sea (NIS), which shifted from anticyclonic to cyclonic at the end of 1997. This transition has been previously documented by altimeter data and Copernicus reanalysis. Our hindcast simulation accurately captures this change. Here we examine the temporal and spatial scales of the near-surface circulation during the transition and investigate the factors contributing to the observed variability of the basin dynamics, including local wind-stress, deep-water density anomalies, and the lateral current associated with the Atlantic Ionian Stream (AIS). We find that while wind stress does play a role, the primary factor driving long-term variability in the NIS near-surface circulation is the AIS. During the late 1980s to mid-1990s, the AIS was weak and local cyclonic winds were also weak, allowing the AIS to enter the NIS along the coasts of Sicily. This led to the formation of a wide anticyclonic cell in the NIS. From the mid-1990s to 2010, the AIS was stronger and, favored by stronger cyclonic winds, detached from the coasts of Sicily heading directly towards the Levantine basin without penetrating the NIS. This process led to the formation of a wide cyclonic cell over the NIS. These results highlight the role of the AIS in controlling the circulation of the NIS.</div></div>","PeriodicalId":20620,"journal":{"name":"Progress in Oceanography","volume":"234 ","pages":"Article 103472"},"PeriodicalIF":3.8,"publicationDate":"2025-04-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143833977","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Trophic niche shifts in Japanese anchovy, Engraulis japonica, during ontogenetic migration in a temperate continental shelf system","authors":"Changseong Kim ,&nbsp;Jaebin Jang ,&nbsp;Jaesik Yang ,&nbsp;Jang Han Choi ,&nbsp;Hee Yoon Kang ,&nbsp;Seong Yong Moon ,&nbsp;Ho Young Soh ,&nbsp;Heeyong Kim ,&nbsp;Chang‑Keun Kang","doi":"10.1016/j.pocean.2025.103471","DOIUrl":"10.1016/j.pocean.2025.103471","url":null,"abstract":"<div><div>Understanding the mechanisms driving ontogenetic niche shifts in fishes has predominantly focused on dietary changes in large predatory migrants. This study investigates trophic niche dynamics in a small, pelagic migratory fish, the Japanese anchovy (<em>Engraulis japonicus</em>). By mapping migratory paths across varied oceanographic regions on a temperate continental shelf of Korean waters, we quantified changes in the trophic niche using δ¹³C and δ¹⁵N values across different ontogenetic stages (juvenile, subadult, and adult). We hypothesized that biological and ecological processes associated with fish ontogeny and migration cause trophic niche shifts. Results showed that juvenile anchovies had a narrow trophic niche, which expanded as they matured, indicating a shift from specialist to generalist feeding habits, unlike many large predatory fishes. Limited isotopic niche overlap among life stages suggested niche partitioning within inshore habitats where all stages coexist. Morphological and behavioral traits related to life history likely drive these feeding modes and prey use changes. Isotopic profiles varied with migratory routes, reflecting spatial variations in zooplankton isotope baselines. Adults showed higher δ¹³C in the southern offshore (Yangtze River Diluted Water area) and lower δ¹⁵N in the eastern offshore (Tsushima Warm Current area) compared with inshore (South Korea Coastal Water area), resulting in distinct isotopic niches. This isotopic variation is likely due to differing lower trophic-level processes and zooplankton assemblages, as supported by our dietary mixing model. Our findings highlight that ontogenetic changes in feeding habits and adaptive responses to prey availability along their migratory paths facilitate trophic niche shifts in Japanese anchovy.</div></div>","PeriodicalId":20620,"journal":{"name":"Progress in Oceanography","volume":"234 ","pages":"Article 103471"},"PeriodicalIF":3.8,"publicationDate":"2025-04-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143769094","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Wind-driven upwelling in the Adriatic Sea: Coastal vs. open-sea processes","authors":"Mirko Orlić ,&nbsp;Gordana Beg Paklar ,&nbsp;Tomislav Džoić ,&nbsp;Petra Lučić Jelić ,&nbsp;Iva Međugorac ,&nbsp;Hrvoje Mihanović ,&nbsp;Stipe Muslim ,&nbsp;Miroslava Pasarić ,&nbsp;Zoran Pasarić ,&nbsp;Antonio Stanešić","doi":"10.1016/j.pocean.2025.103470","DOIUrl":"10.1016/j.pocean.2025.103470","url":null,"abstract":"<div><div>The paper concentrates on the east Adriatic and a ten-day (20–29 May 2017) interval when a research cruise has been carried out, when the bottom probes have been operating close to the coast, and for which the satellite data have been available. Meteorological modeling has shown that two pulses of northern winds occurred at the time. The shipborne CTD and ADCP data collected on 28 May 2017 revealed a dense-water dome, with the surface cyclonic circulation developed around it, at a distance of 15–20 km from the coast. The temperature bottom probes and SST satellite sensors pointed to a decrease of temperature on two occasions, around 21 and 25–27 May 2017, close to the coast. The coincidence of the wind pulses with these processes in the sea indicated that they could be interpreted in terms of the wind-driven open-sea and coastal upwelling. In order to verify the interpretation, a simple analytical model has been developed and a combination of meteorological and oceanographic numerical modeling, with the wind field decomposed into the curl and curl-free components using the Helmholtz-Hodge approach, has been utilized. The theory and numerical simulations showed that the open-sea upwelling was related to the wind-curl effect while the coastal upwelling was controlled by interaction of the boundary and wind-curl effects. The phenomena were influenced by a positive feedback mechanism, which is more pronounced in shallow basins than in deep basins. This suggests that comparative studies of upwelling phenomena in different basins may be useful.</div></div>","PeriodicalId":20620,"journal":{"name":"Progress in Oceanography","volume":"234 ","pages":"Article 103470"},"PeriodicalIF":3.8,"publicationDate":"2025-04-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143816302","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Ocean mixed layer depth 2000–2020: Estimation assessment and long-term trends","authors":"Haochen Tang ,&nbsp;Chen Wang ,&nbsp;Huimin Li ,&nbsp;Yijun He","doi":"10.1016/j.pocean.2025.103467","DOIUrl":"10.1016/j.pocean.2025.103467","url":null,"abstract":"<div><div>Accurate estimation of mixed layer depth (MLD) is crucial for understanding the upper ocean dynamics as well as their implications on climate and marine ecosystems. While various methods have been proposed to estimate MLD from vertical temperature and/or density profiles, a systematic evaluation across different algorithms remains untapped. In this study, twelve approaches for MLD estimation are implemented and compared based on the Argo profiles collected from 2000 to 2020. Each method is assessed based on the quality index (QI), which measures the uniformity of temperature or density profiles within the boundaries of the estimated MLD. We found the two methods of linear fitting and relative variance exhibit similar QI levels higher than the others. A ranking scheme for that the method with the highest QI for a given profile earns one score is then designed and applied. The linear fitting one obtains the highest and is thus recommended as the most reliable method for geophysical analysis. The global MLD patterns derived using this method are analyzed with extremes being predominantly found in mid-latitudes due to strong seasonal variations. Significant long-term changes are observed, particularly in the southern hemisphere during summer, where the MLD shows a deepening trend over the past 20 years. Results presented here shall provide valuable insights for choosing the most reliable MLD estimation methods and understanding the environmental drivers of MLD variations.</div></div>","PeriodicalId":20620,"journal":{"name":"Progress in Oceanography","volume":"234 ","pages":"Article 103467"},"PeriodicalIF":3.8,"publicationDate":"2025-03-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143679753","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Internal wave energetics and interactions with mesoscale structures in the Sicily Channel area","authors":"Robin Rolland ,&nbsp;Pascale Bouruet-Aubertot ,&nbsp;Yannis Cuypers ,&nbsp;Aurélie Albert ,&nbsp;Julien Le Sommer","doi":"10.1016/j.pocean.2025.103465","DOIUrl":"10.1016/j.pocean.2025.103465","url":null,"abstract":"<div><div>The Sicily Channel plays a crucial role in the general circulation of the Mediterranean Sea. However, the internal wave dynamics is still sparsely characterized in this area which is a hotspot for internal tides. Here, we benefit from a high-resolution model of the Mediterranean Sea with and without tidal forcings to study the synoptic internal wave dynamics in the Sicily Channel area as well as their interactions with the (sub)mesoscale field. We found strong semi-diurnal internal tide generation in the Sicily Channel and the Messina Strait. Diurnal internal tides are generated in the Sicily Channel, Pelagie Islands and the Malta Plateau, and are bottom-trapped because of their sub-inertial frequency. In contrast near-inertial waves are mainly generated in winter in the Tyrrhenian Sea and the northern Ionian Sea. We show that the geometry of the Sicily Channel prevents near-inertial wave to propagate through it. Near-inertial waves are trapped in anticyclonic eddies. In summer, we show that diurnal-inertial internal waves generated by the intense thermal breeze near coastal areas are trapped in anticyclonic eddies with an effective inertial frequency close to the diurnal frequency even far from 30°N of latitude. Implications for turbulence and mixing are discussed. We present indirect evidence of an enhanced forward energy cascade in the presence of tidal motions. Future work will focus on the impact of tidal motions on the energy cascade using a nested non-hydrostatic numerical simulation.</div></div>","PeriodicalId":20620,"journal":{"name":"Progress in Oceanography","volume":"234 ","pages":"Article 103465"},"PeriodicalIF":3.8,"publicationDate":"2025-03-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143675638","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}

{"title":"Seasonality and interannual variability of physical, chemical and biological states and processes in the northern Barents Sea and adjacent areas","authors":"Bodil A. Bluhm,&nbsp;Johanna M. Aarflot,&nbsp;Tove M. Gabrielsen,&nbsp;Øyvind Foss,&nbsp;Agneta Fransson,&nbsp;Nils Olav Handegard,&nbsp;Oliver Müller","doi":"10.1016/j.pocean.2025.103469","DOIUrl":"10.1016/j.pocean.2025.103469","url":null,"abstract":"","PeriodicalId":20620,"journal":{"name":"Progress in Oceanography","volume":"234 ","pages":"Article 103469"},"PeriodicalIF":3.8,"publicationDate":"2025-03-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"143891525","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}