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The role of tidal residual currents in the North Aegean SeaNARA Subscribed
Spatiotemporal Patterns and Physical Drivers of Satellite-derived Chlorophyll-a in the Aegean SeaNARA Subscribed
Chlorophyll-a is widely used as an indicator of phytoplankton biomass and primary productivity in the Aegean Sea, with direct implications for marine ecosystem functioning. However, the connection of its variability to physical drivers in the region remain relatively understudied. This study investigates the interannual variability and long-term trends of sea surface chlorophyll-a in the Aegean Sea over 1998–2022 and their rel...
The evolution and drivers of dense water formation (DWF) in the North–Central Aegean Sea (NCAeg) during winter 2021–2022 are studied using observations from two Argo floats and the output of an operational data-assimilating model. Dense water with σθ>29.1 kgm−3 was produced over most of the NCAeg, except for the northeastern part covered by Black Sea water (BSW), where the maximum surface density was
Research infrastructures have been established throughout Europe in order to create robust organizations that will facilitate and enhance research and innovation processes and will advance society with innovative products and services. The Hellenic Integrated Marine Observing, Forecasting and Technology System (component of HIMIOFoTS RI) has been implemented in the framework of the National Roadmap for Research Infrastructures...
There is a general scarcity of oceanic observations that concurrently examine air–sea interactions, coastal–open-ocean processes and physical–biogeochemical processes, in appropriate spatiotemporal scales and under continuous, long-term data acquisition schemes. In the Mediterranean Sea, the resulting knowledge gaps and observing challenges increase due to its oligotrophic character, especially in the eastern part of the basin...
Acoustic Doppler current profiler observations of migration patternsof zooplankton in the Cretan SeaOA Marine
The lack of knowledge of the mesopelagic layer inhabitants, especially those performing strong vertical migration, is an acknowledged challenge. This incomplete representation leads to the exclusion of an active carbon and nutrient pathway from the surface to the deeper layers and vice versa. The vertical migration of mesopelagic inhabitants (macroplanktonic and micronektonic) was observed by acoustical means for almost 2.5 ye...
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