![temperatureSensor.jpg [Translate to English:] Integrierter Temperatursensor](/t3resources/imek/_processed_/4/0/csm_temperatureSensor_29cfc6474f.jpg)
For use in compact, cost-effective drifter buoys, sensors are required that provide precise and long-term stable measurements despite their small size. In large-scale drifter campaigns, sensor costs often represent the largest share of project expenses.
A central goal of the AMuSeD project is therefore the development of compact and affordable sensors for fundamental oceanographic parameters—particularly temperature and conductivity, which serve as the basis for determining salinity.
Inductive conductivity sensors enable low-drift, robust measurements over extended periods. Their encapsulated design provides reliable protection against corrosion and biofouling. Conductivity cells offer a more economical alternative but are more maintenance-intensive and less stable in long-term deployments.
Most commercially available sensors are designed for industrial applications and feature large, complex probes—often unsuitable for mobile maritime platforms and IoT systems. There is a clear need for compact, energy-efficient sensors with standardized data interfaces.
In addition to conductivity, local temperature measurement is essential for accurately determining water density according to TEOS-10. Developing an integrated temperature sensor in-house not only provides technical advantages but also offers significant cost-saving potential.
The iMEK is therefore developing miniaturized, combined conductivity and temperature sensors that can be seamlessly integrated into modular platforms like AMuSeD, enabling long-term, cost-effective, and precise measurement of fundamental oceanographic parameters.
With the ongoing development of the AMuSeD project, detecting flow fields above and below the drifter platform is becoming increasingly important. The focus is on the shallow coastal waters of the German Bight, where water depths typically reach up to 50 meters.
To measure flow velocities in the water column, acoustic Doppler current profilers (ADCPs) are primarily used. These sensors operate on the Doppler principle, measuring the movement of suspended particles in the water and enabling the calculation of flow vectors at different depth layers. Other methods, such as tracer-based approaches or satellite-supported surface measurements, can be used as supplements but generally do not provide complete vertical profiles.
However, for specific deployment in shallow coastal waters, many commercially available ADCP systems are technically oversized and economically impractical. Their size, power consumption, and cost far exceed the requirements of compact drifter platforms, often amounting to several times the production cost of an entire AMuSeD system.
Therefore, the project aims to develop customized, miniaturized flow sensors that enable cost-optimized and energy-efficient detection of flow fields in the North Sea. Such systems could not only allow better interpretation of drifter movements but also provide valuable data on vertical and horizontal flow structures—a crucial contribution to understanding dynamic processes in shallow shelf seas.
