1. Where is Rijeka?
Rijeka is a major and vibrant city located on the northern Adriatic Sea in Croatia. It is situated enclosed in the Kvarner Gulf, which is one of the main inlets of the Adriatic. Due to its strategic position, over the centuries it has developed into an indispensable port and a center of commerce, culture, and transport.
Geographically, Rijeka is surrounded by a diverse landscape: to the east, it is dominated by the U ka mountain range that rises majestically, forming a dramatic backdrop to the city, while the coastal area is of mixed aspect, with rocky shorelines giving way to small, sandy beaches in places. Off the coast of Rijeka, there is a complicated bottom topography, including shallow shelves close to the shore and deep channels while going more open in the gulf. Such complicated bathymetry strongly affects the local coastal currents.
Culturally, Rijeka is a real melting pot because it has been under the rule of different civilizations-for centuries, from the Romans to Austrians and Italians. It is reflected in its architecture, as witnessed by the many grand Austro-Hungarian-era buildings in the heart of the city, such as the Rijeka Town Hall, which bears witness to that sumptuous era. Also, the local cuisine is part of its diversity in history: it is very tasty, a mixture of Mediterranean and Central European flavors, emphasizing fresh seafood.
2. What is the condition of the coastal currents around Rijeka?
The coastal currents around Rijeka are influenced by various conditions. One of the major ones is related to wind patterns. One of the most well-known strong cold northeasterly winds, the Bora, is one of the meteorological features very often present along this area. The Bora is capable of giving a drastic turn to surface currents whenever it blows. It can push the surface water towards the shore, increasing the speed and changing the direction of the coastal currents. The Jugo is southerly wind that may have the opposite effect and pushes the water away from the coast.
Tidal forces act even as the tidal range is not big in the Adriatic Sea. The periodic rising and fall of the sea because of the tides interact with the bathymetry of that place. Around Rijeka, where submarine ridges, canyons, and a generally shallow area exist, such a complex nature of the seabed will result in channeled and changed tidal currents which may make the current system very complicated in some areas of stronger or variable currents.
The other factor involves river discharges. The Rijeka River and the rest of the minor streams discharge into the Kvarner Gulf. In this respect, freshwater input could impact the density variations in the coastal waters. This less dense freshwater tends to float atop the surface of saltier seawater, creating a two-layer system that can affect the current patterns, especially near the river mouths.
3. How to observe the coastal water flow of Rijeka?
Surface Drifting Buoy Method
Surface drifting buoys are a simple method for observing currents along coasts. These kinds of buoys are equipped with either GPS or satellite-tracking devices. Once thrown into the water, they drift with the movements of the surface waters. By tracking the buoys' movements over time, researchers can calculate the direction and speed of the surface - level currents. However, this technique is applicable only to the surface layer of the water column, usually up to a few meters deep, and may not be representative of the currents at greater depths.
Anchor-moored Ship Method
An anchor-moored ship can be used to measure coastal currents. Current meters are attached to the ship's hull at different depths. As the water flows past the ship, these meters record the speed and direction of the current at each depth. This method allows for the collection of data from multiple depths, providing insights into the vertical structure of the currents. Nevertheless, it is confined to the zone of the ship's mooring, and the presence of the ship can interfere with natural water circulation, which possibly influences the measurement results.
Acoustic Doppler Current Profiler (ADCP) Method
The Acoustic Doppler Current Profiler (ADCP) represents one of the most sophisticated and handy tools for current measurements along the Rijeka coast. It can be installed on a ship, on the seabed, or on a buoy. ADCPs transmit acoustic signals into the water. These signals, in turn, are scattered by water-suspended particulates-mostly plankton or sediment, even small bubbles. An ADCP current meter calculates the velocity at different depths into the water column with high precision through the analysis of the Doppler shift of the reflected signals. This method gives high-resolution data over a large area, allowing detailed insight into the three-dimensional structure of the coastal currents.
4. How do the ADCPs using the Doppler principle work?
The principle of ADCPs is based on the Doppler principle. This instrument emits acoustic signals with fixed frequency. After those signals have collided with the moving particles in the water, the reflected signal frequency will be different from that of the emitted ones. When those particles go towards the instrument, the reflected frequency is higher and vice versa: a blue shift and red shift. It is the frequency shift that the ADCP measures. However, by knowing the original frequency of the emitted signal, and having a measure for the frequency of the reflected signal, it is able to compute for the water's velocity. For computing three-dimensional flow velocities of the water, an ADCP current profiler sends several angle signals. Besides, the time of flight of the acoustic signals to the particles and back allows the ADCP to calculate the depth at which the velocity measurements are taken.
5. What's needed for high-quality measurement of Rijeka coastal currents?
Equipment Requirements
- Material Reliability: The casing of the ADCP flow meter shall be manufactured with materials able to resist the marine environment. Among the best options is a titanium alloy. It provides very good corrosion resistance, which is very important in the long-time operation mode in salty waters such as the Adriatic Sea. A titanium alloy may resist salt water corrosion, great mechanical tension, and high pressure in greater depth.
- Small Size and Light Weight: Small size and light weight mean that an ADCP is easier to deploy. It can easily be installed on different platforms, whether it is a small research vessel, buoy, or seabed-mounted applications. A reduced size minimizes the interference of the device with natural water flow and its impact on the flow.
- Low Power Consumption: Seeing that many of the ADCP deployments will depend on battery power or limited power supplies, low power consumption is a necessity. This would allow the device to run continuously for more extended periods without needing battery replacements or recharging. Long-term use, especially in coastal current monitoring, will require this.
- Cost-Effective: The ADCP meter to be used for large-scale measurement of the coastal currents around Rijeka should be relatively cheap. Lesser cost allows multiple devices to be deployed in various locations, leading to wider knowledge about the complex current patterns of the area.
6. Selection of Appropriate Equipment for the Measurement of Current
According to the Intended Use
- Ship-borne ADCP: In this type of ADCP, the instrument is installed on a moving ship. It is good to perform large-scale surveys of coastal currents. While the ship is sailing through water, the ADCP profiler will continuously measure the current at different locations and thus get a broad-scale view of the current patterns. This is useful for mapping out large areas of the coastal waters around Rijeka.
- Bottom-mounted ADCP: those being deployed at the sea bottom. This set of instruments offers fixed-point measurement over a period of time, in fixed points for that matter. By permanently staying on the bottom, the measurements will produce current conditions on a really greater, long drawn out times over one place alone. In a nutshell, these will come very useful if needed to be looking at the variability of long term and seasonal change of the current concerning its changes in velocity and along shore flow.
- Buoy-mounted ADCP: Buoy-mounted ADCPs are attached to floating buoys. They move with the water currents, providing real-time data on the movement of the water masses. This type is useful in studying the surface-layer currents and their short-term changes. It can also be used in tracking the movement of water masses in relation to weather events.
Based on Frequency
- The depth to which one wants to measure in the water is affected by the choice of the ADCP frequency. A 600kHz ADCP is generally good for waters of a maximum of approximately 70 m. It is best suited for giving high-resolution data for shallow water applications like the nearshore areas around Rijeka; thus, this higher frequency measures the relatively shallow coastal waters with more detailed measurements.
- A 300kHz ADCP can be used for water depths of about 110m. It could be very adequate for areas around Rijeka with moderate water depths. The lower frequency enables deeper penetration of the acoustic signals into the water column than in the case of the 600kHz ADCP.
- For deeper waters up to 1000m, a 75kHz ADCP is more in order. The lower frequency allows the acoustic signals to travel greater distances through the water and so this would make it suitable for measuring currents in deeper parts of the Adriatic Sea near Rijeka.
Recommended Brands
There are a number of well-renowned brands offering ADCPs in the market. Teledyne RDI, Nortek, and Sontek are among the leading manufacturers. However, for those looking for an economical yet high-quality option, the Chinese brand China Sonar PandaADCP is highly recommended. Made of all-titanium alloy, it offers excellent durability and corrosion resistance. This brand provides an outstanding cost-performance ratio, making it suitable for large-scale coastal current measurements around Rijeka. You can visit their website at (https://china-sonar.com/) for more information.
Here is a table with some well known ADCP instrument brands and models.
Brand | model |
---|---|
Teledyne RDI | Ocean Surveyor ADCP, Pinnacle ADCP, Sentinel V ADCP, Workhorse II Monitor ADCP, Workhorse II Sentinel ADCP, Workhorse II Mariner ADCP, Workhorse Long Ranger ADCP, RiverPro ADCP, RiverRay ADCP, StreamPro ADCP, ChannelMaster ADCP, etc. |
NORTEK | Eco, Signature VM Ocean, Signature ADCP, AWAC ADCP, Aquadopp Profiler, etc. |
SonTek | SonTek-RS5, SonTek-M9, SonTek-SL, SonTek-IQ, etc. |
China Sonar | PandaADCP-DR-600K, PandaADCP-SC-300K, PandaADCP-DR-300K, PandaADCP-SC-600K, PandaADCP-DR-75K-PHASED, etc. |
Estimating Coastal Currents of Rijeka