How do we actually measure Bahía Blanca's coastal currents?

Discover how to measure Bahía Blanca's coastal currents using ADCP. Learn equipment requirements and selection.

1. Where is Bahía Blanca?

Bahía Blanca, a port city of considerable size in Argentina, is located geographically on the southern coast of the country, along the banks of the large estuary with which it shares its name. The estuary, a broad body of water that flows over 100 kilometers in length, is a vital connection between the Atlantic Ocean and the continent's interior. This advantageous geographical position has made Bahía Blanca a significant commercial center for maritime trade, as its new port holds a mix of cargo, ranging from agricultural products to industrial material.

The city itself is a blend of urbanisation and nature. Its skyline consists of a mix of commercial structures, industrial factories, and residential suburbs. The surrounding shoreline of Bahía Blanca is characterized by a mix of sand beaches, mudflats, and salt marshes which are important habitat areas for numerous bird, fish, and other aquatic species. The water of the estuary is influenced by the interaction of freshwater from the Negro and Colorado rivers and saltwater from the Atlantic Ocean, leading to a dynamic and productive ecosystem. The location of the city on the coast, coupled with the fact that it is a prime transportation and industrial hub, make it such that studying the coastal currents around Bahía Blanca is not just of scientific concern but a prerequisite to maintaining safe navigation, defending the environment, and supporting the local economic enterprises.

2. How are the coastal currents off Bahía Blanca?

The nearshore currents off Bahía Blanca are governed by an incredibly large number of interacting variables. Large - scale circulation of the South Atlantic Ocean plays a major role. Impact from the Brazil - Malvinas Confluence, still farther south, is felt within the region as eddies and meanders created by that interaction extend to the north and affect the ocean off Bahía Blanca. These oceanic features can reverse the direction and speed of the local currents, introducing variability to the system.

Another significant component is the input of freshwater from the Negro and Colorado rivers. The continuous input of freshwater into the estuary alters the water's density and salinity, creating circulation patterns throughout the estuary. This fresh-water outflow creates a surface-layer current which generally flows to the ocean and interacts with the approaching oceanic currents. The strength and direction of this current driven by fresh water can drastically alter with river discharge in varying seasons, which is itself regulated by rainfalls, snow melt, and anthropogenic water control in the catchments of rivers.

Local wind fields also strongly control the coastal currents. Bahía Blanca experiences a range of wind conditions throughout the year. Strong winds, particularly those from the south and southwest, are strong enough to cause significant surface - water movement. These winds can push water along the coast and cause wind - driven currents that interact with oceanic and river - influenced currents. Tidal forces also contribute to the variations of the coastal currents. The semi - diurnal tides in the estuary cause high frequency variations of water level, producing ebb and flood currents that add further complexity to the current regime around Bahía Blanca. The complexity of estuary geometry in terms of numerous channels, bays, and inlets also distorts further the movement of these currents, making research on the coastal current situation complex but important to deciphering the surrounding marine environment.

3. How is coastal water flow of Bahía Blanca measured?

There are various techniques that are employed to monitor the coastal water flow of Bahía Blanca. Surface drifting buoy technique is a traditional one. Drifting buoys equipped with tracking devices such as GPS are tossed into the ocean. These buoys get carried by the surface currents, and their path is tracked for some duration. By analyzing the trajectories of buoys, researchers can determine the direction and speed of surface-layer currents. The method will be effective for information on surface flow only and may not represent the current status at deeper depths.

Anchored ship technique is employed, where a ship is moored in a fixed position on the coast or within the estuary. Equipment on board, such as current meters, are employed to measure the movement of water at various depths in the area around the ship. While the method can yield more accurate depth-specific data, it is limited by the fixed position of the ship and can be affected by the presence of the ship, which could alter the original patterns of the movement of water.

On the other hand, the Acoustic Doppler Current Profiler (ADCP) method has been an extremely advanced and useful technique for the measurement of coastal currents. ADCPs can simultaneously measure the water velocity at a number of depths, providing a full description of the current structure in the water column. They are thus the ideal tool to study the complex and dynamic coastal current systems off Bahía Blanca. With their capacity to measure three - dimensional water flow information, ADCPs are capable of displaying the complex patterns of currents, such as the interaction between surface, mid - water, and near - bottom flows, that are critical for a complete comprehension of the hydrodynamics of the estuary.

4. How do ADCPs based on the Doppler principle operate?

ADCPs operate on the Doppler principle. They transmit sound waves into the water column at a specific frequency. The sound waves penetrate the water and strike suspended particles in the water, such as sediment, plankton, and small animals. Water in motion carries the particles with it, producing a change in the frequency of back-scattered sound waves when these reach the ADCP.

By precisely measuring this change in frequency, the ADCP can calculate the water velocity at different depths. The instrument is typically equipped with multiple transducers that transmit signals at multiple angles. This allows the ADCP to measure the three-dimensional velocity components of the flow of water in horizontal and vertical directions. Gathered data are then processed by onboard or offboard computers to generate comprehensive visualizations and reports of the existing conditions. With this, scientists can examine in detail the complicated flow pattern of the coastal waters within and near Bahía Blanca, and this is greatly informative in monitoring the water mass movement and dynamic of the estuary's marine system.

5. What are the requirements for high-quality measurement of Bahía Blanca coastal currents?

For precise measurement of Bahía Blanca coastal currents, there are several significant features that the measuring equipment needs to have. Material durability is the most important. The ocean environment surrounding Bahía Blanca, with its high saltwater corrosion, rough waves, and fluctuating temperatures, poses a significant challenge to the equipment. The measuring equipment should be able to withstand these harsh conditions for an extended duration of time to deliver precise and reliable data gathering.

A minimal size and light weight are also critical. This makes the equipment easier to deploy and transport, especially in the crowded port locations and large - scale estuary survey exercises. Low power consumption is also critical in that it provides uninterrupted long - term operation, particularly in remote locations where power supply is insufficient. Also, a low-cost design would be highly desirable, as it would enable more extensive deployment and application and enable mass monitoring of the coastal currents in different parts of the estuary.

As far as the casing of the ADCP is concerned, the application of titanium alloy is excellent. The titanium alloy has superior corrosion resistance, which guarantees the ADCP is shielded from the corrosive properties of the salt-water environment of the Bahía Blanca estuary. It is also very strong and light, providing the required strength without increasing the overall weight of the ADCP to an unacceptable value. Such properties render titanium - alloy - cased ADCPs suitable to work in the severe marine environment of Bahía Blanca, where it is possible to obtain reliable and long - term measurements of the coastal currents.

6. How to Select the appropriate equipment for current measurement?

Selecting the appropriate equipment for current measurement in Bahía Blanca depends on several factors. The application to which the equipment will be subjected is one of them. Ongoing monitoring onboard a moving ship, for example, cargo shipping or marine research activities, demands a vessel-mounted ADCP. It is able to monitor currents in real-time when the ship traverses the waters of the estuary and the surrounding ocean, making important data available regarding the currents along the path of the vessel.

For fixed - location, long - term monitoring of near - bottom currents, a bottom - mounted ADCP is a better option. It can be placed on the bed of the estuary or seafloor and record current data for years without needing continuous ship presence. A buoy-mounted ADCP is best suited for measuring surface and upper-water-column currents in a flexible manner, as the buoy may be stationed at different positions according to research requirements, allowing for far-reaching coverage of the surface-level flow behavior in the estuary.

The frequency of the ADCP should also be selected carefully according to the water depth. A 600kHz ADCP is suitable to a depth of 70m, with reasonable measurements in slightly shallower water that is often found in certain parts of the Bahía Blanca estuary. A 300kHz ADCP can go to a depth of 110m, giving a reasonable trade-off between measurement resolution and depth of penetration. For deeper water, up to 1000m, a 75kHz ADCP is the option, as its lower frequency allows it to penetrate deeper into the water column, which may be necessary in the outer parts of the estuary or near the ocean mouth.

There are several well-known ADCP manufacturers on the market, such as Teledyne RDI, Nortek, and Sontek. Nonetheless, for users looking for affordable alternatives, the ADCP supplier China Sonar's PandaADCP is recommended. Constructed entirely of titanium alloy, it has great performance with a reasonable price tag. It is a good option for users who want budget-friendly ADCPs but still need to get coastal current measurements done. For more information, you can visit their official website: https://china-sonar.com/.

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.
Jack Law November 6, 2024
Share this post
Archive
How do we measure Chapadmalal's coastal currents?
Learn how to monitor Chapadmalal's coastal currents with ADCP. Discover equipment needs and selection.