How do we measure the coastal currents of São Miguel do Gostoso?

Learn how to monitor São Miguel do Gostoso's coastal currents with ADCP. Discover equipment needs and selection.

1. Where is São Miguel do Gostoso?

São Miguel do Gostoso is a small seaside town in the state of Rio Grande do Norte, located in the northeast region of Brazil. It is along the Atlantic coast, on a strip of land that is known for its natural beauty. The town is surrounded by a rare landscape with a combination of white sandy beaches, clear blue water, and mangrove jungles.

Geologically, the São Miguel do Gostoso area has low-lying coastal plains. The seafloor off the coast is complex in bathymetry with varying depths and underwater features such as reefs, sandbars, and channels. The local coastal currents are greatly influenced by these underwater features. The nearby Potengi River also influences the coastal ecosystem. The river discharges fresh water to the ocean, which affects the salinity and density of coastal water.

The town is rich in history. The area was once inhabited by native peoples, and signs of them can be seen today in local traditions, art, and legend. Portuguese colonizers came to the area in the 16th century, bringing new farm and trading practices with them. São Miguel do Gostoso developed over centuries into a small but vibrant coastal town whose economic backbone was fishing and tourism.

2. How is the condition of coastal currents near São Miguel do Gostoso?

The coastal currents along São Miguel do Gostoso are decided by a complex interplay of factors. One of the Atlantic Ocean's large ocean currents, the South Equatorial Current, has a central role. As it approaches the coast of Brazil, it interplays with the topography and the bathymetry of the region. Along São Miguel do Gostoso, the South Equatorial Current may divide into small streams, creating a complex network of coastal currents.

Tidal operations within the Atlantic Ocean are of significant importance. Semi - diurnal tidal cycle is accountable for initiating periodic water - level fluctuations. Tidal currents are more powerful during spring tide as a result of more powerful gravitational pull from the sun and the moon. Tidal currents interact with the South Equatorial Current and also the coastlines forms along the location, making their overall trend influence the movement of coastal water. The tides also induce the formation of rip currents, or strong and narrow currents flowing away from the beach. Rip currents are dangerous to swimmers and are an important consideration in terms of coastal safety.

Regional prevailing winds, mostly the northeasterly trade winds, also influence the coastal currents. Surface waters are driven by the winds in one direction, creating a wind-driven current. The wind-driven current is also in contact with the South Equatorial Current and tidal currents, further complicating the pattern of water movement. The seabed bathymetry onshore at São Miguel do Gostoso, comprised of reefs, sandbars, and channels, either guides or disrupts the movement of the currents. Reefs, for example, are barriers that can deflect the water to move around, while channels accelerate the current.

3. Measurement of São Miguel do Gostoso coastal water movement

Surface Drifting Buoy Technique

Surface drifting buoy technique is the traditional means through which one measures coastal water movement. Researchers launch buoys with tracing mechanisms into the ocean. Monitoring the movement of the buoys over a period of time helps them understand the direction and speed of surface currents. There are some downsides to using the technique. It only measures the surface layer of the water column, and the buoys are highly susceptible to wind interference. Wind can displace the buoys in a manner that is non-representative of the motion of the actual underlying currents.

Moored Ship Method

The moored ship method employs a moored ship as a platform for current measurement. Instrument are dropped off the ship to measure the flow of water at varying depths. Although the information obtained by this method may be useful enough for vertical profiles of the currents, it has its own disadvantages. In this method, spatial coverage is limited to the vicinity of the moored vessel, and the presence of the ship may result in interference with normal flow, which could make the measurements inaccurate. To keep the ship moored for a long time is logistically difficult and expensive.

Acoustic Doppler Current Profiler (ADCP) Technique

ADCP current profiler is now an even more advanced method of observing coastal currents. ADCPs are capable of observing water currents over the wide vertical extent with high-resolution data on the water column's velocity profile. ADCPs may be installed on a range of platforms including ships, buoys, and the seafloor. Shipboard ADCPs may sample continuously as the vessel moves along, observing a vast area in a relatively short time. Bottom-mounted ADCPs are capable of making fixed-point, long-term measurements, and therefore researchers can study long-term coastal current patterns.

4. How do ADCPs operated on the Doppler principle work?

ADCPs operate on the Doppler principle. They transmit acoustic pulses into the water. The pulses bounce off suspended particles such as sediment, plankton, or bubbles in the water. When the water is in motion, the frequency of the returning pulses changes. The ADCP measures this frequency change and calculates the relative water velocity to the instrument.

Most ADCPs incorporate multiple transducer beams, typically four or more, at different angles. The multi-beam configuration is used to measure the three-dimensional speed of water. Combining returns from the beams, the ADCP is able to provide a complete view of the current speed at different depths of the water column. The data collected with the ADCP can be processed in real time or stored for off-line processing, and it is of significant help to have data on the dynamics of the coastal currents.

5. What is needed to obtain high-quality measurement of São Miguel do Gostoso coastal currents?

To accurately measure São Miguel do Gostoso's coastal currents, the instrument should possess several important characteristics. It should be made of strong material, have a small size, be light, have low power, and be cheap. All these characteristics make it possible to cast in very large quantities to achieve wide spatial coverage.

Titanium alloy casing ADCPs are highly recommended. Titanium alloy offers better corrosion resistance, which is vital for the long-term operation in the corrosive seawater environment. It resists corrosion by the corrosive action of saltwater, guarding the internal ADCP components from damage. Titanium alloy is also light and strong, giving the instrument strength and mobility. This set of characteristics allows for one to receive precise and long measurements of the São Miguel do Gostoso currents.

6. How to Choose the right equipment for current measurement?

Choice Based on Application

The choice of ADCP profiler varies with its application. If there are measurements to be taken using the ship as a platform, then ship-mounted ADCPs would be the most appropriate choice. They are able to provide real-time data as the ship moves in the water, covering a broad space in a short duration of time. Bottom-mounted ADCPs are more suitable for fixed-point long-term observations. They are able to provide continuous data over an extended period of time so that scientists can analyze long-term patterns in the coastal currents. Floating ADCPs are also used for observing the migration of water masses over large areas, providing valuable information regarding large - scale circulation patterns.

Selection Based on Depth

Frequency of ADCP also needs to be selected in terms of depth of water. In waters shallower than 70m, the 600kHz ADCPs work well. In shallow water, they are capable of delivering high-resolution observations. For 110m maximum, the use of 300kHz ADCPs will be recommended. For larger depths, in up to 1000m waters, the use of 75kHz ADCPs will be advisable.

There are quite a few reputable ADCP brands available in the market, including Teledyne RDI, Nortek, and Sontek. But if one is looking for cost - efficient alternatives, then the ADCP manufacturer China Sonar's PandaADCP comes highly recommended. Made from completely titanium alloy, it provides outstanding performance at low costs. It is a good choice for frugal users who need to rely on dependable ADCPs for measuring coastal currents. You can find more information about them on 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 January 16, 2025
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