How do we measure the coastal currents of Porto de Galinhas?

Learn how to monitor Porto de Galinhas's coastal currents with ADCP. Discover equipment needs and selection.

1. Where is Porto de Galinhas?

Porto de Galinhas is a quaint seaside village in Pernambuco state, northeastern Brazil. It lies along the Atlantic Ocean, approximately 70 kilometers north of the state capital, Recife. The village is renowned for its natural beauty, with lovely beaches, azure water, and unique rock formations.

Geologically, the area around Porto de Galinhas is characterized by the conjunction of low-lying coastal plains and fossil coral reefs. The seabed along the coast is complex in its bathymetry, having irregular depths and a variety of underwater features such as sandbars, channels, and the aforementioned coral reefs. The coral reefs are not only an integral part of the native marine ecosystem but also play a role in the creation of the coastal currents. The village is also formed by the discharge of the small streams and rivers into the sea, affecting the salinity and density of the coastal water.

Porto de Galinhas has a rich history. The area had originally been settled by native inhabitants, whose heritage can still be seen in local tradition, artwork, and folklore. The Portuguese colonists arrived in the area in the 16th century, bringing with them new agricultural and trade practices. The village expanded over time into a small but important seaside town, with tourism and fishing making up its economy.

2. What are the coastal currents in front of Porto de Galinhas?

The coastal currents off Porto de Galinhas are controlled by a complicated interaction of a number of factors. The South Equatorial Current, which is one of the principal ocean currents in the Atlantic Ocean, is significant. When it arrives at the Brazilian coast, it interacts with the local topography and bathymetry. Off Porto de Galinhas, the South Equatorial Current can split into subsidiary branches, producing a complicated pattern of coastal currents.

Atlantic Ocean tides are of significant importance. The semi - diurnal tidal regime generates recurring water - level fluctuations. During spring tides, the increased gravitational pull of the sun and moon creates stronger tidal currents. The tidal currents interact with the South Equatorial Current and coastal geometry to influence the general motion of coastal waters. The tides also cause the formation of rip currents, or narrow, powerful currents that are directed away from the shore. Rip currents pose a threat of death to swimmers and cause serious concern when it comes to coastal safety.

Regional prevailing winds, mostly northeasterly trade winds, also influence coastal currents. Prevailing winds are capable of compelling surface waters to move in one direction, giving rise to a wind-driven current. The current, driven by the wind, is blended with the South Equatorial Current and the tidal currents, even more complicating the pattern of the movement of water. Bathymetry on the seabed near Porto de Galinhas, its coral reefs, sandbars, and channels can funnel or hinder the flow of the currents. Coral reefs, for example, may act as a barrier deflecting the water and forcing it to circumvent them, while channels cause the current to accelerate.

3. How to track the coastal water flow of Porto de Galinhas?

Surface Drifting Buoy Method

The surface drifting buoy method is a traditional method of tracking coastal water flow. Scientists drop buoys equipped with tracking devices into the sea. By tracking the drift of these buoys over time, they can determine the direction and speed of the surface currents. But this method has some drawbacks. It can only provide information about the surface layer of the water column, and the buoys are very susceptible to wind interference. The wind can cause the buoys to oscillate in a manner that is not indicative of the true motion of the currents below.

Moored Ship Method

The moored ship method involves utilizing an anchored ship as a platform to measure currents. Gear is lowered from the ship to measure the water flow at various levels. Even though the method can generate high-resolution vertical profiles of the currents, there are several drawbacks. The spatial range is limited to the area around the moored ship, and the ship may disturb the natural flow of the water and invalidate the measurements. Moreover, mooring a vessel for a few days can also prove to be logistically complex and costly.

Acoustic Doppler Current Profiler (ADCP) Technique

ADCP flow meter is now an advanced and convenient instrument to acquire coastal currents measurement. ADCPs can measure the water flows in a significant vertical range with complete information regarding the velocity distribution of the water column. They can be mounted on any one of a number of types of platforms: ships, buoys, or on the sea bed. Ship - mounted ADCPs may continuously record data as the ship travels, monitoring a large region in a brief period. Bottom - mounted ADCPs may provide long - term, fixed - point measurements, allowing scientists to monitor long - term trends in coastal currents.

4. How do ADCPs that rely on the Doppler principle work?

ADCPs operate on the Doppler principle. They project acoustic pulses into the water. They bounce back from suspended particles such as sediment, plankton, or bubbles in the water. When the water is in motion, the frequency of the back-scattered pulses shifts. Detecting this frequency shift, the ADCP calculates the speed of the water relative to the instrument.

Most ADCPs possess a number of transducer beams, typically four or more, pointed in different directions. The multi-beam configuration enables the three-dimensional water velocity to be measured. By integrating the signals of these beams, the ADCP current meter is able to generate a composite picture of the current velocity at different depths within the water column. The data obtained by means of the ADCP is subject to treatment in real - time or stored for further analysis, providing useful information as to the dynamics of coastal currents.

5. What is required for good-quality measurement of Porto de Galinhas coastal currents?

In order to obtain high-quality measurement of the coastal currents of Porto de Galinhas, the equipment for measurement should possess some significant characteristics. It should be made of robust materials, have small size, low weight, low power consumption, and low cost. These characteristics make it possible to use a high number of instruments to achieve good spatial coverage.

ADCPs with titanium alloy casings are highly recommended. Titanium alloy also possesses greater corrosion resistance, which is imperative for prolonged applications in the harsh marine environment. The alloy withstands corrosive action from seawater and thereby damage to internal ADCP parts is prevented. The titanium alloy is also rugged and lightweight and therefore the instrument is long lasting and transportable. This pairing of characteristics provides precise and long - term current measurements of coastal currents off Porto de Galinhas.

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

Usage - Based Selection

The ADCP selection relies on its use. Ship - mounted ADCPs are the most appropriate for ship - borne measurements. They can give real-time information as the vessel travels in the water, traversing a wide area in a relatively short distance. For fixed - point long - term monitoring, bottom - mounted ADCPs are better. They can give continuous data over a long period, enabling researchers to analyze long - term trends in the coastal currents. Floating ADCPs have the advantage of being able to monitor the drift of water bodies over extensive spatial scales, thereby giving useful indications of large-scale circulation patterns.

Choice Based on Depth

The ADCP frequency should also be established based on the water depth. In cases of water depths less than 70m, 600kHz ADCPs must be employed. These are capable of providing high-resolution measurements in shallow waters. In cases of water depths not exceeding 110m, 300kHz ADCPs must be employed. For deeper waters, which run up to 1000m, 75kHz ADCPs are more suitable.

There are a number of popular ADCP brands available in the market, including Teledyne RDI, Nortek, and Sontek. For users looking for budget - friendly solutions, though, the ADCP supplier China Sonar's PandaADCP is an excellent choice. Constructed completely of titanium alloy, it has great performance but at a very reasonable price. It is the perfect solution for cost - aware users who need good ADCPs for coastal current measurement without sacrificing performance. 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 July 31, 2024
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