Field report № 3 · Anlo coast, Volta Region, Ghana
The sea keeps redrawing the line.
Between Dzita and Aflao, the Atlantic is moving a coastline that people live on. Keta has already lost streets to the sea. Since May 2018, survey teams from the Centre for Coastal Management have walked the same transects through the same fishing towns — carrying GPS rovers, drones and wave buoys — writing down exactly where the land is. This is what six field seasons have recorded.
Reporting from sixteen survey stations, west → east · Centre for Coastal Management, UCC§ 1 · field report
Overview
In Ghana and maybe the entire West Coast of Africa, there are issues at both national and regional scales accounting for lack of data. Data is unavailable along the beaches in West Africa to help better appreciate and compute the variability and fluctuations in morphology observed at the beaches.
A large-scale survey was initiated to provide information to understand the morpho- and hydrodynamic evolution of the Lower Volta Basin, between Ada and Aflao, and other areas within the Bight of Benin. The first stage of the survey program focuses on the Volta Delta coastline, its topogragphy and nearshore bathymetry as these control other parts of the Delta.
The Volta Delta lies within the Keta Basin, which is one of several fault-controlled sedimentary basins in West Africa (Appeaning Addo et al. 2018). The delta is low-lying and almost flat, featureless and descends gradually from inland to the Gulf of Guinea, thus exposing it to various hazards.
§ 2 · field report
HistoricalSurvey
Several beach surveys and experiments have been conducted along the beaches in Ghana and West Africa. These experiments were not conducted on a regular basis and have all ended. They include: Grand Popo beach experiment in Benin, 2013, Saint Louis Beach 2016 COASTVAR Experiment and Afrobarometer Survey in Senegal, 2021.
The first intensive nearshore field experiment in the Gulf of Guinea was conducted at Grand Popo Beach, Benin, in February 2013, on an open wave-dominated micro- to meso-tidal coast, located mid-way between Cotonou and Lomé harbours.
Nonetheless, that project did not cover large spatial extent and was done annually for two years. The current program of survey will complement existing data on the Delta.
§ 3 · field report
SiteDescription
This survey is focused on the lower Volta Delta and its surrounding coastal areas within the Bight of Benin. The Bight of Benin coastal area is characterized by high population density, schools, harbours and farmlands. The Bight of Benin, in the Gulf of Guinea, is more than 400 km long, ranging between 1° to 5°E in longitude, and 5 to 7°N latitude facing the South Atlantic Ocean. This embayment covers the coastal environments of four countries: Ghana, Togo, Benin, and Nigeria. It is a wave-dominated coast formed by sandy beach-ridge barriers and lagoons, bordered by the Niger River Delta in the east and the Volta River Delta in the west, and fed by several small coastal rivers and lagoons (Abessolo et al., 2021).
The coastline is vulnerable to coastal flooding and episodic erosion. Wave climate. It is an open environment exposed to long swell waves that travel far from mid- to high latitudes (45-60°) in the South Atlantic as well as to locally generated short-waves in the tropical band(6°N-15°S). The mid- to high-latitude wind regime is characterized by strong westerlies whereas the subtropical area (30-35°S) is dominated by south easterly trade winds blowing off the coast of Namibia.
The southwesterly swells impinge slightly obliquely (at angles of 10-15°) on the nearly rectilinear west-east oriented Bight of Benin coast, generating the afore-mentioned unidirectional and large longshore drift toward the east (Almar et al., 2015). The tidal regime is microtidal (from 0.3 m to 1.8 m for neap and spring tidal ranges, respectively).
§ 4 · field report
Data ToBe Collected
In order to initiate the development and validation of erosion and flooding models as well as evaluate regional coastal zone management policies in terms of their effectiveness, efficiency, coherency, and relevance;
This Project will collect data on water levels, nearshore swell waves, nearshore bathymetry on a 15-arc resolution, currents of sediment drifts, discharge and flow rates from some key rivers (e.g., Mono, Oti, and Volta Rivers), Shoreline changes, and beach topography
Generally, the beaches of Ghana are composed of coarse-grained sediments, such as sand and gravel, with some areas having a mix of sediment sizes. There is erosion evidence in some places along Ghana's coastline as a result of both human activity (such as sand mining) and natural processes (such as wave action, tidal currents, and storm surges). These erosion-prone areas may have less sediment accumulation, resulting in a narrower beach profile
In summary, the data to be collected will be hosted on this website and released to stakeholder on agreed request.
§ 5 · contents of the record
Six datasets,one coastline.
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01
Waves
deployment May 2023 – Aug 2023
1,415 wave records -
02
Topography
campaigns Jan 2023 – Oct 2024
5,110 beach-profile measurements - 03 Bathymetry first survey in preparation
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04
Shoreline position
campaigns May 2018 – Oct 2024
11,388 shoreline points -
05
Orthophotos
flown May 2018 – Oct 2024
46 orthophoto mosaics - 06 Drone, video & camera catalogue in preparation
1,415 wave records from a single instrument — logged whether or not anyone was watching.
wave record · deployment May 2023 – Aug 2023§ 6 · the survey team · 1 member
The people onthe transect.
§ 8 · to researchers
The record isyours to use.
Every published dataset above is available on request for research and public-interest use: raw profiles, processed shorelines, wave spectra and orthomosaics, with station coordinates and campaign notes. Tell us what you are working on and which stations and periods you need. We ask two things in return: cite the programme in anything you publish, and where your findings concern a particular town, help us bring them back to the people who live there.
Request the data Centre for Coastal Management · University of Cape Coast · Response within 5 working days