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COUNTRY FILES (contd.)

GABON

1. GEOGRAPHY AND CLIMATE (after Welcomme, 1979)

Gabon (with a surface area of 257 670 km2) is divided into two main zones:

  1. a low-lying coastal region; and
  2. an interior plateau which is transected by river valleys and mountain chains of about 900 m in altitude. The highest peak is 1 550 m.

The climate is hot and humid with a long cold dry season from June to September, a short rainy season from October to December, a short dry season from December to January, and a long rainy season from January to May.

Gabon is very sparsely populated. The main commercial activity is forestry, the majority of the country being thickly wooded.

2. HYDROGRAPHY

2.1 Lakes

There are several freshwater lakes associated with the Ogoouè River flood-plain (Lakes Onangue, Azingo, Anengue, Avanga, Gome, Nkonie and Nguene). Lake Mandji lies on the lower Nyanga River. A complex of four small lakes near Bongo (Lakes Longo-Longo, Kisoro, Mafoumi and Gore) discharge into Ndogo Lagoon.

2.2 Rivers, Floodplains and Swamps

The main river in the country is the Ogoouè which rises in the highlands of the Congo but flows for 820 km through Gabon to discharge into the Atlantic at Port Gentil. There are several other rivers draining this wet and forested country, i.e., the Nyanga, the Benito and a series of tributaries of the Ogoouè. Floodplains are developed on the lower Ogoouè and its tributaries, the Ngounie and the Ivindo.

2.3 Reservoirs: None

2.4 Coastal Lagoons

There are four major (Nkomi, Ngobe, Ndogo and Mbia) and several minor lagoons.

2.5 Aquaculture

There were 2 000 ponds in 1959. In 1967 there were 1 093 ponds with a combined surface area of 35.5 ha. See section 4.1 for aquaculture production by species.

3. FISHERY PRODUCTION/POTENTIAL

3.1 Fish production and per caput supply

Table 1. FISH PRODUCTION AND PER CAPUT SUPPLY - Gabon, 1970–1987

 Nominal Production
(including exports)
(t) 2
Nominal Consumer Supply
(including exports)
(kg/person)
YearPopulation
'000
1
Inland captureAquaculture
3
Marine capture
6
TotalInland captureAquaculture
3
Marine captureTotal
1970   950   400- 4  3 600  4 0000.4-  3.8  4.2
1971   960   400-  3 600  4 0000.4-  3.8  4.2
1972   971   400-  3 600  4 0000.4-  3.7  4.1
1973   981   400-  4 500  4 9000.4-  4.6  5.0
1974   992   400-  4 500  4 9000.4-  4.5  4.9
19751 003   400-  5 656  6 0560.4-  5.6  6.0
19761 015   400-  5 656  6 0560.4-  5.6  6.0
19771 027   400-  5 656  6 0560.4-  5.5  5.9
19781 039   400-12 95013 3500.4-12.412.8
19791 0521 800-19 20021 0001.7-18.320.0
19801 0641 800-18 00019 8001.7-16.918.6
19811 0811 800-17 70019 5001.7-16.318.0
19821 0981 7928 518 80020 6001.60.00717.118.7
19831 1151 7928 517 60019 4001.60.00715.817.4
19841 1331 7982 519 20021 0001.60.00216.918.5
19851 1511 7982 519 20021 0001.50.00216.718.2
19861 1741 9763 518 81020 7891.70.00316.017.7
19871 1981 8973 519 00020 9001.60.00315.817.4

1 Source: FAO
2 Source: FAO Fisheries Department FISHDAB; see also section 4.1
3 included in “Inland capture” if not specified.
4 - = data not available.
5 Vincke, 1989, pers.comm.
6 From 1980 to 1983, marine exports were as follows: 1980: 166 t; 1981: 2 079 t; 1982: 1 422 t; 1983: 1 457 t.
Data for artisanal fisheries estimated in collaboration with Gabonese fishery authorities. Industrial catch in 1986 recorded as 8 600 t.

3.2 Inland catch range and potential yield

No detailed data available for Lakes Anengue, Azingo, Mandje and Onangue; Benito and Ogoouè Rivers; Mbia, Ndogo, Ngobe and Nkomi Lagoons.

Total annual yield: 1 800 to 1 900 t (1979–1987)
Potential annual yield: 2 500 t (estimate based on 500 t inland freshwater and 2 000 t in lagoons).

4. STATE OF THE FISHERY (adapted from Welcomme, 1979)

4.1 Yield

For a country with such an extensive network of inland waters, the 1970–77 nominal catch of 400 t quoted in Table 1 seems very low. Mougnassa (1977) advances a more reasonable figure of about 30% of the total national catch (6 056 t), which would put the recent yield at 1 800 t, a figure completely consistent with the 1 485 inland fishermen listed as working in the country.

Fig. 1

Fig. 1. MAP OF GABON

Even at 1 900 t (in 1986–87) the yield of the inland fisheries appears very low considering the extent of the resource. It may safely be suggested, therefore, that the fishery is underdeveloped - an observation confirmed by Mougnassa (1977), who describes the fishery as developing.

There is a small aquaculture sector which produces about 2–8 t of fish per year (1982–1987).

Production, by species, from aquaculture in Gabon from 1982 to 1987 is reported by Vincke (1989, pers.comm.) as follows:

Species198219831984198519861987
Oreochromis niloticus8 t8 t2 t2 t3 t3 t

4.2 Factors influencing yield

At present human and sociological factors seem to be keeping the fishery at a low level of productivity. Fishermen are not abundant and are badly equipped. There is little infrastructure in the form of training establishments or marketing networks or sales facilities for fishing gear.

4.3 Future development possibilities

It is fairly certain that the inland fisheries of Gabon will develop in the future. More catch can be anticipated from the natural waters and, with the recent introduction of aquaculture, the production of freshwater fish could probably be increased consistently.

5. KEY BIBLIOGRAPHY

Collart & Giudicelli, 1984
Deceuninck, 1988

6. WATER BODIES DIRECTORY

Lakes  
AnengueBongo Lake ComplexOnangue
AzingoMandje 
   
Rivers  
BenitoOgoouè 
   
Lagoons  
Mbia (= Mbanio)Ngobe 
NdogoNkomi 

LAKE ANENGUE

Geographical data 
Location:Gabon - 1° 8'S; 9° 28'E
Surface area:88 km2
Max. length:18 km
Max. width:7 km
Inflowing river:Ogooué (lateral spillage)
Outflowing river:Ogooué

LAKE AZINGO

Geographical data
Location:Gabon - 0° 34'S; 10° 2'E
Surface area:106 km2
Max. length:19 km
Max. width:8 km
Inflowing river:Ogoouè (lateral spillage)
Outflowing river:Ogoouè

BONGO LAKE COMPLEX

Geographical data
Location:Gabon - 2° 15' -22'S; 10° 6'-11'E
Special features:a tandem series of four small lakes (Longo-Longo, Kivoro, Mafoumi and Gore, in upstream to downstream order). The outflow from Lake Gore enters Ndogo Lagoon.

LAKE MANDJE

Geographical data 
Location:Gabon - 2° 50'S; 10° 22'E
Surface area:45.5 km2
Max. length:13 km
Max. width:5 km
Inflowing river:Nyanga (lateral spillage)
Outflowing river:Nyanga

LAKE ONANGUE

Geographical data
Location:Gabon - 0° 58'S; 10° 4'E
Altitude:30 m asl
Surface area:167.5 km2
Max. length:32 km
Max. width:20 km
Inflowing river:Ogoouè (lateral spillage)
Outflowing river:Ogoouè

BENITO RIVER
(International water)

Geographical data 
Source:northern Gabon
Altitude:700 m asl
Total length:365 km
Countries traversed:Equatorial Guinea (Rio Muni), Gabon
Discharges to:Atlantic Ocean - 1° 35'N; 9° 37'E

OGOOUE RIVER
(International water)

Geographical data 
Source:Congo (Leketi, Zala and Massa Mountains)
Altitude:880 m asl
Total length:920 km (100 km in Congo, 820 km in Gabon)
Drainage area:205 000 km2 (at Lambarene)
Countries traversed:Gabon, Congo
Major tributaries:Ivindo, Ngouniè, Ofoouè
Discharges to:Atlantic Ocean - 1° 2'S; 8° 53'E
Volume of discharge at mouth:
 1 950–7 340 m3/sec (mean monthly);
 13 500 m3/sec (maximum)
Flood regime:bimodal flood with peaks in April-May and November-December
Special features:large floodplain in lower reach with several associated lakes (Anengue, Ovanga, Onangue, Gome, Nkome, Azingo and Nguene). Other swampy/floodplain depressions associated with Ngoumiè and Ivindo tributaries (the latter mostly in Congo).

MBIA (= MBANIO) LAGOON

Geographical data 
Location:Gabon - 3° 23–46'S; 10° 40-11° 10'E
Surface area:242 km2
Max. length:69 km
Max. width:5 km

NDOGO LAGOON

Geographical data 
Location:Gabon - 2° 23'–40'S; 9° 38'–10° 10'E
Surface area:582 km2
Max. length:64 km
Max. width:13 km
Inflow:discharge from Bongo Lake Complex

NGOBE LAGOON

Geographical data 
Location:Gabon - 1° 51'–2° 6'S; 9° 16'–36'E
Surface area:402 km2
Max. length:41 km
Max. width:14 km

NKOMI LAGOON

Geographical data 
Location:Gabon - 1° 20–44'S; 9° 1–36'E
Surface area:806 km2
Max. length:72 km
Max. width:16 km

7. BIBLIOGRAPHY

Barret, 1983
Collart & Giudicelli, 1984
Deceuninck, 1988
Mougnassa, 1977
Welcomme, 1972; 1979

THE GAMBIA

1. GEOGRAPHY AND CLIMATE

The Gambia (surface area of 10 000 km2) is a long, low-lying strip of land flanking the Gambia River for the lower 480 km of its course. Nowhere does the land rise above 40 m in altitude. Much of the river is estuarine and mangroves penetrate upstream for a considerable distance. Salt water penetrates 150 km upstream in the floods and 200 km during the dry season.

The winters are cool and summers warm. The climate is dry for most of the year, with a single rainy season lasting from June to September. The flood of the river coincides with this.

The Gambia is a wholly agricultural country whose activities are confined to the banks of the river. There is some rice culture, but little flood control or irrigation. On the whole the flood regime still controls the activities of the rural communities.

2. HYDROGRAPHY

2.1 Lakes: There are no lakes.

2.2 Rivers, Floodplains and Swamps

The country is dominated by one river, the Gambia, entering from Senegal. During the rainy season about 40% of the country is flooded.

2.3 Reservoirs: None

2.4 Coastal Lagoons

There is one small lagoon on the north shore of the Gambia River estuary near Njakunda.

2.5 Aquaculture

Vincke (1989, pers.comm.) estimates the following aquaculture production units existing in 1985: breeding centres: 1 (surface area: 1 ha); family type ponds: unknown.

3. FISHERY PRODUCTION/POTENTIAL

3.1 Fish production and per caput supply

(See Table 1)

3.2 Inland catch range and potential yield

Annual catch: Gambia River (1977–82): 1 423–3 508 t.
Total annual yield: 1 400–3 500 t
Potential annual yield: 2 000–8 000 t (Welcomme, 1979)

Table 1. FISH PRODUCTION AND PER CAPUT SUPPLY - Gambia, 1970–1987

 Nominal Domestic Production
(excluding exports)
(t) 2
Nominal Consumer Supply
(excluding imports and exports)
(kg/person)
YearPopulation
'000
1
Inland captureAquaculture
3
Marine capture
6
TotalInland captureAquaculture
3
Marine captureTotal
1970469   800- 45 000  5 8001.7-10.712.4
1971479   800-5 200  6 0001.7-11.012.5
1972490   800-5 200  6 0001.7-10.612.2
1973501   800-9 60010 4001.6-19.220.8
1974512   800-9 99510 7951.6-19.521.1
1975524   800-9 99510 7951.5-19.120.6
1976536   800-9 99510 7951.5-18.620.1
1977548   870-22 131  23 0011.6-40.442.0
19785601 000-27 724  28 7241.8-49.551.3
19795722 700-8 44311 1434.7-14.819.5
19805832 700-10 565  13 2654.6-18.122.7
19815952 700-11 368  14 0684.5-19.123.6
19826072 7000 56 512  9 2124.4010.715.1
19836182 6982 58 95311 6534.4       0.00314.518.9
19846302 6991 59 18211 8824.3       0.00114.618.9
19856432 7000 58 01210 7124.2012.516.7
19866572 7000 510 562  13 2624.1016.120.2
19876712 7000 511 676  14 3764.0017.421.4

1 Source: FAO
2 Source: FAO Fisheries Department FISHDAB
Excludes catches by Seagull Goldstores Ltd. No comprehensive catch assessment survey for inland waters. Data from 1979 estimated on basis of special study undertaken in 1979.

3 included in “Inland capture” if not specified.
4 - = data not available.
5 Vincke, 1989 (pers.comm.)
6 Exports are not exactly known, but are thought to be small.

4. STATE OF THE FISHERY

4.1 Yield

It is evident that the recorded catch is low compared with the empirically predicted state of the resource. The Gambia River can be divided into two main fisheries:

Two estimates of potential can be advanced. First, simply on the basis of the length of the river, one would expect to find at least 2 300 t of fish per year. The area is, however, largely estuarine and also has extensive upstream floodplains which, on the basis of 55 kg/ha (mean derived from other similar systems), would be expected to produce about 11 000 t/yr. These two estimates are disparate and, because of the lack of fundamental research work on the river, it is difficult to decide which corresponds best to the real situation. The catch levels of 1977–82 would indicate a higher level of catch than that predicted by a simple river length model.

Fig. 1

Fig. 1. MAP OF THE GAMBIA

Vincke (1989, pers.comm.) gives the following data for aquaculture production (1982–87) by species:

Species198219831984198519861987
Oreochromis niloticus02 t1 t000

4.2 Factors influencing yield

Factors which may influence yield in the future are plans to control the flood of the Gambia River, which would cut down on the amount of floodland available to the fish.

4.3 Future development possibilities

The recorded catch of inland fish in Gambia may rise in the next few years, due not so much to any actual increases in production as to improvements in statistical systems which will enable better estimates of catch.

5. KEY BIBLIOGRAPHY: None.

6. WATER BODIES DIRECTORY

GAMBIA RIVER
(International water)

Geographical data 
Source:Fouta Djallon (Guinea)
Altitude:1 100 m
Total length:1 120 km (last 480 km in Gambia; 200 km in Guinea)
Drainage area:77 000 km2
Countries traversed:Gambia, Guinea, Senegal
Discharges to:Atlantic Ocean at Bathurst, Gambia - 12° 23'N, 16° 20'W
Special features:in Gambia most of the banks are flooded during the rains, and the estimated area of waters at peak floods of 2 000 km2 covers about 40% of the area of Gambia. There is a small lake/lagoon on the northshore floodplain river Njakunda. The saline downstream reaches of the river are lined with mangroves and are generally estuarine in character.
 
Physical and chemical data
Temperature:about 20° C
pH:6.3

Fisheries data
No. of fish species: 81
Total annual catch and effort:

 YearTotal catch
(t)
No.of fishermenNo.of boats
19773 171--
19783 198--
19792 795--
19802 596--
19811 423564554
19823 508--

7. BIBLIOGRAPHY

Welcomme, 1979

GHANA

1. GEOGRAPHY AND CLIMATE (Welcomme, 1979)

Ghana (with a surface area of 238 539 km2) is divided into three main regions. There is a narrow sandy coastal plain, behind which there is a range of low but abrupt hills; to the north there are low-lying plains. The southwestern part of the country is densely forested, and to the north are bush savanna and grasslands.

The coastal belt is warm, fairly dry to the east, but becoming more humid to the west. The forest zone is very humid but the rest of the country becomes progressively more arid northward. In the south there are two rainy seasons (March-June and September-November), separated by dry periods. In the north the two wet seasons tend to be closer together and merge into one (May-October).

Ghana is almost entirely agricultural, except for some industries which are located mostly at Tema. The Akosombo Dam was built mostly to provide power for industrialization, especially the Volta Aluminium Company (Valco) based at Tema, which consumes 60% of this power. Ghana also supplies power to Togo and Benin. Forestry is also an important activity in the southwest of the country.

2. HYDROGRAPHY (after Welcomme, 1979, and Balarin, 1988)

2.1 Lakes

The only natural freshwater lake of any size in the country is Lake Bosumtwi, a crater lake situated in Ashanti Region. This supports some commercial fishing activity.

2.2 Rivers, Floodplains and Swamps

Ghana is extremely well watered and is drained principally by the Black, White and Red Volta Rivers and the Oti River, but several smaller water courses, including the Pra, Tano and Bia drain the forested southwestern areas (see Fig. 1, Table 1). Flooding on the lower Volta River is now controlled by the Akosombo Dam.

The hydrology of the Volta River is well documented by Nerguaye-Tetteh et al., (1984). The most important flow is from the Oti. Peak flows are between September and October, with an annual average of 1 230 m3/s. Examining past trends, it is noted that from 1936 to 1958 conditions altered fairly evenly between wet and dry years. However, from 1962 to 1971 the flow regime was relatively wet; then from 1972 to 1978 it became dry again, followed by two wet years. Thereafter 1981 to 1983 were the driest years of the series, emphasizing the effect of the Sahelian drought. In general, water quality is good for both irrigation and livestock uses.

Extensive marsh and swamp occur around the borders of most of the coastal lagoons but no quantified data is available.

2.3 Reservoirs

Ghana contains the largest man-made reservoir in Africa, the 8 482 km2 Volta Reservoir. The reservoir, which is backed up behind the Akosombo high dam, is over 400 km long and has drowned much of the lower courses of the various rivers of the Volta system. It is used as a water store to generate electricity, but the severe drought of 1981–83 drastically reduced the output.

Table 1. MAJOR RIVER SYSTEMS AND HYDROLOGICAL ZONES - GHANA

(Sources: Govt. of Ghana, 1966; Welcomme, 1972; Nerguaye-Tetteh et al., 1984)

Drainage Basin
1
Major River SystemsFlow Range
(Annual mean)
m3/S × 103
No. of Fish Species
NameLength
km
Catchment
km2 2
1Volta Basin 165 700  
   (149 600)(0.057) 
1aBlack Volta65035 1050.01–1.1096
    (0.135) 
1b.White Volta 45 8000.1–1.41 
   (72 900)(0.112) 
1c.Oti90016 2150.01–1.27 
1d.Volta 68 580(0.141)70
2.Bia2006 4700.1332
   (9 500)(0.08) 
3.Tano6251 4900.03–0.78 
   (16 000)(0.13) 
4.Ankobra 8 4600.11 
5.Pra44523 2000.03–0.92 
    (0.24) 
6.Ochi-Amissa 1 3700.05 
7.Ochi-Nakwa 1 5000.05 
8.Ayensu 1 7000.001–0.06 
9.Densu 2 550  
10.Subri-Amansuri 840  
11.Butre 460  
12.Kakum-Saruwi 980  
13.Todzie 1 8600.06 
14.Aka (Keta Lagoon) 1 720  
15.Minor Coastal Streams 6 150  
 Total 237 870  

1 Numbers refer to Figure 1.
2 Value in parentheses is total drainage area.

Fig. 1

Fig. 1. CLIMATIC ZONES AND MAJOR RIVER SYSTEMS (see Table 1)
(World Bank, 1985 and Govt. of Ghana, 1966)

Table 2. MORPHOLOGICAL DATA FOR MAJOR LAKES, RESERVOIRS AND LAGOONS
(Balarin, 1988)

Name
(date constructed)
Ref.DescriptionFishery potent.
t/yr
Fish species

Use*

Water temp
°C
Volume
103m3
Area
km2
e
Alt.
(m)
Mean depth
(m)
Volta (1966)a b  165.08 482  851950 00070f,p,i   27–32
Bosumtwia 49107 600  27.9
Weija (1974)c 35–57 14.1420   
Barekese (1970)c 6.4  80   
Tono (1975)d0.0918.6200 225   
Vea (1965)d0.024.0200 45   
Kpong (1981)  36.5    p,i 
Nasia         
Golinga         
Tanogo         
Subinia         
Akumandan         
Dawhenya  2.2  30   
Afife  5.5  70   
          
Lagoons         
Keta  330      4 000  27.7
Sakumoa 10    00.5–10120   
Songawa 18      220   
Unvoiyea 11.1  140   
Juen         
Sakumor-choko  23      290   
Mukwe  0.5      
Nakwa  6.5  80   
Nuyi  8      100   

* f = fishery; i = irrigation; p = power generation
Sources:
a Welcomme (1972)
b Czernin-Chudenitz (1971)
c Allen & Gaudet (1978)
d ICOUR (1985)
e Adumua-Bossman & Mensah (1980)

Fig. 2

Fig. 2. THE PRINCIPAL LAGOONS OF GHANA
(from M.A. Mensah, in Weigel, 1985)

Downstream from Volta Reservoir is the newly created Kpong Reservoir. Other smaller reservoirs are Vea and Tono, both in the Upper East Region; Weija and Dawhenya, located near Accra; and Barakese, near Kumasi.

Table 2 gives some morphological data for major reservoirs; Table 3 gives an estimate of the total number of reservoirs, from 1967 to 1982. FAO (1982) lists 300 reservoirs of 2.5 to 1 860 ha in Upper East and West alone, and 120 being planned.

Table 3. ESTIMATES OF NUMBERS OF RESERVOIRS - GHANA
(Balarin, 1988)

RegionLocation1967196919741982
Upper EastBawku-Bolgatanga-Nawrongo150130 169  
NorthernLawra-Wa-Damango-Tamale  17  90 90
VoltaHo  5151

Sources: FD, 1975; Denyoh, 1967; USAID, 1969

2.4 Coastal Lagoons (see Fig. 2)

There are about 50 brackishwater lagoons situated along the coast of Ghana, with a total surface area of some 400 km2 (FAO/IFAD, 1981). These are described in detail by Mensah (1979). The largest of these is the Keta Lagoon, situated around the delta of the Volta River. The nature of this lagoon has changed considerably since the closure of the Akosombo Dam; the former periodic flushes of freshwater do not now occur, and the lagoon has become more saline as a consequence.

The salinity and temperature of the lagoons vary with opening to the sea and flooding of inflowing rivers; open lagoons generally tend to be more productive. Table 2 gives the surface area and fishery potential of the major lagoons.

2.5 Aquaculture

A recent survey published by CSIR (1984) estimates that 1 135–1 400 ponds exist, covering an area of 77.8 ha (i.e., 555–685 m2 average size), of which 70% are household units and 30% community ponds (Table 4).

Table 4. FISH POND DISTRIBUTION IN GHANA, 1982/83
(Abstracted from CSIR, 1986)

RegionArea
(ha)
Household
(%)
Community
(%)
Estimated Total No.
Upper East3.5100    00–10
Upper West   -
Northern3.6901011–30
Brong-Ahafo0.8505011–30
Ashanti9.92080151–170
Volta5.4337770–150
Western3.6851570–150
Central-773311–30
Eastern9.3901011–30
Greater Accra41.7  8515>800
Total77.8  70301 135–1 400

3. FISHERY PRODUCTION/POTENTIAL

3.1 Fish production and per caput supply

Table 5. FISH PRODUCTION AND PER CAPUT SUPPLY - Ghana, 1970–1987

 Nominal Production
(including exports)
(t) 2
Nominal Consumer Supply
(including exports)
(kg/person)
YearPopulation
'000 1
Inland captureAquaculture
3
Marine capture
4
TotalInland captureAquaculture
3
Marine captureTotal
1970  8 61430 000- 5141 500171 5003.5-16.419.9
1971  8 83940 000-176 400216 4004.5-20.024.5
1972  9 07032 000-249 200281 2003.5-27.531.0
1973  9 30741 300-182 400223 7004.4-19.624.0
1974  9 55137 300-182 213219 5133.9-19.123.0
1975  9 80041 945-212 570254 5154.3-21.726.0
197610 12941 945-195 752237 6974.1-19.323.4
197710 46940 704-226 198266 9023.9-21.625.5
197810 82136 261-222 084258 3453.3-20.523.8
197911 18439 368-197 166236 5343.5-17.621.1
198011 56040 000-191 891231 8913.5-16.620.1
198111 94040 000-199 894239 8943.4-16.720.1
198212 33241 873127 6200 680242 6803.40.0116.319.7
198312 73742 675325 6207 898250 8983.40.0316.319.7
198413 15640 550450 6228 518269 5183.10.0317.420.5
198513 58842 643357 6232 934275 9343.10.0317.120.3
198614 05252 679321 6267 713320 7133.70.0219.122.8
198714 53253 614386 6317 817371 8173.70.0321.925.6

1 Source: FAO
2 Source: FAO Fisheries Department FISHDAB
3 included in “Inland capture” if not specified
4 Includes landings of Ghananian flag vessels in the Gambia.
Catch by Ghanaian artisanal fishermen considerably greater than fish landed in Ghana, as Ghanaian fishermen operate from beaches along the West African coast, notably in Liberia, Gambia, Togo, Benin and Sierra Leone. Catches by these canoes included in totals for the respective countries.
From 1980 to 1983, marine exports were as follows: 1980: 29 600 t; 1981: 34 300 t; 1982: 32 100 t; 1983: 22 390 t.

5 - = data not available
6 Vincke, 1989, pers. comm.

3.2 Inland catch range and potential yield

Table 6. INLAND CATCH RANGE AND POTENTIAL YIELD

Water bodyPeriodAnnual catch range (t)Potential annual yield (t)
Volta River1960's4 000 1-
Volta Reservoir1970–7935 900–41 94539 000 2
   50 000 3
Sakumo-Tema Lagoon197115-
No information available for  
Lake Bosumtwi;
Rivers Bia, Black Vota, Oti, Pra, Red Volta, Tano, White Volta;
Reservoirs Barekese, Dawhenya, Kpong, Tono, Weija;
Lagoons Avu, Keta, Mukwe, Sakumo-Accra, Songaw, Unvaiye.
Total Rivers -  4 000 4
 Total Lagoons -15 000 5

1 River clam catch only
2 Welcomme, 1972
3 Denyoh (pers.comm.)
4 Balarin, 1988
5 FAO, 1976

Total annual yield:1980–1985: 40 000 t (see Table 5)
1986–1987: 53 000 t (see Table 5)
Potential annual yield:40 000–69 000 t (Balarin, 1988)
65 000 t (Denyoh, pers.comm.)

4. STATE OF THE FISHERY (adapted from Welcomme, 1979; and Balarin, 1988)

4.1 Yield

The main feature of the inland fishery is the Volta Lake, which has 920 fishing villages and 12 500 small canoes; it produces an estimated 40 000 t/yr (FAO, 1978a), employing about 20 000 fishermen (FAO, 1981).

The catch from the Volta Reservoir reached a peak of 61 783 t in 1969 after the reservoir filled in 1964. Subsequently there has been a decline to 36 000–42 000 t, which seems to be the stabilization level. Catch from other inland waters and the coastal lagoons may be estimated at some 7 000 t.

Denyoh (1985) gives the most recent documented statistics of aquaculture production. Government and private fish ponds total 120 ha and produce 325 t annually (2.7 t/ha/yr average yield). In addition, there are 15 ha of Fisheries Department ponds to provide fingerlings for dam stocking. Table 7 gives the production by species from 1982 to 1987.

Table 7. AQUACULTURE PRODUCTION, BY SPECIES (t)

Species198219831984198519861987
Oreochromis, Sarotherodon spp.25  82-  64--
Clarias gariepinus13  50  60  36  96116
Oreochromis niloticus89193390257225270
Total127  325450357321386

Source: Vincke, 1989, pers.comm.

Pautzke and Crowther (1968) describe a 4 000 t/yr freshwater clam fishery in the lower Volta River below Akuse: Egeria radiata were harvested as young clams in December-January and stocked further upstream at 1 500/m2 to be harvested when grown in May-June. The fate of this activity due to the damming is not known.

4.2 Factors influencing yield

The yield of Volta Reservoir has followed the classic pattern of peak and stabilization. The dam has undoubtedly affected the catch downstream and also the fisheries of some coastal lagoons, especially Keta Lagoon. There has been some effort in recent years to introduce fishculture in the coastal lagoon areas, as this is considered to have good potential for high fish yield in the inland waters. The lagoons are well adapted to brackishwater ponds and species adapted thereto; Mugil spp., tilapias and shrimps (Penaeus spp.), are indigenous in the coastal lagoons.

4.3 Future development possibilities

With a maximum sustainable yield of 50 000 t/yr (Denyoh, pers. comm.), the Volta Reservoir will continue to provide large amounts of fish, and the catch from other water bodies (MSY 15 000 t/yr estimated by Denyoh) is expected to rise. However, FAO/IFAD (1981) considers that inland resources are currently used at a maximum and that there is little further scope for development, but no limits are given.

The recent awareness of fish production through aquaculture, which has resulted in the construction of a good number of fish ponds on commercial scale as well as a number of household ponds all over the country, will be a major breakthrough in Ghana's fish production in inland waters.

5. KEY BIBLIOGRAPHY

Balarin, 1988
Weigel, 1985 (Lagoons)

6. WATER BODIES DIRECTORY

Lakes   
Bosumtwi   
    
Rivers   
BiaOti/PendjariRed VoltaVolta
Black VoltaPraTanoWhite Volta
    
Reservoirs   
BarekeseKpongVeaWeija
DawhenyaTonoVolta 
    
Lagoons   
Aby-Tendo-Ehy ComplexBrenuKetaNakwa
AmansuriChemuKorleOyibi
AmisaElminaKpeshieSakumo-Accra
AngawFosuLaiwiSakumo-Tema
AvuGaoMukweSongaw
BenyaJuenMuniUnvaiye

LAKE BOSUMTWI

Geographical data
Location:Ghana - 6° 30'N; 1° 25'W
Altitude:1 070 m
Surface area:49 km2
Depth:81 m (max)
Max. length:8 km
Max. width:8 km
Shoreline:26.8 km
Catchment area:108 km2
 
Physical and chemical data
Surface temperature: 27.9° C

BIA RIVER
(International water)

Geographical data
Source:Ghana
Altitude:306 m
Total length:300 km (200 km within Ghana)
Drainage area:9 500 km2 (6 500 km2 within Ghana)
Countries traversed: Ghana, Côte d'Ivoire
Discharges to:Abi Lagoon, Côte d'Ivoire - 5°N; 3° W
Volume of discharge at mouth: 83 m3/sec
Special features: Ayame dam and Reservoir
 
Physical and chemical data
pH:6.5–7.5
 
Fisheries data
No. of fish species:32 (Daget & Iltis, 1965)

BLACK VOLTA RIVER
(International water)

Geographical data
Source:Burkina Faso (70 km southwest of Bazo)
Altitude:300 m asl
Total length:1 300 km (650 km in Burkina Faso)
Drainage area:149 600 km2
Countries traversed:Burkina Faso, Côte d'Ivoire, Ghana
Major tributaries:Bougouriba, Tui
Discharges to:Volta Reservoir
Volume of discharge at mouth: 243 m3/sec (mean annual)
Flood regime:unimodal flood peak in September-October
Special features:the Black Volta has several floodplains fringing its upper course in Burkina Faso where some 75 000 ha are liable to flooding each year. A particular feature of this is the Sourou Depression, with 25 000 ha of flooded lowland, and the “Mare aux Hippopotames” (1 200 ha).
  
Physical and chemical data
Conductivity:K20 41–124 μ S/cm (Welcomme, 1972)
pH:6.5–7.3 (Welcomme, 1972)
 6.4 (Blanc and Daget, 1957)
Ionic composition: (Blanc and Daget, 1957)
  mg/l
Na    3.9
 K  0.25
 Ca   380*
 Mg11.86
 CO2  11.3
 Cl  17.5
 SO3     72*
 SiO2125.5

* Ca and SO3 figures seem aberrently high and should be taken with care.

Fisheries data
No. of fish species: 96 (Daget and Iltis, 1965)

OTI/PENDJARI RIVER
(International water)

Geographical data
Source:Atakora Mountains of Benin
Altitude:640 m asl
Total length:900 km
Drainage area:72 900 km2
Countries traversed: Benin, Burkina Faso, Togo, Ghana
Discharges to:Volta Reservoir
Volume of discharge at mouth:500 m3/sec
 
Physical and chemical data (after Blanc & Daget, 1957)
pH:6.4–6.7
Ionic composition:mg/l
Na  3.2
 K0.22
 Ca 300*
 Mg11.6
 CO2   39
 Cl23.4
 SO3   96*
 SiO2 132

* Ca and SO3 figures seem aberrently high and should be taken with care.

PRA RIVER

Geographical data
Source:Ghana
Altitude:550 m
Total length:445 km
Drainage area:22 710 km2
Discharges to:Atlantic Ocean - 5° 1'N; 2° 22'E
Volume of discharge at mouth: 238 m3/sec
 
Physical and chemical data (Welcomme, 1972)
pH:6.9–7.5
Conductivity:K20 140 μ S/cm

RED VOLTA RIVER
(International water)

Geographical data
Source:Burkina Faso (20 km west of Titao)
Altitude:315 m asl
Total length:330 km (60 km in Ghana)
Countries traversed: Burkina Faso, Ghana
Discharges to:White Volta near Gambaga in Ghana
Flood regime:dry from November to June
 
Physical and chemical data (after Blanc & Daget, 1957)
pH6.5
Ionic composition:mg/l
Na  8.9
 K2.86
 Ca 220*
 Mg13.4
 CO271.7
 Cl17.5
 SO3 120*
 SiO2 148

* Ca and SO3 figures seem aberrently high and should be taken with care.

TANO RIVER
(International water)

Geographical data(all data from Welcomme, 1972)
Source:Ghana
Altitude:430 m
Total length:625 km
Drainage area:16 000 km2
Countries traversed: Ghana, Côte d'Ivoire
Discharges to:Abi Lagoon
Volume of discharge:129 m3/sec
 
Physical and chemical data
pH:6.9–9.0

VOLTA RIVER

Geographical data
Source:Ghana, Volta Reservoir (discharge through Akosombo Dam). Previously began at now-flooded-junction of White Volta and Black Volta Rivers.
Altitude:14.3 m asl (Akosombo taihace)
Total length:86 km (from Kpong dam to sea)
Drainage area:390 000 km2
Surface area:44 km2
Countries traversed:Ghana
Discharges to:Atlantic Ocean - 5° 46'N; 0° 40'E
Volume of discharge at mouth: 1 150 m3/sec (highly regulated by Akosombo Dam)
Special features:Keta and Songaw Lagoon Complex near mouth. Upper reach now permanently flooded by Volta and Kpong Reservoirs.
  
Fisheries data(cited in Balarin, 1988)
No. of fish species:122
Total annual catch:4 000 t of the river clam Egeria radiata

WHITE VOLTA RIVER
(International water)

Geographical data
Source:Burkina Faso (35 north of Sakonice)
Altitude:298 m asl
Total length:660 km (255 km in Burkina Faso)
Drainage area:92 880 km2 (at Nawuni)
Countries traversed:Burkina Faso, Ghana
Major tributaries:Red Volta, Kulpawn, Nasia
Discharges to:Volta Reservoir
Volume of discharge at mouth: 240 m3/sec (mean annual at Nawuni)
Flood regime:unimodal peak in September, almost dry January-May
 
Physical and chemical data (Welcomme, 1985)
Conductivity:K20 119 μ S/cm
pH:7.6 (Blanc & Daget, 1957;
 7.2 (Welcomme, 1985)
Ionic composition: (after Blanc & Daget, 1957)
  mg/l
Na    8.9
 K  2.23
 Ca   280*
 Mg  12.4
 CO2     84
 Cl  17.5
 SO3   108*
 SiO2150.6

* Ca and SO3 figures seem aberrently high and should be taken with care.

Fisheries data
Total annual catch: 70 t in Burkina Faso (Welcomme, 1972)

BAREKESE RESERVOIR

Geographical data
Location:Ghana - 6°44'; 1° 42'W
Date closed:February 1970
Surface area:6.4 km2 at USL
Max. length:13 km
Max. width1.25 km
Major inflowing river: Ofin
Outflowing river: Ofin

DAWHENYA RESERVOIR

Geographical data
Location:Ghana - 5° 46'N; 0° 4'E
Data closed:1974
Surface area:0.48 km2 at USL
 
Physical and chemical data
Surface temperature:25.0–31.0° C
pH:7.2–8.0

KPONG RESERVOIR

Geographical data
Location:Ghana - 6° 9'N; 0° 5'E
Altitude:14.17 m asl
Surface area:36.16 km2
Dam height:18.29 m
Date closed:May 1981
Annual fluctuation in level: 0.61–1.52 m
Major inflowing river: Volta

TONO RESERVOIR

Geographical data
Location:Ghana
Surface area:18.60 km2

VEA RESERVOIR

Geographical data
Location:Ghana
Surface area:3.80 km2

VOLTA RESERVOIR

Geographical data (Welcomme, 1972)
Location:Ghana - 6° 15'–9° 00'N; 1° 00'W-0° 15'E (see Fig. 3)
Altitude:85 m
Surface area:8 270 km2
Depth:74 m (max); 19 m (mean)
Volume:165 km3
Max. length:400 km
Max. width:23.8 km
Shoreline:4 828 km
Annual fluctuation in level: 3–4 m
Major inflowing rivers: White Volta, Black Volta, Oti
Outflowing river:Volta
 
Physical and chemical data
Surface temperature: 27–32° C
Conductivity:K18 63–172 μ S/cm (Czernin-Chudenitz, 1971)
Dissolved solids:70 mg/l
pH:North lake: 6.8–7.4;
 South lake: 7.8–8.5
Ionic composition: (Entz, 1969)
              mg/l 
Na1.2–6.8 
 K1.5–6.0 
 Ca3.4–10.2 
 Mg2.4–7.1 
 HCO320–70 
 Cl1–4 
 SO4trace 
 SiO216–25 
 Fe0–0.26 
 P2O50.5 
 NO3-N0.02–1.00 
 (More detailed data are given in Entz, 1984)

Fisheries data
No. of fish species: 70 (Denyoh, 1969)
Main catches: tilapias (50%, overfished), Lates niloticus, Labeo sp., Alestes sp., Citharinus sp., Distichodus sp.
Total annual catch and effort:

 YearTotal catch
(t)
No.of fishermenNo.of boats
1964  3 437--
1965  8 449--
196622 161--
196740 682--
196850 960--
196961 783--
197039 133--
197139 03518 35812 074
197236 011--
197335 900--
197437 300--
197541 94520 61513 814
197640 704--
197738 262--
197837 261--
197939 368--

Potential annual yield:39 000 t (Welcomme, 1972)
 50 000 t (Denyoh, pers.comm.)
Specific references:Entz, 1984; Vanderpuye, 1984
Fig. 3

Fig. 3. LAKE VOLTA RESERVOIR
(Welcomme, 1972)

WEIJA RESERVOIR

Geographical data
Location:Ghana - 5°35'N; 0°22'W
Altitude:14.1 m at USL
Date closed:December 1974
Surface area:33.61 km2
Max. length:14 km
Max. width:2.2 km
Major inflowing river: Densu
Outflowing river:Densu

ABY-TENDO-EHY LAGOON COMPLEX
(International water)

Geographical data
Location:Côte d'Ivoire, Ghana - 5° 5'–23'N; 2° 51'-3° 21'W (Ghana has about 25 km of shoreline along the Tendo-Ehyportia but no actual lagoon surface area)
Surface area:410 km2
Depth:14.9 m (max); 5.0 m (mean)
Max. length:52 km
Max. width:30 km
Annual fluctuation in level: 0.3–0.5 m
Major inflowing rivers: Bia, Tano
Outflow:channel to Atlantic Ocean; also a short canal to Juen Lagoon in Ghana
  
Physical and chemical data:
Surface temperature: 24–30° C
 
Fisheries data
No. of fishermen:1 654 (year unspecified)
No. of boats:617 (year unspecified)
Total annual catch:570 t (mean for 1968–71 period)

AMANSURI LAGOON

Geographical data
Location:Ghana - 5° 1'N; 2° 35'W

AMISA LAGOON

Geographical data
Location:Ghana - 5° 12'N; 1° 1'W
Major inflowing river: Ochi
Outflow:canal to Atlantic Ocean

ANGAW LAGOON

Geographical data
Location:Ghana - 5° 48'N; 0° 47'E
Major inflowing river: Volta
Outflow:canal to Atlantic Ocean

AVU LAGOON

Geographical data
Location:Ghana - 5° 59'N; 0° 45'E
Surface area:46 km2
Max. length:11 km
Max. width:6 km
Major inflowing river: Todzie
Outflow:channels to Keta Lagoon

BENYA LAGOON

Geographical data 
Location:Ghana - 5° 05'N; 1° 21'W

BRENU LAGOON

Geographical data 
Location:Ghana - 5° 4'N; 1°26'W

CHEMU LAGOON

Geographical data 
Location:Ghana
Special features:heavily polluted

ELMINA LAGOON

Geographical data 
Location:Ghana

FOSU LAGOON

Geographical data 
Location:Ghana

GAO LAGOON

Geographical data 
Location:Ghana

JUEN LAGOON

Geographical data 
Location:Ghana - 5° 6'N; 2° 54'W
Outflow:connected by a short canal to Aby-Tendo-Ehy Lagoon Complex in Côte d'Ivoire

KETA LAGOON

Geographical data(see Fig. 4)
Location:Ghana - 5° 55'N; 0° 56'W
Surface area:330 km2
Max. length:29 km
Max. width:13 km
Major inflowing river:outflow from Avu Lagoon
Outflow:short channel to Atlantic Ocean
Catchment area:3 600 km2
 
Physical and chemical data
Surface temperature:27.7° C

Fig. 4

Fig. 4. THE KETA LAGOONS
(Weigel, 1985)

KORLE LAGOON

Geographical data 
Location:Ghana - 5° 32'N; 0° 13'W
Special features:heavily polluted

KPESHIE LAGOON

Geographical data 
Location:Ghana - 5° 33'N; 0° 10'W
 
Physical and chemical data
Salinity:to 72

LAIWI LAGOON

Geographical data 
Location:Ghana - 5° 42'N; 0° 4'E

MUKWE LAGOON

Geographical data 
Location:Ghana -5° 36'N; 0° 3'W
Surface area:0.04 km2
Depth:1.5 m (max)
Max. length:2 km
 
Physical and chemical data
Surface temperature:24-8-32.2° C
Salinity:10–70

MUNI LAGOON

Geographical data 
Location:Ghana - 5° 20'N; 0° 39'W

NAKWA LAGOON

Geographical data 
Location:Ghana - 5° 12'N; 0° 55'W

OYIBI LAGOON

Geographical data 
Location:Ghana - 5° 22'N; 0° 36'W

SAKUMO-ACCRA LAGOON

Geographical data 
Location:Ghana - 5° 32'N; 0° 17'W
Surface area:23.6 km2
Max. length:5 km
Max. width:0.14 km
Major inflowing river:Densu
Outflow:canal to Atlantic Ocean
 
Physical and chemical data
Salinity:<1–36.3

SAKUMO-TEMA LAGOON

Geographical data 
Location:Ghana - 5° 37'N; 0° 2'W
Surface area:1 km2
Depth:0.88 m (max); 0.50 (mean)
Max. length:4.42 km
Outflow:canal to Atlantic Ocean
 
Physical and chemical data
Surface temperature:18–34.3° C
Salinity:<1–50.5
 
Fisheries data
No. of fishermen:13 in 1971 (no boats)
Total annual catch:15 t in 1971

SONGAW LAGOON

Geographical data 
Location:Ghana - 5° 49'N; 0° 28'E
Surface area:18 km2
Max. length:20 km
Max. width:8 km
Major inflowing river:Volta

UNVAIYE LAGOON

Geographical data 
Location:Ghana
Surface area:11.1 km2

7. BIBLIOGRAPHY

Adumua-Bossman & Mensah, 1980
Allen & Gaudet, 1978
Balarin, 1988
Blanc & Daget, 1957
CSIR, 1986
Czernin-Chudenitz, 1971
Daget & Iltis, 1965
Denyoh, 1967; 1969; 1985
Entz, 1969; 1984
FAO, 1976; 1978a; 1981; 1982
FAO/IFAD, 1981
Fisheries Department, 1975
Government of Ghana, 1966
ICOUR, 1985
Mensah, 1979
Nerguaye-Tetteh et al., 1984
USAID, 1969
Vanderpuye, 1984
Weigel, 1985
Welcomme, 1972; 1979; 1985
World Bank, 1985


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