1. GEOGRAPHY AND CLIMATE
Namibia has a surface area of 823 290 km2. The country is largely semi-arid plateau and desert.
The climate is hot and dry with highly restricted rainfall. The economy is based on mineral extraction.
2. HYDROGRAPHY (see Fig. 1)
2.1 Lakes
There are no permanent freshwater lakes of any significant size. Non-permanent is Lake Liamberi, associated with Linyanti swamp.
2.2 Rivers, Floodplains and Swamps
Four large rivers flow along Namibia's borders: the Zambezi, Orange, Cunene and Okavango/Cubango.
2.3 Reservoirs
There are several impoundments: Hardop, Avis, Goreangab, Naute, Van Rhyn, Daan Viljoen, Ondangua, Okatana and Oshikango (the latter three are “saucer” dams located on the flat Ovambo tableland).
2.4 Coastal Lagoons
There is only one important lagoon at Sandwich Habour.
3. FISHERY PRODUCTION/POTENTIAL
3.1 Aquaculture
There is no aquaculture in Namibia (Vincke, 1989, pers.comm.)
3.2 Fish Production and per caput supply (see Table 1 on following page)
3.3 Inland catch range and potential yield
Total annual yield: No data available (except Table 1 and Lake Liamberi: 180 t in early 1980's).
Potential annual yield: No data available.
Table 1. FISH PRODUCTION AND PER CAPUT SUPPLY - Namibia, 1970–1987
Nominal Domestic Production (t) 2 | Nominal Consumer Supply (kg/person) 2 | ||||||||
Year | Population '000 1 | Inland capture | Aquaculture 3 | Marine capture | Total | Inland capture | Aquaculture 3 | Marine capture 4 | Total 4 |
1970 | 1 042 | - 4 | 20 000 | 20 000 | - 4 | ||||
1971 | 1 068 | - 4 | 18 600 | 18 600 | - 4 | ||||
1972 | 1 096 | - 4 | 30 000 | 30 000 | - 4 | ||||
1973 | 1 124 | - 4 | 709 700 | 709 700 | - 4 | ||||
1974 | 1 152 | 50 5 | 840 376 | 840 426 | 0.04 | ||||
1975 | 1 182 | 50 | 760 825 | 760 875 | 0.04 | ||||
1976 | 1 213 | 50 | 574 424 | 574 474 | 0.04 | ||||
1977 | 1 245 | 50 | 404 095 | 404 145 | 0.04 | ||||
1978 | 1 278 | 50 | 412 638 | 412 688 | 0.04 | ||||
1979 | 1 313 | 50 | 351 080 | 351 130 | 0.04 | ||||
1980 | 1 349 | 50 | 252 562 | 252 612 | 0.04 | ||||
1981 | 1 386 | 50 | 278 549 | 278 599 | 0.04 | ||||
1982 | 1 425 | 50 | 233 489 | 233 539 | 0.04 | ||||
1983 | 1 465 | 100 | 364 628 | 364 728 | 0.07 | ||||
1984 | 1 507 | 100 | 186 981 | 187 081 | 0.07 | ||||
1985 | 1 550 | 100 | 185 420 | 185 520 | 0.06 | ||||
1986 | 1 596 | 100 | 201 202 | 201 302 | 0.06 | ||||
1987 | 1 643 | 150 | 519 368 | 519 518 | 0.09 |
1 Source: FAO
2 Source: FAO Fisheries Department FISHDAB
Important note:
Inland capture: excluding export
Marine capture: export statistics not available.
The 1970–87 catch data for Namibia include most of the quantities caught by fishing craft flying the South African flag and landed in Lüderitz and Walvis Bay (Namibia). Most of these landings are utilized for reduction into fish meal, for export abroad and domestic use. No statistics are available to ascertain precisely what part of the marine capture is actually used for domestic consumption.
3 No aquaculture in Namibia
4 No data available
5 1974–1987 rough estimates for inland capture
4. STATE OF THE FISHERY
4.1 Yield
No statistical data available except for Lake Liamberi, but it seems likely that catches are only a small fraction of the potential.
4.2 Factors influencing yield
Low rainfall and also, undoubtedly, the unstable security situation.
4.3 Future development possibilities
Development of inland fisheries is likely, once national sovereignty and stable internal security have been achieved.
Fig. 1. RIVERS AND LAKES OF SOUTHERN AFRICA
(Welcomme, 1972)
5. KEY BIBLIOGRAPHY (none)
6. WATER BODIES DIRECTORY
Lake | |
Liamberi | |
Rivers | |
Cunene | Orange |
Okavango/Cubango | Zambezi |
Floodplain, Reservoir, Lagoon | |
Ovambo Floodplain, Linyanti Swamp | |
Hardap (Fish River) Reservoir | |
Sandwich Harbour Lagoon |
LAKE LIAMBERI/LINYANTI SWAMP
(International water)
Geographical data (see Fig. 1) | |
Location: | Botswana, Namibia -18°S; 24°20'E |
Surface area: | 101 km2 (non-drought periods) (NORAD, 1985). Surface area very variable depending on annual flood inflow volume in any particular year; may dry out. Very little of its surface area lies in Botswana. |
Inflowing river: | Linyanti/Chobe |
Outflowing river: | Linyanti/Chobe |
Fisheries data | |
No. of fish species: | 43 (NORAD, 1985) |
Total annual catch: | - about 800 t in the 1960's and early 1970's, most of it marketed in Zambia and Zimbabwe; - no production in the late 1970's; - about 180 t in the early 1980's (NORAD, 1985) |
Potential annual yield: | |
For 101 km2 open water: 250 t (25 kg/ha/yr: NORAD, 1985) |
CUNENE RIVER
(International water)
Geographical data | |
Source: | Central Angola (Bie Plateau) |
Altitude: | 1 800 m asl |
Total length: | 975 km |
Drainage area: | 83 000 km2 |
Countries traversed: | Angola, Namibia |
Major tributaries: | Calonga |
Discharges to: | Atlantic Ocean - 17° 15'S; 11° 46'E |
Volume of discharge at mouth: 6.77 km3/yr | |
Special features: | In Angola, the Cunene is impounded at Matala (20-m-high dam), Kuene and Gove (58-m-high dam, 2 436 km3 storage volume), and on the Calonga tributary north of Cassinga. |
OKAVANGO/CUBANGO RIVER
(International water)
Geographical data (Welcomme, 1972) | |
Source: | Bie Plateau, Angola |
Altitude: | 2 560 m asl |
Countries traversed: | Angola, Botswana, Namibia |
Major tributaries: | Cuito |
Discharges to: | The mouth of the Okavango splits into three main arms to form an internal delta which discharges into the Okavango Swamps. A further branch, the Thamalkane River, is connected to Lake Dow. A reversible and periodic connection exists between the Okavango and the Kwando/Cuando and Zambezi system. During the floods the Okavango sends surplus water to the Kwando/Cuando (or Chobe) River which, in turn, joins the Zambezi. If the Zambezi floods arise early, however, the process may be reversed. |
Volume of discharge at mouth: 254 m3/sec |
ORANGE RIVER
(International water)
Geographical data (Welcomme, 1972) | |
Source: | Lesotho, Drakensberg Mountains |
Altitude: | 3 300 m |
Total length: | 2 160 km |
Drainage area: | 640 000 km2 |
Countries traversed: | Lesotho, Namibia (north shoreline only), South Africa |
Major tributaries: | Vaal River (1 200 km) |
Discharges to: | South Atlantic |
Flood regime: | Floods between November and March |
Special features: | Aughrabies Falls |
Physical and chemical data | |
Conductivity: | K25 159 μ S/cm (mean) (Keulder, 1970) |
pH: | 7.7 |
ZAMBEZI RIVER
(International water)
Geographical data (Welcomme, 1972) (See map under “Mozambique Country” entry) | |
Source: | northwest Zambia and eastern Angola |
Altitude: | 1 600 m |
Total length: | 2 574 km (120 km of shoreline along the Caprivi Strip belongs to Namibia) |
Drainage area: | 1 300 000 km2 |
Countries traversed: | Angola, Mozambique, Zambia, Botswana, Namibia, Zimbabwe |
Major tributaries: | Cuando, Kafue, Luangwa, Shire. The Zambezi system also communicates with the Okavango system via the Chobe River. |
Discharges to: | Indian Ocean - 18°47'S; 36°E |
Volume of discharge at mouth: 7 070 km3/sec | |
Flood regime: | December to July, maximum in March |
Special features: | Barotse floodplain (700–9 000 km2), Kafue flats (200–7 000 km2), Lukanga swamps (3 000–8 000 km2), Kariba and Cahora Bassa dams/reservoirs. |
Physical and chemical data above Lake Kariba (Coche, 1968)
Flood | Low water | |||
Temperature: | 30° C | 17° C | ||
pH: | - | 7.4 | ||
Conductivity: | K20: | 50 μ S/cm | 96 μ S/cm | |
Total alkalinity: | 20 mg/l | 44 mg/l | ||
Total hardness: | 17.9 mg/l | 38.1 mg/l | ||
Ionic composition: | mg/l | mg/l | ||
Na | 1.70 | 3.26 | ||
K | - | 0.88 | ||
Ca | 4.93 | - | ||
Mg | 1.47 | 3.86 | ||
NO2-N | 0.00376 | 0.00024 | ||
NO3-N | 0.0047 | 0.0158 | ||
PO4-P | 0.0295 | 0.0078 |
Fisheries data
No. of fish species: Upper Zambezi: 49; Middle Zambezi: 50 (Jubb, 1961)
OVAMBO FLOODPLAIN
(International water)
Geographical data | |
Location: | Angola, Namibia - 16° –18° S; 14° 50' –16° E |
Surface area: | 23 000 km2 (15 000 km2 in Angola; 8 000 km2 in Namibia) |
Major inflowing river: | Cunene |
Outflowing river: | overspill and seepage to Etosha Pan. |
HARDAP (= FISH RIVER) RESERVOIR
Geographical data | |
Location: | Namibia - 24° 30'S; 17° 50'E |
Surface area: | 42.0 km2 |
Max. length: | 15 km |
Max. width: | 4 km |
Major inflowing river: | Fish |
Outflowing river: | Fish |
SANDWICH HARBOUR LAGOON
Geographical data | |
Location: | Namibia - 23° 22'S; 14° 29'E |
Surface area: | 22.1 km2 |
Max. length: | 10.5 km |
Max. width: | 3 km |
7. BIBLIOGRAPHY
Coche, 1968
Jubb, 1961
Keulder, 1970
NORAD, 1985
Welcomme, 1972
1. GEOGRAPHY AND CLIMATE
Reunion (surface area of 2 500 km2) is a mountainous island of volcanic origin. Coastal areas are forested. There are numerous torrential rivers. Maximum elevation is 3 069 m asl. The climate is tropical, but varies with altitude. Cyclones occur. The economy is based on agriculture, mainly sugar and flower oil.
2. HYDROGRAPHY
2.1 Lakes
There are no natural lakes of significant size.
2.2 Rivers, Floodplains and Swamps
There are numerous short torrential mountainous rivers.
2.3 Reservoirs
There are no large impoundments.
2.4 Coastal Lagoons
There are no lagoons.
3. FISHERY PRODUCTION/POTENTIAL
3.1 Aquaculture
Inland and marine aquaculture are practised. (See Table 1)
Table 1. AQUACULTURE PRODUCTION BY SPECIES (t)
Species | 1985* | 1986 | 1987 | |
Inland aquaculture | ||||
Salmo gairdneri | 12 | 14 | 15 | |
Macrobrachium rosenbergii | 4 | 6 | 7 | |
Marine aquaculture | ||||
Marine fishes | 1 | 3 | 5 | |
Chelonia mydas | 30 | 50 | - | |
Total | 47 | 73 | 27 |
Source: Vincke, 1989 (pers.comm.)
* No data available for earlier years
3.2 Fish production and per caput supply (See Table 2)
Table 2. FISH PRODUCTION AND PER CAPUT SUPPLY - Reunion, 1970–1987
Nominal Domestic Production (including exports) (t) 2 | Nominal Consumer Supply (including exports) (kg/person) | ||||||||
Year | Population '000 1 | No inland capture | Aquaculture 3 | Marine capture 5 | Total | No inland capture | Aquaculture 3 | Marine capture 5 | Total |
1970 | 441 | - 4 | 1 700 | 1 700 | - | 3.8 | 3.8 | ||
1971 | 449 | - | 2 200 | 2 200 | - | 4.9 | 4.9 | ||
1972 | 457 | - | 2 200 | 2 200 | - | 4.8 | 4.8 | ||
1973 | 465 | - | 2 500 | 2 500 | - | 5.4 | 5.4 | ||
1974 | 474 | - | 2 677 | 2 677 | - | 5.6 | 5.6 | ||
1975 | 482 | - | 2 213 | 2 213 | - | 4.6 | 4.6 | ||
1976 | 487 | - | 2 092 | 2 092 | - | 4.3 | 4.3 | ||
1977 | 493 | - | 779 | 779 | - | 1.6 | 1.6 | ||
1978 | 499 | - | 2 007 | 2 007 | - | 4.0 | 4.0 | ||
1979 | 504 | - | 2 482 | 2 482 | - | 4.9 | 4.9 | ||
1980 | 510 | - | 2 120 | 2 120 | - | 4.1 | 4.1 | ||
1981 | 514 | - | 3 573 | 3 573 | - | 6.9 | 6.9 | ||
1982 | 518 | - | 3 464 | 3 464 | - | 6.7 | 6.7 | ||
1983 | 522 | - | 3 025 | 3 025 | - | 5.8 | 5.8 | ||
1984 | 527 | - | 2 732 | 2 732 | - | 5.2 | 5.2 | ||
1985 | 531 | 16 6 | 2 625 | 2 641 | 0.03 | 4.9 | 4.9 | ||
1986 | 539 | 20 6 | 2 044 | 2 064 | 0.04 | 3.8 | 3.8 | ||
1987 | 547 | 22 6 | 1 521 | 1 543 | 0.04 | 2.8 | 2.8 |
1 Source: FAO
2 Source: FAO Fisheries Department FISHDAB
3 Inland aquaculture only
4 - = data not available
5 Marine exports were as follows: 1980: 114 t; 1981: 569 t; 1982: 894 t; 1983: 1 308 t.
6 Vincke, 1989 (pers.comm.)
3.3 Inland catch range and potential yield
No data available for annual catch or potential yield for the main rivers: Bras de la Plaine, Langevin, Marsouins, Mat and Roches.
Total annual yield: Inland catch: 0 t; Inland aquaculture: 22 t (in 1987) (Vincke, 1989, pers.comm.).
4. STATE OF THE FISHERY
4.1 Yield
Capture fisheries are probably restricted to angling, but no catch data is available. There is some marine turtle and fish farming, as well as rainbow trout and Macrobrachium culturing. Production by species is given in Table 1.
4.2 Factors influencing yield
Generally, a lack of large surface water reserves. The high potential of marine fisheries does not encourage professional inland fisheries.
4.3 Future development possibilities
Undoubtedly some aquaculture development is possible; tilapia, trout and prawns have already been introduced to the island. Tilapia species in particular now occur in all river basins. The prospect for capture fisheries are, however, minimal.
5. KEY BIBLIOGRAPHY (none)
6. WATER BODIES DIRECTORY
Rivers | |
Bras de la Plaine | Mat |
Langevin | Roches |
Marsouins |
BRAS DE LA PLAINE RIVER
Geographical data | |
Drainage area: | 83 km2 |
Countries traversed: | Reunion |
Discharges to: | Indian Ocean |
Volume of discharge at mouth: 6.09 m3/sec (mean annual) | |
Flood regime: | peak discharge in January (7.38 m3/sec, monthly mean) |
LANGEVIN RIVER
Geographical data | |
Drainage area: | 36 km2 |
Countries traversed: | Reunion |
Discharges to: | Indian Ocean |
Volume of discharge at mouth: 2.46 m3/sec (mean annual) | |
Flood regime: | peak discharge in January (3.62 m3/sec, monthly mean) |
MARSOUINS RIVER
Geographical data | |
Drainage area: | 27.5 km2 |
Countries traversed: | Reunion |
Discharges to: | Indian Ocean |
Volume of discharge at mouth: 5.29 m3/sec (mean annual) | |
Flood regime: | peak discharge in March (11.5 m3/sec, monthly mean) |
MAT RIVER
Geographical data | |
Drainage area: | 145 km2 |
Countries traversed: | Reunion |
Discharges to: | Indian Ocean |
Volume of discharge at mouth: 9.42 m3/sec (mean annual) | |
Flood regime: | peak discharge in March (14.7 m3/sec, monthly mean) |
ROCHES RIVER
Geographical data | |
Drainage area: | 24.4 km2 |
Countries traversed: | Reunion |
Discharges to: | Indian Ocean |
Volume of discharge at mouth: 4.18 m3/sec (mean annual) | |
Flood regime: | peak discharge in March (11.8 m3/sec, monthly mean) |
1. GEOGRAPHY AND CLIMATE (Welcomme, 1979a)
Rwanda has a surface area of 24 950 km2 and consists mainly of grassy uplands which form part of the watershed between the Zaire and Nile River systems. It slopes from a range of high volcanoes in the northwest to savanna plains in the east. To the west the hills descend abruptly into Lake Kivu.
The high elevation makes for a temperate climate and frost may even occur in the high mountains. There is a short dry season in January with the major rainy season occurring from February to May. The main dry season lasts from May to September and the short rains from September to December. The rainfall is far heavier on the mountainous areas to the north and northwest than on the eastern savannas.
The population of Rwanda is entirely rural with small holdings dispersed throughout most of the country. Cattle herding is also very important although limited to the highlands because of heavy Tsetse infestations in the plains. There is one extensive national park along the lower portion of the Kagera River which contains many of the more important lowland lakes.
2. HYDROGRAPHY (see Fig. 1)
2.1 Lakes
Rwandan lakes fall into four main groups and into two main river basins:
Lake Kivu, Zaire River Basin - very deep and rich in nutrients;
High altitude lakes in the north (i.e. Lakes Luhondo and Bulera, the latter being associated with the Rugezi Swamps), Nile River Basin. These two lakes are cold, deep and rather infertile;
Upper Akagera* Lakes Complex (i.e. Lakes Birira, Cyohoha South, Gaharwa, Gashanga, Kidogo, Kirimbi, Mirayi, Mugesera, Muhazi, Murago, Rugwero, Sake), Nile River Basin. Mean altitude: 1 360 m (except Muhazi; 1 450 m). These lakes are warm, shallow and fertile. They are interspaced among the flooded papyrus plain of the Akanyaru and the Nyabarongo Valleys. The combined surface area in Rwanda is 166.5 km2;
Lower Akagera Lakes Complex (i.e., Lakes Chuju, Hago, Ihema, Iwapibali (=Rwakibale), Kishanja, Kivumba, Mihindi, Nasho, Ngerenke, Muhari, Rwampanga, Rwanyakizinga, Rwehikama), Nile River Basin. Mean altitude: 1 200 m. These are warm, shallow and fertile. They are spread over the lateral floodplain of the Akagera River below the Rusumo Falls. The combined surface area is 178.4 km2.
2.2 Rivers, Floodplains and Swamps
The country is dominated by the Akanyaru-Nyabarongo-Akagera River, which drains the majority of the country. The river is encased in narrow valleys for much of its upper course, but forms broad papyrus-filled swamps in its middle reaches. In its lower course, below the Rusumo Falls, it expands over large areas of savanna into a swamp mostly included in the Akagera National Park. The combined surface area of the Akagera swamps is about 1 000 km2 in Rwanda. A higher altitude swamp occurs in the north of the country: Rugezi Swamp, 80 km2, tributary of Lake Bulera. One other short but important river is the Ruzizi, which flows out of Lake Kivu toward Lake Tanganyika.
2.3 Reservoirs
Two reservoirs have been built, but are not used for fish production: Shyogwe reservoir near Gitarama (8.5 ha), drinking water reserve; and Nyabisundu reservoir near Bukare (7 ha), irrigation water reserve (Reizer, 1975).
2.4 Coastal Lagoons: None; Rwanda is landlocked.
3. FISHERY PRODUCTION/POTENTIAL
3.1 Aquaculture
In the late 1950's total pond area was circa 450 ha. There were 2 662 ponds in 1978 with a combined area of 77.64 ha, an estimated production of 18 891 kg and an average yield of 243 fish/ha/yr. (Source: Ministère de l'Agriculture et de l'Elevage, Annual Report, 1978).
3.2 Fish production and per caput supply
Table 1. FISH PRODUCTION AND PER CAPUT SUPPLY - Rwanda, 1970–1987
Nominal Domestic Production (excluding exports) (t) 2 | Nominal Consumer Supply (excluding imports and exports (kg/person) | ||||||
Year | Population '000 1 | Inland capture | Aquaculture 2 3 | Total 2 | Inland capture | Aquaculture 3 | Total |
1970 | 3 718 | 1 500 | - 4 | 1 500 | 0.4 | - | 0.4 |
1971 | 3 838 | 1 600 | - | 1 600 | 0.4 | - | 0.4 |
1972 | 3 963 | 300 | - | 300 | 0.07 | - | 0.07 |
1973 | 4 091 | 800 | - | 800 | 0.2 | - | 0.2 |
1974 | 4 223 | 1 368 | - | 1 368 | 0.3 | - | 0.3 |
1975 | 4 360 | 1 198 | - | 1 198 | 0.3 | - | 0.3 |
1976 | 4 504 | 1 008 | - | 1 008 | 0.2 | - | 0.2 |
1977 | 4 654 | 1 325 | - | 1 325 | 0.3 | - | 0.3 |
1978 | 4 811 | 696 | 19 5 | 715 | 0.1 | 0.004 | 0.1 |
1979 | 4 974 | 954 | - | 954 | 0.2 | - | 0.2 |
1980 | 5 144 | 1 181 | 19 | 1 200 | 0.2 | 0.004 | 0.2 |
1981 | 5 317 | 955 | - | 955 | 0.2 | - | 0.2 |
1982 | 5 496 | 1 210 | - | 1 210 | 0.2 | - | 0.2 |
1983 | 5 681 | 1 175 | 37 | 1 212 | 0.2 | 0.006 | 0.2 |
1984 | 5 872 | 744 | 42 | 786 7 | 0.1 | 0.007 | 0.1 |
1985 | 6 070 | 851 | 55 | 906 | 0.1 | 0.009 | 0.1 |
1986 | 6 277 | 1 420 | 65 | 1 485 6 | 0.2 | 0.010 | 0.2 |
1987 | 6 491 | 1 630 | - | 1 630 | 0.2 | - | 0.2 |
1 Source: FAO
2 Source: FAO Fisheries Department FISHDAB; see other sources data (bibliography) item 3.3.
3 included in “Inland capture” if not specified
4 - = data not available
5 Source: Ministère de l'Agriculture et de l'Elevage, 1978
6 Giudicelli et al., 1987: 1 800 t
7 Ministère de l'Agriculture et de l'Elevage, 1985: 1 256 t in 1984
Fig. 1. RWANDA, HYDROGRAPHIC NETWORK
(adapted from Mahy, 1977)
3.3 Inland catch range and potential yield
Table 2.
Water body | Period | Annual catch range (t) | Potential annual yield (t) | |
Lake Kivu | 1987 | 1 500–2 000 | 945–5 500 | |
High altitude lakes | 1975 | 100 1 | 200 1 | |
Bilinga | - | - | - | |
Bulera | - | - | 50 | |
Karago | - | - | - | |
Luhondo | 1974 | 50–100 | 50 | |
Rugezi Swamp | - | - | 10–120 | |
Total | (100) | (110–220) | ||
Upper Akagera Lakes | 1975 | 1 200 1 | 1 300 1 | |
Birira | 1975 | 70 | 21–67 | |
Cyohoha South | 1975 | 40 | 70–225 | |
Gaharwa | 1975 | 10 | 9–29 | |
Gashanga | 1975 | 30 | 9–29 | |
Kidogo | 1975 | 40 | 9–28 | |
Kirimbi | 1975 | 20 | 14–42 | |
Mirayi | 1975 | 20 | 9–29 | |
Mugesera | 1975 | 300 | 156–490 | |
Muhazi | 1986 | 40 | 40–200 | |
Murago | 1975 | 10 | 9–27 | |
Rugwero | 1975 | 200 | 80–90 | |
Sake | 1975 | 180 | 178 | |
Total | (960–1 200) | (774–1 594) | ||
Lower Akagera Lakes | 1975 | 650 1 2 | 2 300 1 | |
*Chuju | - | - | 1–2.5 | |
*Hago | 1975 | 90 | 64–210 | |
*Ihema | 1983 | 186 | 340–900 | |
Iwapibali/Rwakibare | - | - | 14–50 | |
*Kishanja | - | - | 3–9 | |
*Kivumba | - | - | 35–110 | |
*Mihindi | - | - | 44–140 | |
*Muhari | - | - | 2–7.5 | |
Nasho | 1975 | 50 | 55–160 | |
*Ngerenke | - | - | 5–20 | |
*Rukira | - | - | 2–6 | |
Rwampanga | 1975 | 30 | 38–110 | |
*Rwanyakizinga | - | - | 78–250 | |
Rwehikama | 1975 | 70 | 77–260 | |
Total | (426–650) | (758–2 235) | ||
Akagera Swamps | - | - | (4 000) 3 | |
Akagera River and tributaries | - | 200 | ||
TOTAL (rounded) | 3 000–3 950 | 2 600–9 650 |
1 Aubray, 1976
2 Reizer, 1975
3 unaccessible; not in total
* Lakes located in Akagera National Park
4. STATE OF THE FISHERY
4.1 Yield
Present yield estimates vary from 1 630 t (Table 1) to 1 800 t (Giudicelli et al., 1987), and 3 000–3 950 t (see table 2). An average current estimate of 2 500 t/yr seems reasonable.
4.2 Factors influencing yield
A variety of factors influence the yield of Rwandan inland waters. Lake Kivu traditionally has been a poor lake for fishing and, as a consequence, only the narrow coastal fringe has been exploited in a desultory manner (about 300 t of cichlids per year) (Welcomme, 1979a).
Now that Limnothrissa miodon has become established in Lake Kivu (yield about 1 900 t in 1987), an average total yield of about 2 000 t can be expected from the Rwandese waters of Lake Kivu.
The high altitude lakes (i.e. Bulera and Luhondo) and Upper Akagera Lakes Complex are fairly intensely exploited, although with proper management they could possibly sustain higher levels of catch. The Lower Akagera Lakes Complex was barely exploited because most of it lies within the game reserve and because of the lack of transport facilities in Rwanda (fish was caught mainly by Tanzanian fishermen in Lake Ihema). More recently, a development project in Lake Ihema allows fish catching and marketing to be effective in Rwanda (186 t in 1983; 400 t in 1986).
4.3 Future development possibilities
The fish catch from Rwanda could be increased, depending mainly on fisheries management. Although some authors estimate that Lake Kivu could yield up to about 5 500 t/yr for the Rwandan waters, a recent study, based on acoustic stock assessment surveys, estimates that the catchable L. miodon stock does not exceed 945 t in Rwanda.
Overfishing and destructive fishing methods have already considerably decreased production in the Upper Akagera Lakes and in those Lower Akagera Lakes not located in the National Park. Proper fisheries management and respect of fisheries regulations would significantly increase production. Dunn (1974) simply proposes a limit of 5 fishermen/km2 for each lake and a catch limit of 12.5 t/km2/yr.
The decision to officially open lakes located in the National Park to fishing activities must consider, on one hand, the estimated yield (1 730 t/yr) and, on the other hand, the damages that may arise in the National Park (Dunn, 1974).
No great increases can be anticipated for the high altitude lakes.
5. KEY BIBLIOGRAPHY
General: Aubray, 1976; Dunn, 1974; Mahy, 1977; Reizer, 1975
Lake Kivu: Hanek et al., 1988
Akagera Basin: Burgis, Mavuti, Moreau and Moreau, 1987; Frank et al., 1984;
Kiss, 1977a, b
6. WATER BODIES DIRECTORY
Lakes | ||
Bilinga | Kidogo* | Muhazi (= Mohasi) |
Birira | Kirimbi | Murago (= Rumira) |
Bulera | Kishanja (= Kisanji) | Nasho |
Chuju | Kivu | Ngerenke |
Cyohoha North | Kivumba | Rugwero |
Cyohoha South | Luhondo | Rukira |
Gaharwa | Mihindi | Rwampanga (= Mponga) |
Gashanga | Mirayi | Rwanyakizinga (= Rwanye) |
Hago | Mugesera | Rwehikama |
Ihema | Muhari | Sake |
Iwapibali (= Rwapibale = Rwakibale = Rwakibare) | ||
Karago | ||
Swamps | ||
Akagera** | Rugezi (= Ruguesi) | |
Rivers | ||
Akagera** | Ruzizi |
* Mistakenly called “Murago” on some official maps (Dunn, 1974)
** Also called “Kagera”
LAKE BILINGA
Geographical data | |
Location: | Rwanda - 1°37'S; 29° 32'E |
Altitude: | over 2 300 m |
Surface area: | 0.2 km2 |
Max. length: | 0.8 km |
Max. width: | 0.5 km |
Outflowing river: none; internal basin |
Fisheries data
Potential annual yield: High altitude, isolated lake. Production, if any, must
be very low. No data available.
LAKE BIRIRA
Geographical data | |
Location: | Rwanda (Upper Akagera Lakes Complex) |
Surface area: | 5.4 km2 |
Depth: | 6.0 m (mean) |
Physical and chemical data (Kiss, 1976a) | |
Surface temperature: | 25° C |
Conductivity: | 157 μ S/cm |
pH: | 8.0 |
Fisheries data | |
No. of fishermen: | 6 in 1973; recommended number: 27 (Dunn, 1974) |
No. of boats: | 6 in 1973 |
Total annual catch and effort: 70 t in 1975 (Reizer, 1975) | |
Potential annual yield: | 21 t (40 kg/ha: Aubray, 1976) |
67 t (125 kg/ha: Dunn, 1974) |
LAKE BULERA
Geographical data | |
Location: | Rwanda - 1° 26'S; 29° 46'E |
Altitude: | 1 866 m |
Surface area: | 54 km2 |
Depth: | 174 m (max); 80 m (mean) |
Max. length: | 13 km |
Max. width: | 7 km |
Volume: | 4.5 km3 |
Inflowing river: | Rusumu, Kabura |
Outflowing river: | short channel to Lake Luhondo |
Physical and chemical data (Damas, 1954) | |||
Surface temperature: 19° C | |||
Conductivity: | 110 μ S/cm | ||
pH: | 7.5; 8.2 (Mahy, 1977) | ||
Oxygen: | Surface: oversaturated | ||
-160 m: 0.52 mg/l | |||
Ionic composition: | mg/l | ||
Ca | 7.1 | ||
Mg | 3.9 | ||
Cl | 0 | ||
SO4 | 0 | ||
Fisheries data | |||
Fish species: | Main catches: Oreochromis niloticus, introduced in 1961 | ||
No. of fishermen: | 85* (Reizer, 1975) | ||
Total annual catch: | 100 t* (Reizer, 1975) | ||
Potential annual yield: | For Lake Bulera: 50 t (10 kg/ha: Reizer, 1975) |
* (for Lake Bulera+Lake Luhondo+Rugezi Swamp)
LAKE CHUJU
Geographical data | |
Location: | Rwanda (Lower Akagera Lakes Complex) |
Surface area: | 0.2 km2 |
Fisheries data | |
No. of fishermen recommended: 1 (Dunn, 1974) | |
Potential annual yield: | 1 t (40 kg/ha: Aubray, 1976) |
2.5 t (125 kg/ha: Dunn, 1974) |
LAKE CYOHOHA NORTH
Geographical data | |
Location: | Rwanda (Upper Akagera Lakes Complex) No longer exists; dried out completely and is now cultivated area. |
LAKE CYOHOHA SOUTH
(International water)
Geographical data | |||
Location: | Rwanda, Burundi - 2° 20'–2° 35'S; 29° 58'–30° 13'E (Upper Kagera Lakes Complex) | ||
Altitude: | 1 380 m | ||
Surface area: | 76 km2 (18 km2 in Rwanda) (Kiss, 1977a) | ||
Depth: | 11 m (mean: 5.2 m) (Kiss, 1977a) | ||
Volume: | 395 × 106 m3 | ||
Max. length: | 32 km | ||
Max. width: | 2 km (Kiss, 1977a) | ||
Shoreline: | 227 km total; 63 km in Rwanda (Kiss, 1977a) | ||
Note: | Lake called “Cyohoha” in Burundi. | ||
Physical and chemical data (Kiss, 1976a; 1977a) | |||
Conductivity: | K20 250–256 μ S/cm; 296 (surface); 319 (bottom) μ S/cm | ||
pH: | 8.5–9.5 (surface); 7.2 (bottom) | ||
Temperature: | 23–27° C (surface) | ||
Ionic composition: | mg/l | ||
Na | 25.75 | ||
K | 9.55 | ||
Ca | 9.0 | ||
Mg | 10.85 | ||
Cl | 4.30 | ||
SiO2 | 5.05 | (surface-bottom) | |
HCO3 | 152–171 |
Fisheries data | ||
No. of fish species: | 7: (3 Oreochromis spp., 2 Haplochromis spp., | |
1 Synodontis sp., 1 Clarias sp.) (Kiss, 1977a) | ||
No. of fishermen: | 65 in Rwanda in 1973; 31 recommended (Dunn, 1974) | |
20 in Rwanda in 1975 (Kiss, 1977a) | ||
50 in Lake in 1975 (Kiss, 1977a) | ||
No. of boats: | 65 in Rwanda in 1973 | |
Total annual catch: | in Rwanda: | 90 t in 1968 |
40 t in 1973 (Dunn, 1974) | ||
40 t in 1975 (Reizer, 1975) | ||
20 t in 1975 (Kiss, 1977a) | ||
in Lake: | 60 t in 1975 (Kiss, 1977a) | |
Potential annual yield: | ||
70 t in Rwanda (40 kg/ha: Aubray, 1976) | ||
225 t in Rwanda (125 kg/ha: Dunn, 1974) |
LAKE GAHARWA
Geographical data | |
Location: | Rwanda (Upper Akagera Lakes Complex) |
Surface area: | 2.3 km2 |
Depth: | 2.0 m (mean) |
Physical and chemical data (Kiss, 1976a) | |
Surface temperature: | 25.0° C |
Conductivity: | 192 μ S/cm |
pH: | 10.0 |
Fisheries data | |
No. of fishermen: | 26 in 1973; recommended: 11 (Dunn, 1974) |
No. of boats: | 26 in 1973 |
Total annual catch: | 59 t in 1968 |
10 t in 1973 - overexploitation (Dunn, 1974) | |
10 t in 1975 (Reizer, 1975) | |
Potential annual yield: | 29 t (125 kg/ha: Dunn, 1974) |
9 t (40 kg/ha: Aubray, 1976) |
LAKE GASHANGA
Geographical data | |
Location: | Rwanda (Upper Akagera Lakes Complex) |
Surface area: | 2.3 km2 |
Depth: | 3.0 m (mean) |
Physical and chemical data (Kiss, 1976a) | |
Surface temperature: | 26° C |
Conductivity: | 134 μ S/cm |
pH: | 7.0 |
Fisheries data | |
No. of fishermen: | 13 in 1973; recommended: 11 (Dunn, 1974) |
No. of boats: | 13 in 1973 |
Total annual catch: | |
30 t in 1973 (Dunn, 1974) | |
30 t in 1975 (Reizer, 1975) | |
Potential annual yield: | |
29 t (125 kg/ha: Dunn, 1974) | |
9 t (40 kg/ha: Aubray, 1976) |
LAKE HAGO
Geographical data (Kiss, 1977a) | ||||
Location: | Rwanda (Lower Akagera Lakes Complex), Akagera National Park | |||
Surface area: | 16.1 km2 | |||
Depth: | 5.8 m (max); 4.5 m (mean) | |||
Max. length: | 6.0 km | |||
Max. width: | 5.8 km | |||
Volume: | 45.2 × 106 m3 | |||
Shoreline: | 33.5 km | |||
Physical and chemical data (Kiss, 1976a, 1977a) | ||||
Conductivity: | 97 μ S/cm (surface); 99 μ S/cm (bottom) | |||
pH: | 8.92 (surface); 7.82 (bottom) | |||
Ionic composition: | mg/l | |||
Surface | Bottom | |||
Na | 5.5 | 5.4 | ||
K | 5.4 | |||
Cl | 5.66 | 4.95 | ||
Ca | 9.5 | 9 | ||
Mg | 3.0 | 4.03 | ||
CO3 + HCO3 | 54.9 | 61.0 | ||
SiO2 | 5.2 | 6 | ||
Fe++ | 0.45 | 0.70 |
Fisheries data | |
No. of fishermen: | 6 in 1975–76 (Kiss, 1977); recommended: 80 (Dunn, 1974) |
Total annual catch: | 90 t in 1975–76 (Kiss, 1977a) |
Potential annual yield: | |
210 t (130 kg/ha: Dunn, 1974) | |
64 t (40 kg/ha: Aubray, 1976) |
LAKE IHEMA
Geographical data (Kiss, 1977) | |
Location: | Rwanda (Lower Akagera Lakes Complex), Akagera National Park |
Altitude: | 1 291 m |
Surface area: | 86 km2 |
Depth: | 7 m (max); 4.8 m (mean) |
Max. length: | 22 km |
Max. width: | 7.8 km |
Shoreline: | 78 km |
Volume: | 512.6 × 106 m3 |
Physical and chemical data (Kiss, 1976a, 1977b) | ||||
Surface | Bottom | |||
Temperature: °C | 24.6–26.7 | 23.5 | ||
pH: | 7.15 | 6.3 | ||
Oxygen: (saturation %) | 105 | 8 | ||
Conductivity: (μ S/cm) | 110 | 103 | ||
Ionic composition: | mg/l | |||
Na | 5.9 | 3.9 | ||
K | 1.9 | 1.0 | ||
Cl | 8.8 | 7.8 | ||
Ca | 2.46 | 6.92 | ||
Mg | 3.9 | 5.4 | ||
CO3+HCO3 | 42.7 | |||
SiO2 | 6–9.2 | 6.7–9.2 | ||
NO2 | 0 | 0–0.3 | ||
NH4 | 0 | 0.03–0.5 | ||
PO4 | 0 | 0–0.03 |
Fisheries data | |
No. of fish species: | 35 species in 9 families: Cichlidae (11 sp), Mormyridae (7 sp), Characidae (3 sp), Clariidae (2 sp), Cyprinidae (7 sp), Schilbeidae (1 sp), Mochokidae (2 sp), Mastacembelidae (1 sp), Ciprinodontidae (1 sp), (Frank et al., 1984) |
Main catches: | Cichlidae (70%): mainly Oreochromis niloticus and O. macrochir; Clariidae (25%): mainly Clarias gariepinus (Frank et al., 1984) |
No. of fishermen: | 50 in 1968, 30 in 1970, 20 in 1971, 12 in 1972 (Kiss, 1977b) |
42 (21 fishing units) in 1981 (Micha, quoted in Frank et al., 1984) | |
360 recommended (Dunn, 1974) |
Total annual catch: | |||
Year | Total catch (t) | ||
1968, 1969 | 450 | ||
1970 | 180 | ||
1972 | 75 | (Kiss, 1977b: Tanzanian fishermen; decrease of catch due to increase of Rwandese watch on lake) | |
1981 | 168 | (Frank et al., 1984: catches from a fisheries development project) | |
1982 | 171 | ||
1983 | 186 | ||
Potential annual yield: | |||
900 t = 1 200 t minus 300 t (predators) (Kiss, 1977b) | |||
900 t (Dunn, 1974) | |||
400 t (186 t for commercial species) (Micha, quoted in Frank et al., 1984) | |||
340 t (40 kg/ha: Aubray, 1976) |
LAKE IWAPIBALI (= RWAPIBALE = RWAKIBALE = RWAKIBARE)
Geographical data (Kiss, 1977b) | |
Location: | Rwanda (Lower Akagera Lakes Complex), Akagera National Park |
Surface area: | 3.6 km2 |
Depth: | 6 m (max); 4.3 m (mean) |
Max. length: | 4 km |
Max. width: | 1.8 km |
Shoreline: | 9.5 km |
Volume: | 13.6 × 106 m3 |
Physical and chemical data (Kiss, 1976a, 1977b) | ||||
Surface | Bottom | |||
Temperature: °C | 23.7–26.8 | 22.7–23.6 | ||
Conductivity: (μ S/cm) | 107 | |||
pH: | 7.05 | 6.40 | ||
Ionic composition: | mg/l | |||
Ca | 5.12 | 3.64 | ||
Mg | 3.80 | 3.30 | ||
Na | 4.5 | 4.3 | ||
K | 1.8 | 1.3 | ||
Fe++ | 0.4 | 0.8 | ||
Cl | 8.1 | 8.7 | ||
CO3-HCO3 | 54.9 | 39.65 | ||
SiO2 | 8.4 | 8.4 | ||
Fisheries data | ||||
No. of fishermen: 4 in 1975/76 (Kiss, 1977a); 18 recommended (Dunn, 1974) | ||||
Potential annual catch: | ||||
50 t (138 kg/ha: Dunn, 1974) | ||||
14 t (40 kg/ha: Aubray, 1976) |
LAKE KARAGO
Geographical data | |
Location: | Rwanda - 1°38'S; 29°31'E |
Altitude: | over 2 300 m |
Surface area: | 0.3 km2 |
Max. length: | 1 km |
Max. width: | 0.5 km |
Inflowing river: | Nyamukongoro |
Outflowing river: | none; internal basin |
Fisheries data: | |
Potential annual yield: | high altitude, isolated lake; production, if any, must be very low. No data available. |
LAKE KIDOGO
Mistakenly called “MURAGO” on some official maps (Dunn, 1974)
Geographical data | |
Location: | Rwanda (Upper Akagera Lakes Complex) |
Surface area: | 2.2 km2 |
Depth: | 3.0 m (mean) |
Physical and chemical data | |
Surface temperature: | 24.0°C |
Conductivity: | 129 μ S/cm |
pH: | 6.5–7.0 |
Fisheries data | |
No. of fishermen: | 8 in 1973; recommended: 11 (Dunn, 1974) |
No. of boats: | 8 in 1973 |
Total annual catch: | |
20 t in 1968 (Dunn, 1974) | |
40 t in 1973 (Dunn, 1974) | |
40 t in 1975 (Reizer, 1975) | |
Potential annual yield: | |
9 t (40 kg/ha: Aubray, 1976) | |
28 t (125 kg/ha: Dunn, 1974) |
LAKE KIRIMBI
Geographical data | |
Location: | Rwanda (Upper Akagera Lakes Complex) |
Surface area: | 3.4 km2 |
Depth: | 2.5 m (mean) (Kiss, 1976a) |
Physical and chemical data (Kiss, 1976a) | |
Surface temperature: | 24.0°C |
Conductivity: | 204 μ S/cm |
pH: | 8.0 |
Fisheries data | |
No. of fishermen: | 15 in 1973; recommended: 11 (Dunn, 1974) |
No. of boats: | 15 in 1973 |
Total annual catch: | |
20 t in 1973 (Dunn, 1974) | |
20 t in 1975 (Reizer, 1975) | |
Potential annual yield: | |
14 t (40 kg/ha: Aubray, 1976) | |
42 t (125 kg/ha: Dunn, 1974) |
LAKE KISHANJA (= KISANJI)
Geographical data | |
Location: | Rwanda (Lower Akagera Lakes Complex) |
Surface area: | 0.7 km2 |
Fisheries data | |
No. of fishermen: | recommended: 4 (Dunn, 1974) |
Potential annual yield: | |
3 t (40 kg/ha: Aubray, 1976) | |
9 t (125 kg/ha: Dunn, 1974) |
LAKE KIVU
(International water)
see entry under country “ZAIRE”
LAKE KIVUMBA
Geographical data (Kiss, 1977b) | ||||
Location: | Rwanda (Lower Akagera Lakes Complex), Akagera National Park | |||
Surface area: | 8.7 km2 | |||
Depth: | 5.6 m (max); 4.2 m (mean) | |||
Max. length: | 5.2 km | |||
Max. width: | 3.5 km | |||
Volume: | 30.3 × 106 m3 | |||
Shoreline: | 18.2 km | |||
Physical and chemical data (Kiss, 1976a, 1977b) | ||||
Surface | Bottom | |||
pH: | 9.15 | 6.70 | ||
Conductivity: (μ S/cm) | 103 | 100 | ||
Ionic composition: | mg/l | |||
Ca | 9.00 | 8.00 | ||
Mg | 2.7 | 3.3 | ||
Na | 5.4 | 5.2 | ||
Fe++ | 0.55 | 0.8 | ||
Cl | 6.3 | - | ||
CO3-HCO3 | 61.01 | - | ||
SiO2 | 8 | 8.5 |
Fisheries data | |
No. of fishermen: | 5 in 1975 (Kiss, 1977b) |
46 recommended (Dunn, 1974) | |
Potential annual yield: | |
110 t (126 kg/ha: Dunn, 1974) | |
35 t (40 kg/ha: Aubray, 1976) |
LAKE LUHONDO
Geographical data | |||
Location: | Rwanda - 1°30'S; 29°44'E | ||
Altitude: | 1 760 m | ||
Surface area: | 26.1 km2 | ||
Depth: | 68 m (max); 30 m (mean) | ||
Max. length: | 10 km | ||
Max. width: | 7 km | ||
Volume: | 1.0 km3 | ||
Inflowing river: | Gasura, outflow from Lake Bulera | ||
Outflowing river: | Mukungwa | ||
Physical and chemical data (Damas, 1954) | |||
Surface temperature: | 20°C | ||
Conductivity: | 200 μ S/cm | ||
pH: | 8.0 | ||
Oxygen: | Surface: oversaturated | ||
No oxygen in hypolimnion (-10 m), but not permanent, as water movement may occur (Mahy, 1977) | |||
Ionic composition: | mg/l | ||
Ca | 10.0 | ||
Mg | 8.4 | ||
Cl | 0 | ||
SO4 | 0 | ||
Fisheries data | |||
Main catches: | Oreochromis niloticus (mainly); Haplochromis sp. | ||
No. of fishermen: | 55 in 1973 (Dunn, 1974) | ||
85 (Lake Lahondo+Lake Bulera+Rugezi Swamp) (Reizer, 1975) | |||
Total annual catch: | |||
16 t in 1968 | |||
50–100 t (Dunn, 1974) | |||
100 t in 1975 (Lake Luhondo+Lake Bulera+Rugezi Swamp) | |||
(Reizer, 1975; Aubray, 1976) | |||
Potential annual yield: | 50 t (20 kg/ha: Reizer, 1975) |
LAKE MIHINDI
Geographical data (Kiss, 1977b) | |
Location: | Rwanda (Lower Akagera Lakes Complex), Akagera National Park |
Surface area: | 10.9 km2 |
Depth: | 6.8 m (max); 4.4 m (mean) |
Max. length: | 4.2 km |
Max. width: | 3.9 km |
Shoreline: | 14.5 km |
Volume: | 41.8 × 106 m3 |
Physical and chemical data (Kiss, 1976a; 1977b) | |||
Temperature: | 22.6–24° C | ||
Conductivity: | 97 μ S/cm | ||
pH: | 7.10 | ||
Ionic composition: | mg/l | ||
Na | 3.6 | ||
K | 0.9 | ||
Ca | 4.34 | ||
Mg | 4.50 | ||
Cl | 6.40 | ||
CO3+HCO3 | 39.65 | ||
Fe++ | 0.9 | ||
Fisheries data | |||
No. of fishermen: | 8 in 1975 (Kiss, 1977b) | ||
54 recommended (Dunn, 1974) | |||
Potential annual yield: | |||
140 t (128 kg/ha: Dunn, 1974) | |||
44 t (40 kg/ha: Aubray, 1976) |
LAKE MIRAYI
Geographical data | |
Location: | Rwanda (Upper Akagera Lakes Complex) |
Surface area: | 2.3 km2 |
Depth: | 3.5 m (mean) (Kiss, 1976a) |
Physical and chemical data (Kiss, 1976a) | |
Surface temperature: | 25.5° C |
Conductivity: | 144 μ S/cm |
pH: | 7.0 |
Fisheries data | |
No. of fishermen: | 17 in 1973; recommended: 11 (Dunn, 1974) |
No. of boats: | 17 in 1973 |
Total annual catch: | |
20 t in 1973 (Dunn, 1974) | |
20 t in 1975 (Reizer, 1975) | |
Potential annual yield: | |
29 t (125 kg/ha: Dunn, 1974) | |
9 t (40 kg/ha: Aubray, 1976) |