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1 Technical Note: Hydrology of the Lake Chilwa wetland, Malawi Matthew McCartney June 2007 Description Lake Chilwa is located in the Southern region of Malawi on the country’s eastern boarder with Mozambique between latitude 15°00’S and 15°30’S and between longitude 35°30'E and 35°55'E. The wetland comprises the lake (i.e. open water), typha swamps, marshes and seasonally inundated grassland floodplain. The entire wetland is approximately 40 km from east to west and 60 km from north to south with a total area of about 2,310 km 2 (EAD, 2001). The water level of the lake is at an altitude of 627 masl. There is no outflow from the lake, which consequently varies considerably in size and salinity depending on precipitation in the catchment area. The catchment is 8,349 km 2 of which 5,669 km 2 (68%) is in Malawi and 2,680km 2 (32%) is in Mozambique (EAD, 2001). A small increase in water level results in a large increase in the lakes surface area. Lake Chilwa is very shallow, averaging 1-2 metres in depth with a maximum depth of only just over 2.5 metres (Figure 1). The wetland has a history of cyclic drying and filling. In the last century alone it has dried and filled eight times. The lake dried completely 1967/68 and most recently in 1996/97 1 . The hydrology of the lake is an important control on the ecology of the wetland, determining not only the water chemistry and physical properties, but also the composition of the vegetation and soil characteristics (Howard-Williams and Walker, 1974). Figure 1: Bathymetric map of Lake Chilwa (source: UNESCO, 2004). Climate The climate of the region is largely controlled by the movement of air masses associated with the Inter-Tropical Convergence Zone (ITCZ). During the summer, high land temperatures produce low pressures and moisture is brought to the catchment through the inflow of maritime air masses from the Indian Ocean. During the winter, the sun moves north and the land cools, causing the 1 For this study, an attempt was made to obtain time series of lake water level from the Ministry of Water Resources. However, currently these data are unavailable in electronic form.

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Technical Note: Hydrology of the Lake Chilwa wetland, Malawi Matthew McCartney June 2007 Description Lake Chilwa is located in the Southern region of Malawi on the country’s eastern boarder with Mozambique between latitude 15°00’S and 15°30’S and between longitude 35°30'E and 35°55'E. The wetland comprises the lake (i.e. open water), typha swamps, marshes and seasonally inundated grassland floodplain. The entire wetland is approximately 40 km from east to west and 60 km from north to south with a total area of about 2,310 km2 (EAD, 2001). The water level of the lake is at an altitude of 627 masl. There is no outflow from the lake, which consequently varies considerably in size and salinity depending on precipitation in the catchment area. The catchment is 8,349 km2 of which 5,669 km2 (68%) is in Malawi and 2,680km2 (32%) is in Mozambique (EAD, 2001). A small increase in water level results in a large increase in the lakes surface area. Lake Chilwa is very shallow, averaging 1-2 metres in depth with a maximum depth of only just over 2.5 metres (Figure 1). The wetland has a history of cyclic drying and filling. In the last century alone it has dried and filled eight times. The lake dried completely 1967/68 and most recently in 1996/971. The hydrology of the lake is an important control on the ecology of the wetland, determining not only the water chemistry and physical properties, but also the composition of the vegetation and soil characteristics (Howard-Williams and Walker, 1974). Figure 1: Bathymetric map of Lake Chilwa (source: UNESCO, 2004). Climate The climate of the region is largely controlled by the movement of air masses associated with the Inter-Tropical Convergence Zone (ITCZ). During the summer, high land temperatures produce low pressures and moisture is brought to the catchment through the inflow of maritime air masses from the Indian Ocean. During the winter, the sun moves north and the land cools, causing the

1 For this study, an attempt was made to obtain time series of lake water level from the Ministry of Water Resources. However, currently these data are unavailable in electronic form.

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development of a continental high pressure system. The descending and outflowing air produces the regional dry season. For this reason rainfall is seasonal and largely occurs during the summer months, November to April (Figure 2). Mean annual precipitation for the catchment is approximately 1363 mm, but the rainfall pattern is irregular with significant variation from one year to the next and often several concurrent years of below average rainfall (Figure 3). Rainfall distribution in the wetland’s catchment is uneven. In the highlands average annual rainfall ranges from 1,100 mm to 1,600 mm, reaching 2000 mm on the high plateaus of Zomba and Mulanje and in the Chilaka Hills. Zomba town, located at 884 masl, receives an average of approximately 1380 mm a year. The lowland plains, surrounding the lake, receive much less rainfall; 900 to 1,000 mm per year Howard-Williams and Walker, 1974; World Lakes database, 2006). In years of heavy rainfall floods are common in some parts of the catchment. Potential evapotranspiration (determined by the method of Penman-Monteith) averages approximately 1320 mm, but typically exceeds rainfall in the dry season months, May to October (Table 2; Figure 1).

Temperatures in the Lake Chilwa catchment vary with altitude. The highlands are cool throughout the year, but the plains become very hot in the months of September to November with mean maximum temperatures approaching 300C. The lowest mean temperatures roughly coincide with the dry season (Table 2). Table 1: Climate stations for which data obtained

Nos. Name Latitude Longitude Altitude (masl)

Distance from wetland (km)

Rainfall data Temperature data

Potential Evaporation

MW55ZMBO Zomba (Town)

15.38 oS 35.33 oE 884 35.8 1893 – 1991 (mnthly total)

1901-1960 (mean mnthly)

Monthly average only

MW45CHKW Chikwe 14.75oS 35.67oE 717 36.7 1982-1991 (mnthly total)

Monthly average only

N/A

MW65CHTK Chitakali 16.00oS 35.45oE 645 76.5 1914-1988 (mnthly total)

N/A N/A

MW65MLNJ Mulanje 16.08oS 35.67oE 628 83.4 1981-1991 (mnthly total)

Monthly average only

Monthly average only

MW65MMSO Mimosa 16.08oS 35.58oE 653 83.8 1954-1992 (mnthly total)

Monthly average only

N/A

MW54CHLK Chileka 15.68 oS 34.97 oE 767 84.5 1939-1996 (mnthly total)

1939-1991 (mean mnthly)

Monthly average only

MZ65MLNG Milange* 16.10oS 35.78oE 745 86.6 1914-1968 (mnthly total)

Monthly average only

Monthly average only

* Located in Mozambique (source: FAO databases FAOClim and LocClim)

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Table 2: Mean monthly climate data (simple arithmetic mean of data from different stations)

Month Catchment

Precipitation (mm) Potential Evapotranspiration (mm) (Penman-Monteith)

Mean Daily Temperature (oC)

Jan 273 131 24 Feb 246 114 24 Mar 225 118 24 Apr 92 106 23 May 31 96 21 Jun 27 79 19 Jul 23 87 18

Aug 21 109 20 Sep 17 131 23 Oct 44 163 25 Nov 114 148 25 Dec 248 133 25

Annual 1363 1414 22 (source: FAO LocClim database) Figure 2: Mean monthly rainfall and Potential Evapotranspiration (Penman-Monteith)

derived from the FAO Loc-Clim database. a) b)

Figure 3: Rainfall measured at Zomba: a annual time series b) deviation from the annual

mean

0

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1000

1500

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1893

1899

1905

1911

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River flows Several rivers flow into Lake Chilwa, but only the six most prominent rivers (i.e., the Sombani, Namdzi, Likangala, Thondwe, Domasi and Phalombe) are perennial. Abstractions for human use are relatively low; about 0.15 Mm3 per day, with by far the largest abstractions (0.12 Mm3 per day) being for irrigation. However, there is some concern that as population in the catchment rises abstractions will increase (EAD, 2001). At present there is no water management plan for the catchment. Flow is measured on several of these rivers. Figure 4 shows graphs of time series of flow for the four gauging stations for which flow data were made available by the Ministry of Water Resources (Table 3). Although, as a consequence of different data availability, they cover different periods of time, the graphs illustrate:

i. the high seasonal variation in flow. ii. the considerable inter-annual variability in flow in all the rivers iii. the frequent occurrence of consecutive years in which flow is below the mean annual

discharge iv. the extremely poor data collection from the early 1980s to date; there are almost no

years with complete data at any of the three stations still operating. Table 3: Gauging stations for which mean monthly flow data are available Gauge number

River Length of record

Nos. of complete years

Latitude Longitude Catchment area (km2)

20221 Likangali at Nkokanguqo

1959-2002 20 15.41oS 35.44oE 144.0

20102 Sombani at Phaloni Hill

1951-1979 (closed)

24 15.63oS 35.76 oE 843.0

20303 Domasi at Domasi TTC

1957-1998 24 15.28 oS 35.38 oE 72.8

20222 Thondwe at Jali

1959-2002 19 15.49 oS 35.48 oE 302.0

Annual flows on all the rivers correlate reasonably well with annual rainfall (Figure 5). However, analyses of runoff (i.e., flow effectively normalized for catchment area), indicates considerable differences between the rivers. Although the seasonal pattern is the same at all the gauging stations (i.e. typically 77-85% of total annual runoff occurring between January and May) there are considerable differences in the magnitude of runoff measured at each of the gauging stations (Figure 6). This most likely reflects differences in rainfall between the different catchments; higher rainfall over higher altitude catchments resulting in more runoff. However, the altitudes of the gauging stations and areal weighted rainfall over each catchment are not available to confirm this hypothesis.

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a)

b)

c)

d)

0

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Flow

(Mm

3 )

Figure 4: Flow measured at gauging stations on rivers flowing into lake Chilwa and

departure from the mean annual flow: a) Sombani at Phaloni Hill; b) Domasi at Domasi TTC; c) Likangala at Nkokanguwo; d) Thondwe at Jali

0

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(Mm

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(Mm

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/195

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020406080

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/196

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/199

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(Mm

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/196

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a) b)

c) d)

Figure 5: Correlation between annual rainfall and annual flow at: a) Sombani at Phaloni

Hill; b) Domasi at Domasi TTC; c) Likangala at Nkokanguwo; d) Thondwe at Jali

Figure 6: Comparison of runoff (mm) from each of the catchments

y = 0.2104x - 105.2R2 = 0.3416

0

50

100

150

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250

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Rainfall (mm)

Flow

(Mm

3 )y = 0.0926x - 16.676

R2 = 0.5366

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Rainfall at Chileka (mm)

Flow

(Mm

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y = 0.1296x - 39.284R2 = 0.6697

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Rainfall at Chileka (mm)

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y = 0.1186x - 35.228R2 = 0.4301

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(Mm

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off (

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Sombani Domasi Likangala Thondwe

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Wetland water budget A crude (back of the envelope) estimate of the average annual water budget for the wetland was determined. The water budget of the wetland is approximated by the equation:

P + Qi = E + Qo (equation 1) Where: P = precipitation onto the wetland Qi = inflow into the wetland E = evapotranspiration from the wetland

(a combination of open water evaporation and evapotranspiration from the swamps and grass)

Qo = outflow Mean annual evapotranspiration from the wetland was estimated to be 3,782 Mm3 (Table 4). This estimate was derived from assumed areas for the different wetland vegetation types (EAD, 2001) and estimates of likely evapotranspiration losses. Open water evaporation was assumed to be 1,800 mm. Evapotranspiration from the typha swamp and marshes was assumed to be 1,700 mm. Potential evaporation from floodplain grasses was assumed to be 1,400 mm, with actual evapotranspiration slightly less in the dry season due to water deficit. Actual evapotranspiration from cultivated areas was assumed to be 1,350 mm, since these areas are irrigated and so water deficits are low. Table 4: Estimated evapotranspiration from different parts of the wetland.

Area Evapotranspiration (mm) Wet season* Dry season * Wet season Dry season Annual Total

(km2) (km2) mm Mm3 mm Mm3 Mm3 Open water 1054 648 900 948.6 900 583.2 1531.8 Typha swamp 640 699 900 576.0 800 559.2 1135.2 Marsh 163 300 900 146.7 800 240.0 386.7 Floodplain 220 430 707 155.5 600 258.0 413.5 Cultivated+ 233 233 750 174.8 600 139.8 314.6 Total 2001.6 1,780.2 3781.8

* wet season is November to April and dry season is May to October + irrigated rice, wetland rice and vegetable gardens (dimbas) Table 5 presents a summary of the mean annual water fluxes, with inflow (Qi) computed from equation 1. The estimation suggests that approximately 60% of the water in the wetland originates as direct rainfall onto the wetland, with 40% originating as flow from the surrounding catchment. The estimated inflow of 1,472 Mm3 equates to an average annual runoff from the catchment (6,039 km2) of 244 mm. Assuming an average annual rainfall over the catchment of 1,363 mm (Table 1) this corresponds to a coefficient of runoff of 17.9%.

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Table 5: Estimate of the average annual water fluxes (Mm3) into and out of the Lake Chilwa wetland

Wet Season Dry Season Annual Direct rainfall onto the wetland+ 2,033 277 2,310 Evapotranspiration from the wetland 2,002 1,780 3,782 Outflow from the wetland 0 0 0 Inflow 1,177 294 1,472 + Estimated to be 1,000 mm with 88% falling in the wet season Data requirements to improve the analyses

i) time series of water levels measured in the lake ii) any additional data on inflows into the lake iii) a water-level volume relationship for the wetland iv) better estimates of areal coverage of different wetland/vegetation types and variation

between the wet and dry season - from image analysis References Environmental Affairs Department (EAD), 2001. Lake Chilwa Wetland Management Plan. Ministry of Natural Resources and Environmental Affairs, Malawi Government. Howard-Williams, C. and Walker, B.H. 1974. The vegetation of a tropical African Lake: classification and ordination of the vegetation of Lake Chilwa (Malawi). The Journal of Ecology, 62 (3) 831-854. World Lakes Database 2006. Lake Chilwa. http://www.ilec.or.jp/database/afr/afr-01.html accessed 11/08/2006. UNESCO 2004. Man and the Biosphere Programme- Lake Chilwa bioreserve nomination. UNECO, Paris, France 57pp.