Water in Africa: structurally scarce, variability increasing (climate change), governance weak. Not temporary drought — systemic stress.
Why scarcity is worsening:
- Population growth: SSA population 1.1B → 2.5B by 2050 (UN projections). Urban water demand doubling. Agricultural expansion (food production) = water demand spike.
- Climate change: Rainfall variability increasing. Dry seasons longer, wet seasons more intense (flooding, not storage). IPCC projections: Southern Africa -10 to -20% rainfall by 2050.
- Infrastructure deficit: Dams, treatment plants, distribution = underfunded. Urban supply = intermittent (Nairobi 3-5 days/week). Rural = borehole or nothing.
- Groundwater depletion: Unregulated extraction. Water table dropping 1-3m/year in some regions. Borehole depths increasing (cost + yield uncertainty).
- Transboundary conflicts: Nile (11 countries), Niger, Zambezi = shared basins. Upstream damming = downstream stress. Political friction rising.
Cape Town Day Zero (2018)
Context: 3-year drought. Dams at 15% capacity. City announced "Day Zero" — date when taps would be shut off (4M people).
Response: Extreme rationing (50L/person/day limit), agricultural restrictions, desalination emergency deployment, aquifer pumping.
Outcome: Day Zero avoided (rains arrived). But: $300M crisis cost, tourism collapse, businesses relocated, insurance repricing.
Lesson: Developed African city (best infrastructure on continent) nearly ran dry. If Cape Town vulnerable, everywhere is.
The investor error: Treating water as "available" input. Reality: water = primary constraint for agriculture, manufacturing, urban development. Site selection without water risk assessment = Russian roulette.