The Okavango Delta’s Pulse-Driven Hydro-Sediment Connectivity and Botswana’s Adaptive Wetland Governance
奥卡万戈三角洲脉冲式水沙连通性与博茨瓦纳适应性湿地治理
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Annual flood pulses from Angola’s highlands drive biogeochemical cycling and geomorphic reorganization across the Okavango Delta’s 15,000 km² alluvial fan.
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Unlike deltaic systems fed by predictable river regimes, its hydrology depends entirely on episodic, rainfall-triggered runoff routed through porous Kalahari sands.
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