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A new methodology for monitoring peatland degradation: Case study of the Okavango River Delta, Botswana

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Presented by Rosa María Román-Cuesta, from the Center for International Forestry Research (CIFOR), during the session 'Collective Actions for Peatlands Restoration in Indonesia' at UNFCCC's COP23 in Bonn, Germany, on November 9, 2017.

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A new methodology for monitoring peatland degradation: Case study of the Okavango River Delta, Botswana

  1. 1. Rosa Maria Roman-Cuesta (R.Roman-Cuesta@cgiar.org) Rosa Maria Roman-Cuesta, Thomas Gumbricht Indonesian Pavilion, 9th November, COP23, Bonn A new methodology for monitoring peatland degradation and restoration: the case study of the Okavango River Delta, Botswana
  2. 2. Monitoring peatland degradation/restoration Action • To develop a new pantropical methodology to monitor medium- term (i.e. 10-15 year) peatland changes. - The focus is on peat soil moisture - The analysis is on trends - Disaggregation between climate variability and human action Peatland degradation/restoration: soil moisture decreases/increases independently of rainfall trends. Collective • Ground validation of detected trends through: - Existing restoration projects & associated communities - Existing science initiatives
  3. 3. Method Rainfall trends TRMM satellite data Moisture trends MODIS satellite data (soil reflection calibrated with ground moisture) Trend relation between rainfall and soil moisture 2001-2016 250m
  4. 4. Pantropical wetlands map: peatlands Gumbricht et al. (2017) Swamp-bogsFloodout-swamps Okavango Delta • There are different types of peatlands (swamp-bogs, fens, riverine, floodout- swamps): anaerobic conditions prevail long enough to promote peat formation. • Degradation/restoration processes differ. • Peatland changes all relate to a balance between water availability vs soil moisture. Okavango Delta
  5. 5. The Okavango River Delta case study • A very large, swampy inland delta with marked seasonality (UNESCO world heritage). • All the water reaching the Delta is ultimately evaporated and transpired. • Each year approximately 11 cubic kilometers of water spreads over the 15,000 km2 area.
  6. 6. https://www.nationalgeographic.org/projects/okavango/water Floodout water supply: Two rivers originating in southern Angola supply nearly all the water that flows into Botswana’s Okavango Delta (Cuito River and Cubango River) Threats:  Conservation of water supply sources: • Cubango River is affected by fast development and poor management. • Rainfall variability  Extensive human-set fires in the delta and catchment area. The Okavango River Delta case study
  7. 7. Monitoring peatland degradation in Okavango(2001-2016) • Increased soil moisture-rainfall trend in the southern and eastern sides of the Okavango River Delta • Decreased soil moisture-rainfall trend in the western sides • Research on drivers: ground validation of fire, rainfall, and drainage, and effect on Peat status.
  8. 8. • Oma https://www.nationalgeographic.org/projects/okavango/ • National Geographic Expeditions (annually since 2015-present) to understand the ecology and threats of the Okavango River Delta and Catchment area. • Research on Water, Biodiversity, and Human communities in the area. • Identification of threats: fire among the most extended problems. Poor management and unsustainable development • Relevant findings: new species of flora and fauna, and peat in the Cuito River and supply Lakes
  9. 9. Next steps •Validating Okavango peat trends (i.e. cooperation with National Geographic funded researchers and data access) •Expanding research to Indonesia and Peru case studies. •Developing a pantropical map of peatland degradation/regeneration
  10. 10. Questions https://www.nationalgeographic.org/projects/okavango/

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