Hydrological Feedbacks in Tropical African Wetlands

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CHAPTER ONE : INTRODUCTION

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Hydrological Feedbacks in Tropical African Wetlands Simon Dadson University of Oxford (simon.dadson@ouce.ox.ac.uk)

Key challenges Linking across scales: can we predict the hydrological response to climate change? Representing feedbacks: how does the landsurface govern fluxes of water, energy, and carbon? Sustainable water futures: how can policymakers balance adaptation to climate change with food security, biodiversity, and other ecosystem services? HYDROLOGY & WATER RESOURCES BIODIVERSITY & ECOSYSTEM SERVICES FOOD PRODUCTION & SECURITY

Water use and ecosystem services HYDROPOWER FISHING RUAHA NATIONAL PARK USANGU WETLANDS AGRICULTURE IRRIGATION Water use in the Rafiji Basin, Tanzania. Upstream irrigation has dried wetlands, affected wildlife and reduced hydropower. Need to understand links between climate change, land use and water Photos: M. Acreman management

Hydrological feedbacks in the Earth system Feedbacks strongest in transition zones between wet and dry climates. Need to know state of soil moisture in order to provide accurate forecasts. Changes to water management can affect regional climate. Koster et al., 2004. Science 305:1138-1140

Maximum wetland fraction (1993-2004) Data: Prigent et al., 2008

Important Wetlands in Africa Niger Delta Lake Chad Sudd (S. Sudan) Congo Zambezi Okavango Mitch and Gosselink (2007)

Seasonal Inundation Data: Prigent et al., 2008

Flow routing and inundation in JULES Joint UK-Land Environment Simulator (JULES) takes temperature, wind speed, humidity, LW & SW radiation and precipitation from RCM; Evaporation Diagnose state of soil moisture by using a Radiation Pareto distribution of Rainfall soil moisture stores; Snow Convert to surface and subsurface flow. Flux of soil moisture and heat Inundated wetland area calculated using sub-grid elevation data wetland inundation Dadson et al., 2010, J. Geophys. Res., 115: D23114

Flow routing and inundation in JULES HydroSHEDS digital topography (90 m hydrologically sound DEM) Used to produce inundation parameters for large-scale model

Land-atmosphere atmosphere feedbacks in W. Africa Niger Inland Delta, Mali; Inundation drives water vapour flux and temperature anomaly; Seasonal flooding provides up to 50% of water vapour to atmosphere. Dadson et al., 2010, J. Geophys. Res., 115: D23114

Impact of flooding on water and energy fluxes Timing of flows accurately reproduced (R 2 = 0.70); ongoing work to improve groundwater in JULES Satellite observations show good representation of seasonal inundation pattern (passive & active microwave, near infra-red); Evaporation increases from 11 to 22 mm/day with inundation scheme; Evaporation reduces surface temperature by 5 K and diurnal temperature range by up to 15 K. Dadson et al., 2010, J. Geophys. Res., 115: D23114 Prigent et al., 2007, J. Geophys. Res, 112: D12107

Observed land-atmosphere atmosphere feedback warmer cooler warmer Number of new storms initiating in region of wetland After flooding Before flooding +50% Meteosat 1982-2005: Chris Taylor, CEH Time of day Development of a wetland breeze ; 50% more daytime storms during floods Better land-surface modelling will improve weather forecasts in West Africa. Dadson et al., 2010, J. Geophys. Res., 115: D23114 Taylor, (2010), Geophys. Res. Lett., 37, L041652

Links between the water and carbon cycles 0.6 Black: Column mean CH 4 (SCIAMACHY) Blue: Wetland fraction 2000 Wetland fraction 0.4 0.2 1800 1600 Column mean CH 4 (ppb) Max. inundation fraction 0.0 2004 2006 2008 Methane (CH 4 ) is the second most important greenhouse gas after CO 2. Wetlands are largest natural source of CH 4, via anoxic degradation of organics. CH 4 fluxes from wetlands are poorly quantified (105-278 Tg yr -1, 75% tropical).

Water Resources and Ecosystem Services Zwarts et al., 2005 Proposed new 90 MW dam at Fomi will: reduce fish populations by up to 36% disrupt complex relation between flooding and ecology (3-4 million staging waterbirds) but increase rice production in newly-irrigated areas by 320,000 t (to meet 90% of domestic demand) How can policymakers balance need for mitigation of & adaptation to climate change with food security, wetland biodiversity, and other ecosystem services?

Q & A