AAG 2010 Washington DC Savanna Vegetation Changes as Influenced by Climate in East Africa Gopal Alagarswamy, Chuan Qin, Jiaguo Qi, Jeff Andresen, Jennifer.

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Presentation transcript:

AAG 2010 Washington DC Savanna Vegetation Changes as Influenced by Climate in East Africa Gopal Alagarswamy, Chuan Qin, Jiaguo Qi, Jeff Andresen, Jennifer Olson and Nathan Moo re Biocomplexity in the Environment Award

AAG 2010 Washington DC The EACLIPSE Loop

AAG 2010 Washington DC Goal of savanna vegetation modeling What is physical relation between climate and vegetation? What shifts in vegetation and changes of grass production are likely to occur in future? How will vegetation changes influence livelihood systems that depend on livestock and savanna natural resources?

AAG 2010 Washington DC Activities 1.Simulate relation between current climate and savanna vegetation production using ecosystem model Century (Parton et al., 1992) and historical gridded climate data from WorldClim( : WorldClim – Hijmans et al., 2005) (18km and 6 km). 2. Validate ecosystem model Century using remotely sensed net primary productivity (NPP). 3. Project vegetation (grass, bush, trees) changes in the future based on projected climate from RAMS.

Land Cover of Case Study Sites Mt. Kenya Satellite picture of Mount Kenya

AAG 2010 Washington DC Grass Biomass as Simulated by the Century Model in the Northern Site

AAG 2010 Washington DC Validating Century Model to simulate biomass (as NPP) Need measured NPP data over large area to validate Century model. Field measurements of NPP data over large areas are scarce in the study area. Can we use remotely sensed NPP data to validate the Century model?

AAG 2010 Washington DC Comparison of NPP between Century and MODIS Century NPPMODIS NPP

MODIS/ Century NPP Correlation 2010 AAG Washington, D.C. –CENTURY and MODIS NPP are generally correlated with each other. –However, the magnitude of MODIS NPP is much larger than the CENTURY NPP. –WHY?

Validation Steps 1.Compare CENTURY and MODIS grassland NPP of pixels – Using Landcover data: GlobCover – Problem: Other plant species contribute to NPP. 2.Calculate grassland-only MODIS NPP – CENTURY Assumption: Whole pixel is covered by grassland. – remotely sensed NPP of a pixel is explained by: 2010 AAG Washington, D.C.

Summary of Validation CENTURY Model can be validated using R.S. data and be used to simulate grass biomass AAG Washington, D.C.

AAG 2010 Washington DC Relative change in grass biomass from 2000 to 2050

AAG 2010 Washington DC Conclusion 1.Century does satisfactory job of estimating NPP 2.Remotely sensed NPP can be used to validate Century Model. 3.Impact of climate change on NPP varies widely across study area.

AAG 2010 Washington DC Next steps 1.Simulate NPP at higher resolution (6 km) and use additional GCMs. 2.Simulate NPP of other vegetation types (bush, trees, and crops). 3.Link vegetation modeling results to field data results to assess the influence of climate on the livelihood systems.

The EACLIPSE Loop Climate Change Temperature Precipitation Droughts Floods Savanna Vegetation Local level Ecosystem structure (spp., composition, ratio woody/ herbaceous) Forage quant & quality (palatability) Regional level Length of growing period Ecosystem structure Productivity Temporal & spatial lag effects, non-linear response. Resilience to droughts Land Management Grazing Scale: Intensity Mobility-Household Length of Orbit-Community Fire Frequency-Regional Land Use Livelihood Systems - Non-farm -Crops -Livestock Income diversification strategies within dynamic socio-economic system. Household Level decisions on: herd size and composition, grazing strategy, drought response Landscape Level : fire frequency, land use conversion Figure 1.The savanna human-land-climate system loop.

Research issues, questions 1. Seasonality shifts: The impact of highly variable and changing rainy seasons on natural vegetation, agriculture, people and livestock. Questions of recovery time of different vegetation types, flexibility of livestock & cropping. 2.Droughts: How will livelihood systems changes as short-term drought coping strategies evolve to long- term climate change adaptation?

AAG 2010 Washington DC Land cover Composition Those categories contain grassland, but they also have portion of other species. Thus NPP still includes influence from forest or shrubland. Since forest or shrubland normally have higher NPP than grassland, the grassland NPP here was overestimated. 1 Rainfed cropland 2 Mosaic cropland(50-70%)/vegetation 3 Mosaic vegetation(50-70%)/cropland 4 Forest 5 Mosaic forest or shrubland(50- 70%)/grassland 6 Mosaic grassland(50- 70%)/forest or shrubland 7 Closed to open Shrubland 8 Closed to open grassland 9 Sparse vegetation 10 Bare areas 11 Water bodies

AAG 2010 Washington DC Grassland-only NPP CENTURY assume a pixel is covered only by grassland. While, remotely sensed NPP of a pixel is: where n is the number of land cover types; NPP Endmember (i) is the NPP of pure pixel covered by landcover type i. Our objective is to get NPP Endmember-grassland in each pixel, which is the actual grassland NPP if the whole pixel is grassland.