How do composite processes of land-water interactions scale up to generate regional patterns? What is the size and character of the riverine carbon pool.

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Presentation transcript:

How do composite processes of land-water interactions scale up to generate regional patterns? What is the size and character of the riverine carbon pool and the timing of its mobilization compared to net atmosphere-land carbon uptake? (and what are the factors controlling the partitioning of carbon between evasion and fluvial export?). What do these regional patterns in carbon transport and transformation indicate about the overall relation among water movement, landscape structure (topography, soils), and vegetation structure and productivity across the Amazon basin? What are the effects of climate variability and human forcing on fluvial carbon mobilization?

FROM SMALL STREAMS TO THE SEA: AN LBA-III MULTI-SCALE SYNTHESIS OF CARBON AND HYDROLOGICAL DYNAMICS ACROSS THE AMAZON LANDSCAPE Jeff, Alex, Vicky, Cleber, Dani, Reyna, Kelli, Arnaldo, Johannes … SYNTHESIS ACTIVITY: LAND-WATER COUPLING

Assessment of Processes Controlling pCO 2 : Regional Scale Patterns of Sources and Processes – several “update” vignettes……………

Sources of CO 2 Diurnal fluctuation of CO 2 in groundwater seep Forested Ultisol Southern Amazon, Juruena, MT UFMT/Cornell (J. Lehmann, M. Johnson, E. Couto, S. Riha, L. Rodrigues, M. Abdo, E. Selva, and E. Fernandes Carbon, Biogeochemistry, and Hydrology: Dynamics at the Terrestrial-Aquatic Interface

δ 13 C (‰) Δ 14 C (‰) contemporary C 4 grasses contemporary lowland C plants atmosphere carbonate rocks, solid earth CO older Mountain Mixed Lowland CPOC FPOC DOC pCO 2 Isotopic Constraints on Carbon Cycling carbonate weathering by contemporary plant CO 2 E. Mayorga & Seus Amigos Nature (2005)

SCOTT MILLER et al k 600 (cm hr -1 ) U 10 (m s -1 ) Amazon rivers  Mekong rivers Amazon lakes  Mekong lakes S. Miller Tapajos Richey et al. (2002) S. Alin Liege

CONCLUSION: not there – yet * k as f(not only W but surface renewal) * Heterogeneity of pCO 2

LARGE WETLANDS RESEARCH NEEDS Mel ack, SSC, 2003 Process-based models Ecological studies and methane emission measurements Seasonally flooded savannas Floodplains in eastern Peru Interfluvial wetlands in upper Negro basin Freshwater wetlands in Amazon delta Riparian zones of streams

"All models are wrong, but some are useful." G.E.P.Box (1979), Robustness in Statistics (Working towards being) based on Geospatial Hydrology/Landscape Models VIC (Variable Infiltration Capacity) Meso/Macroscale Landscape/Hydrologic Model DHSVM (Distributed Hydrology Soil Vegetation Model) Micro/Mesoscale Landscape/Hydrologic Model Sediments, Chemistry ….and, of course, Coe, Costa, Howard et al

D. Victoria et al

Modeled evapotranspiration for 3 scenarios: C1 – Pasture C2 – Soybean C3 – Forest Wet season Dry season Santiago, 2005

So how do we connect the dots” – do the integration and up/(down)-scaling? Technical Issues Collaboration/ Facilitation Issues (i.e. “people”)

Modelers rarely know much about “chemistry.” And certainly few biologists /chemists know much about (serious) modeling (especially at E&T level…)

Virtual Scaleable Basin The Virtual Scalable Basin (VSB) work attempts to make simulation modeling more flexible in order to: * more easily integrate useful input data sets. * more easily expand calculation for attempting more complex simulation objectives. * more easily develop new simulation modules for participation in modeling runs (thus facilitating collaboration) * take advantage of cutting-edge visualization tools including runtime visualization facilities. * more easily facilitate the sharing of useful output data sets.

Following the Open Modeling Interface (OpenMI), a VSB module “publishes” its interface to explicitly describe required inputs and produced outputs. Each module identifies a minimal yet complete set of metadata values for each input and output that other modules can interrogate for possible interaction.

Throughfall DOC Litterfall Leach DOC Litter C fract Litter Decomposition SOIL DOC DOC resp Percolation Sorption Processes DOC_Soilyr0 Tambem: NO 3, CO 2, NH 4 Porranee Rattanaviwatpong

Task 1. Integration Workshops (#1 late March, 2006; ~Aguas da Sao Pedro) Task 2. Complete and Integrate Cross-System Field Data into VSB Task 3. Establish the Virtual Scaleable Basin (VSB) Modeling and Informatics Infrastructure. Development of Fine-Scale Solute Export Model Scaling Hydrology Models Determination of Surface Forcing. Incorporate NPP Module