Regional Model-Data Comparison: An NACP Interim Synthesis Project Coordinators: Andy Jacobson, Mac Post, Debbie Huntzinger, Bob Cook Participants: Dozens.

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Presentation transcript:

Regional Model-Data Comparison: An NACP Interim Synthesis Project Coordinators: Andy Jacobson, Mac Post, Debbie Huntzinger, Bob Cook Participants: Dozens of modeling teams and data providers, Canada, USA, Mexico, Europe

Regional MDC Questions with Focus on North America Interannual Variation –What is the spatial pattern and magnitude of interannual variation in carbon fluxes during ? –What are the components of carbon fluxes and pools that contribute to this variation? 2002 Drought –Do model results and observations show consistent spatial patterns in response to the 2002 drought? –From measurements and ecosystem models, can we infer what processes were affected by the 2002 drought? Identification of Sources/Sinks –What are the magnitudes and spatial distribution of carbon sources and sinks, and their uncertainties during ?

CarbonTracker Inversion Model, Net Terrestrial Summer Flux (gC/m2/yr) CarbonTracker Estimated C Source/Sink ö

NASA-CASA Estimated C Source/Sink

Atmospheric Inversions Forward Models MODIS Flux tower sites CO 2 Flux GPP, LAI, NPP Use of Multiple Data Sources Survey Data Soil C, Crop NPP, Forest Biomass flux footprint size site continent region

Regional MDC Objectives Development of benchmark data sets and approaches for model-data evaluation. Evaluation of strengths and weaknesses of various model formulations, both inverse models and ecosystem models resulting from the comparison to data. Formal comparison of inverse and forward ecosystem model results for enhancing identification and diagnosis of temporal and spatial patterns of carbon fluxes. Understanding of mechanistic processes which lead to model differences

Synthesis of Interim NACP Results Ecosystem Models Contribute in hand regional, continental results (including ones cut from global analyses) A range of temporal and spatial resolutions No standardization of model runs! Inversion Models Contribute North America results in hand from TRANSCOM or from other relevant activities Spatial scales –TRANSCOM regions, and –1º grids centered on half-degrees Temporal scale - monthly

Ecosystem (Forward) Models ftp://nacp.ornl.gov/synthesis/2008/firenze/continental/continental_data_model_inventory.html

Inversion Models Results by Transcom Regions –Transcom3 IAV inversion (D Baker),13 models –Rödenbeck Jena, 3 different networks –CarbonTracker –FRCGC Japan (Patra) –U Michigan geostat, 2 models –LSCE France (Peylin) –LSCE France (Chevallier) –LSCE France (Rayner) –Penn State (Butler), 2 models Results by 1 degree –U of Toronto –CarbonTracker –LSCE –Jena –U of Michigan –MLEF-PCTM – Colorado State University

Observations and Measurements Satellite based –In Hand: MODIS GPP MODIS NPP (annual) MODIS LAI, FPAR, NDVI, EVI (gap filled, smoothed – from MODIS for NACP) Survey –In Hand: NASS crop yield based annual NPP Soil C (WISE-FC version 3.0), 30cm, 100cm FIA based biomass –In Development: Fast-track change in forest/agriculture C stocks for Canada, USA, Mexico Site based –Eddy flux NEE, estimated GPP, NPP All of these are not strictly direct measurements and involve some level of model intervention

Conversion to Common Grid - both Data and Model Spatial Resolution: 1°x1°, centered at (x.5, y.5 for each grid cell) Domain: 50° to 170° W longitude, 10° to 84° N latitude Temporal Resolution: monthly (or annual) netCDF files, CF-1 convention ftp://nacp.ornl.gov/synthesis/2008/firenze/continental

Fast-Track Inventory-based data for evaluation of Forward Ecosystem Models Organization of Inventory-Based Information By 48/49 states in the U.S. (Alaska not available) By 18 reporting units in Canada By states in Mexico Aggregated estimates for Agriculture Data by County Forest data by State

Inverse Models Produce model predictions of atmospheric CO 2 mole fractions Compare with the observed atmospheric CO 2 mole fraction Difference between them is attributed to differences in estimated (first guess) and the actual sources and sinks Numerical techniques, reduce these differences and solve for a set of sources and sinks that most closely matches the observed CO 2 mole fraction

North America Boreal (NABR) North America Temperate (NATM)

Atmospheric Inversions Forward Models MODIS Flux tower sites CO 2 Flux GPP, LAI, NPP Use of Multiple Data Sources Survey Data Soil C, Crop NPP, Forest Biomass flux footprint size site continent region

Convention: (-) sink (+) source North America: C Flux C Flux Average

2002 Inter-Model Annual Carbon Flux Mean Carbon FluxStandard Deviation Carbon Flux Inverse Models N=5 Forward Models N=12

2004 Inter-Model Annual Carbon Flux Mean Carbon FluxStandard Deviation Carbon Flux Forward Models N=12 Inverse Models N=5

Forward Model Mean July C Flux

Spatial Aggregation – TransCom Regions

IAV of NEE from Forward Models

Inversions 25 th percentile Central 75 th percentile Uptake IAV peak-peak IAV (sd) Forward models 25 th percentile Central 75 th percentile Uptake IAV peak-peak IAV (sd) Summary of NEE (boreal and temperate) comparison between Inverse and Forward Models

Forward or Ecosystem Models Large diversity of model types constructed for different reasons –Statistical relationships with environmental factors –Biologically based process representations based on experimental analyses –Incorporate a subset of processes that contribute to total CO 2 flux – often disturbances that, for a single location, are episodic are left out (NEE vs. NECB). More ecosystem components are modeled and therefore allows comparison with wider range of observations Long-term carbon pools, steady-state issues, dependence on initial conditions introduce difficulties

Atmospheric Inversions Forward Models MODIS Flux tower sites CO 2 Flux GPP, LAI, NPP Use of Multiple Data Sources Survey Data Soil C, Crop NPP, Forest Biomass flux footprint size site continent region

Prepared by Andy Jacobson, NOAA Spatial Aggregation Forward Models for TransCom Regions

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Inter-Model Variation in NEE Components – JJA (summer) 2002 Models included: CLM-CASA CLM-CN ORCHIDEE VEGAS1 EC-LUE MC1 TEM6 CASA-GFed2 NASA-CASA DLEM 1 Standard DeviationMean GPP Ra Rh

Inter-Model Variation in NEE Components – JJA (summer) Standard DeviationMean GPP Ra Rh Models included: CLM-CASA CLM-CN ORCHIDEE VEGAS1 EC-LUE MC1 TEM6 CASA-GFed2 NASA-CASA DLEM

Taylor Diagrams RMSD 2 =sd_obs 2 +sd_mod 2 -2*sd_obs*sd_mod*R

Atmospheric Inversions Forward Models MODIS Flux tower sites CO 2 Flux GPP, LAI, NPP Use of Multiple Data Sources Survey Data Soil C, Crop NPP, Forest Biomass flux footprint size site continent region

Agricultural NPP Select 1 degree cells that are 50% managed agriculture Compare model NPP in same 1 degree cells

Agricultural NPP

Forward Model Summary and Observations Forward models are very different and do not agree on timing or spatial distribution of C sources/sinks Examination of component processes shows the greatest discrepancy is in GPP Need additional analyses –Site data and information about model performance with site NEE –Examine managed forest NPP, esp. Southeast US –Need to clarify additional components of NECB besides NEE

Proceeding from Here Need Additional Model Variables: GPP, NPP, NEE, Ra, Rh, LAI (FPAR, NDVI, EVI), Soil C, Biomass at monthly or annual times Need Additional Model Experiments: Especially various disturbance effects – fire, biomass harvest, insect outbreaks CO 2 forcing, N deposition, management Need ideas: Additional regional/continental observation based datasets Creative methods for model-data comparison

Reporting of Current Findings Tasks Gather additional forward model metadata –What components of NECB are included –How processes are represented –Details on boundary and forcing conditions Develop Manuscripts 1.Fast-track Forest and Agriculture inventory – Model comparison 2.Temporal Analysis – mostly completed, need to complement with and “expert” update of the SOCCR estimates on an annual time step (Jacobson, McGuire, Post, others). This could involve interaction with Site Synthesis results for non-managed ecosystems (Tundra, wetlands, grasslands, stc.) 3.Spatial Analysis (Huntzinger, Post) 4.Extreme event analysis (Zeng)

After the Interim Synthesis: The Well Planned Regional Synthesis Conduct a formal regional scale data-model comparison Development of benchmarks for model evaluation ala C- LAMP Development of inventory change estimates and uncertainties in those estimates that are spatially and temporally resolved – Soil C, Forest, Agriculture Evaluation of inversion sensitivity to terrestrial biosphere model priors and other inversion uncertainties Evaluation of sensitivity of flask station CO 2 concentration estimates to terrestrial biosphere model and fossil fuel fluxes Model-data synthesis activities should NOT be delayed until after all data collection. They should begin now!