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Using Biophysical Models to Ask (and Answer) Questions About Biosphere-Atmosphere Interactions. Dennis Baldocchi Alexander Knohl James Dorsey Biometeorology Lab University of California, Berkeley. ILEAP Meeting Boulder, CO Jan, 2006. ILEAPS Paradigm. Isotopic exchange.
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Using Biophysical Models to Ask (and Answer) Questions About Biosphere-Atmosphere Interactions Dennis Baldocchi Alexander Knohl James Dorsey Biometeorology Lab University of California, Berkeley ILEAP Meeting Boulder, CO Jan, 2006
ILEAPS Paradigm Isotopicexchange
Answering Questions with Models • Diffuse Radiation • Light Use Efficiency • Isoprene emission • Water Use Efficiency • Stable Isotopes • Sub-Grid Parameterization, Energy Balance Closure and Scaling • Insights from a 2-D, ‘Wet’ DaisyWorld
Key Attributes of CanVeg • Seasonality • Leaf Area Index • Photosynthetic Capacity (Vcmax) • Model parameters based on Site Measurements and EcoPhysiological Rules and Scaling • Stomatal Conductance scales with Photosynthesis • Jmax and Rd scale with Vcmax • Multilayer Framework • Computes Fluxes (non-linear functions) on the basis of a leaf’s local environment • Considers • Sun and Shade Leaf Fraction • Leaf Clumping • Leaf Inclination Angle • Non-local Turbulent Transport and Counter-Gradient Transfer
Another Form of Model Testing: Reproducing Spectral Fidelity Baldocchi et al, 2001 Ecological Modeling
How Sky Conditions Affect Net Carbon Exchange (NEE)?: Data Baldocchi, 1997 PCE
CO2 Flux and Diffuse Radiation:Data from AmeriFlux Niyogi et al., GRL 2004
How do Changes in Diffuse Radiation affect Canopy Fluxes?: Case: Mt Pinatubo Explosion, ~ 10% of beam -> diffuse direct beam Solar radiation [W m-2] Year of Mt. Pinatuboeruption diffuse Solar elevation angle [°] Gu et al, 2003, Science
Canopy Photosynthesis and Aerosols: Impact on Daily & Annual Scales, I increase diffuse by 10% beam: 1527 gC m-2 y-1 Canopy Photosynthesis may increase by +50 gC m-2 y-1
Conventional Wisdom:More Light Absorption with Diffuse Radiation WHY?
vpd is Correlated with Diffuse Fraction: Less Physiological Stress (?)
Stable Isotope Discrimination and Diffuse Light Preference of photosynthesis for light 12CO2 vs. heavier 13CO2
Simple Model suggests A/T decreases with D or Ci/Ca e.g. A/T of C4 > C3 But Complex feedbacks need to be considered!
In toto (considering coupled energy balance feedbacks) A/T increases with Ci/Ca
Sub-Grid Variability: Lessons Derived from Wet DaisyWorld Latent Heat Exchange Map
Eddy covariance footprints and ecosystem representativeness Footprint representation Newly developed 3d Lagrangian stochastic footprint model was run for a 1 m canopy and 3 m measurement height. Half a million trajectories were integrated to calculate the source probability density. The footprint calculation was run using the same grid geometry as the DaisyWorld simulation to allow convolution of the results. The EC “tower” was placed in different locations in the simulated ecosystem, and the EC system's view of the ecosystem was calculated.
Eddy covariance footprints and ecosystem representativeness Each histogram shows 500 separate tower locations within the simulated ecosystem.
Conclusions • Biophysical Model aids in understanding the impact of diffuse light on photosynthesis, isoprene emission, water use efficiency and stable isotope discrimination • A cellular automata, energy balance model shows that spatial averaging of energy balance drivers can produce huge errors in grid-scale energy fluxes and can explain lack of energy balance closure
Acknowledgements • Funding • NASA, DOE/TCP, NIGEC/WESTGEC • Diffuse Light and Carbon • Lianhong Gu • Isoprene • Peter Harley, Jose Fuentes, Dave Bowling, Russ Monson & Alex Guenther • 13C Isotopes • Dave Bowling, Russ Monson • Footprints & DaisyWorld • Monique Leclerc, Tess Krebs, Joon Kim, Peter Levy, HaPe Schmid, Brian Amiro
Canopy Photosynthesis and Aerosols: Impact on Daily & Annual Time Scales, II
Quantifying Sources and Sinks • Biology: • Leaf area density, a(z) • internal conc, Ci • stomatal resistance, rs • Physics: • Boundary layer resistance, rb • Scalar conc, C(z)
Partial Explanation:Fiso is very sensitive to Leaf Temperature, which changed little in response to the imposed direct to diffuse partitioning