860 likes | 1.09k Views
Integrating Fluxes of Carbon Dioxide and Water Vapor From Leaf to Canopy Scales. Dennis Baldocchi Ecosystem Science Division/ESPM UC Berkeley. Outline. Overview Leaf-Canopy Scaling and Integration Concepts Show Tests of Such Models over Multiple Time Scales
E N D
Integrating Fluxes of Carbon Dioxide and Water Vapor From Leaf to Canopy Scales Dennis Baldocchi Ecosystem Science Division/ESPM UC Berkeley
Outline • Overview Leaf-Canopy Scaling and Integration Concepts • Show Tests of Such Models over Multiple Time Scales • Use the CANVEG Model to Ask Ecophysiological and Micrometeorological Questions Relating to Trace Gas Fluxes
Classes of Model Complexity • The breadth and linkage of functional components that describe the biophysics of trace gas exchange. • How driving variables are defined and used as inputs to non-linear model algorithms. • The geometric abstraction of the canopy.
System Complexity: Interconnection of Key Ecosystem Processes ESPM 111 Ecosystem Ecology
3-d Representation of Canopy Qi Chen and D. Baldocchi ESPM 111 Ecosystem Ecology
Geometrical Abstraction of the Canopy • One-Dimensional • Big-Leaf • Dual Source, Sun-Shade • 2-Layer • Vegetation and soil • Multi-Layered • Two-Dimensional • Dual source • sunlit and shaded • Vegetated vs Bare Soil • Three-Dimensional • Individual Plants and Trees After Hanson et al Ecol Appl 2004 ESPM 111 Ecosystem Ecology
Dual Source Model:Discrete Form Whole Canopy
Role of Proper Model Abstraction ESPM 111 Ecosystem Ecology
Basics of Ecosystem Models ESPM 111 Ecosystem Ecology
Quantifying Sources and Sinks • Biology: a(z), Ci, rs • Physics: rb, C(z)
Weight Source/Sink by Fraction of Sunlit and Shaded Leaves and Their Environment
Random Spatial Distribution: Poisson Prob Distr. Prob of Beam Penetration Prob of Sunlit Leaf
Sources of Spatial Heterogeneity • Vertical Variations in: • Leaf area index • Leaf inclination angles • Leaf Clumping • Leaf N + photosynthetic capacity • Stomatal conductance • Light, Temperature, Wind, Humidity, CO2
Turbulence Closure Schemes • Lagrangian • Eulerian • Zero Order, c(z)=constant • First Order, F=K dc/dz • Second Order and ++ (dc/dt, dw’c’/dt)
Higher Order Closure Equations and Unknowns ESPM 228 Adv Topics Micromet & Biomet
Lagrangian Near- and Far-Field Theory ESPM 228 Adv Topics Micromet & Biomet
Dispersion Matrix ESPM 228 AdvTopics Micromet & Biomet
Examples: Non-Linear Biophysical Processes Photosynthesis Transpiration Respiration Leaf Temperature
Leaf Energy Balance • R: is shortwave solar energy, W m-2 • L: is Longwave, terrestrial energy, W m-2 • lE: Latent Heat Flux Density, W m-2 • H: Sensible Heat Flux Density, W m-2 ESPM 129 Biometeorology
Leaf Energy Balance, Wet, Transpiring Leaf Net Radiation is balanced by the sum of Sensible and Latent Heat exchange ESPM 129 Biometeorology
Derivation 1: Leaf Energy Balance 2: Resistance Equations for H and lE 3: Linearize T4 and es(T) ESPM 129 Biometeorology
Linearize with 1st order Taylor’s Expansion Series ESPM 129 Biometeorology
Linearize the Saturation Vapor Pressure function ESPM 129 Biometeorology
Wc, the rate of carboxylation when ribulose bisphosphate (RuBP) is saturated • Wj, the carboxylation rate when RuBP regeneration is limited by electron transport. • Wp carboxylation rate with triose phosphate utilization ESPM 228, Advanced Topics in Micromet and Biomet
If Wc is minimal, then: If Wj is minimal, then If Wp is minimal, then ESPM 228, Advanced Topics in Micromet and Biomet
Analytical Equation for Leaf Photosynthesis Baldocchi 1994 Tree Physiology ESPM 228, Advanced Topics in Micromet and Biomet
Seasonality in Vcmax Wilson et al. 2001 Tree Physiol ESPM 228, Advanced Topics in Micromet and Biomet