Page Banner

United States Department of Agriculture

Agricultural Research Service

Title: Inverse Estimation of Vcmax, Lai, and the Ball-Berry Parameter from Carbon and Energy Fluxes

Authors
item Wolf, Adam - UNIV. OF CALIFORNIA
item Akshalov, Kanat - BARAEV KAZAKH RESEARCH
item Saliendra, Nicanor - USDA FOREST SERVICE
item Johnson, Douglas
item Laca, Emilio - UNIV. OF CALIFORNIA

Submitted to: Journal of Geophysical Research
Publication Type: Peer Reviewed Journal
Publication Acceptance Date: September 21, 2005
Publication Date: March 29, 2006
Citation: Wolf, A., Akshalov, K., Saliendra, N., Johnson, D.A., Laca, E.A. 2006. Inverse estimation of Vcmax, leaf area index, and the Ball-Berry parameter from carbon and energy fluxes. Journal of Geophysical Research - Atmosphere 111:D0808 dois 10.1029/2005 JD005927 (1-18).

Interpretive Summary: The dynamics of carbon dioxide and energy above the earth's surface can be modeled accurately by knowing several key environmental and ecosystem characteristics. Our research involved the development of mathematical equations to estimate these various key characteristics. To test these equations, we measured energy and carbon dioxide fluxes in a grassland site in northern Kazakhstan. Results of our tests showed that the mathematical equations we developed could predict carbon and energy fluxes with a 80 to 95% accuracy at either 20-minute or daily time scales. The ecosystem characteristics calculated in our study were consistent with independent measurements of the seasonal dynamics of a grassland site in Kazakhstan and with values published in the literature. These characteristics were also closely associated with daily changes in carbon dioxide. We concluded from our results that the mathematical equations we developed are useful for evaluating the effects of key ecosystem and climatic characteristics on carbon dioxide and energy dynamics in different ecosystems and years.

Technical Abstract: Canopy fluxes of CO2 and energy can be modeled with high fidelity using a small number of environmental variables and ecosystem parameters. Although these ecosystem parameters are critically important for modeling canopy fluxes, they typically are not measured with the same intensity as ecosystem fluxes. We developed an algorithm to estimate leaf area index (LAI), maximum carboxylation velocity (VCmax), the Ball-Berry parameter (m), and substrate-dependent ecosystem respiration rate (.A) by inverting a commonly used modeling paradigm of canopy CO2 and energy fluxes. To test this algorithm, fluxes of sensible heat (H), latent heat (LE), and CO2 (Fc) were measured with eddy covariance techniques in a pristine grassland-forb steppe site in northern Kazakhstan. We applied the algorithm to these data and identified ecosystem characteristics consistent with data across a time series of meteorological drivers from the Kazakhstan data. LAI was calculated by fitting the model to measured H+LE, Vcmax and .A were solved simultaneously by fitting the model to measured CO2 fluxes, and m was calculated by varying the partitioning of available energy between H and LE. Seasonal changes in LAI ranged from 2.0 to 2.4, Vcmax declined from 20 to 5 mol C m-2 s-1, respiration as a percentage of assimilation ranged from 0.5 to 0.75, and m varied from 17 to 24. Our results with the Kazakhstan data showed that LAI, Vcmax, ecosystem respiration, and m can be solved to accurately predict (R2=80 to 95%) carbon and energy fluxes with non-significant bias at 20-minute and daily time scales. The ecosystem characteristics calculated in our study were consistent with independent measurements of the seasonal dynamics of a shortgrass steppe in Kazakhstan and with values published in the literature. These characteristics were closely linked to mean daily fluxes of CO2, but were not dependent on the environmental drivers for the periods they were measured. We conclude that process-model inversion has potential for comparing CO 1 2 3 4 5 2 and energy fluxes among different ecosystems and years, and in providing important ecosystem parameters for evaluating climatic influences on CO2 and energy fluxes.

Last Modified: 4/23/2014
Footer Content Back to Top of Page