Accurate scaling requires mechanistic understanding: using experimental manipulations and tractable models as a testing ground for improving global land.

Slides:



Advertisements
Similar presentations
Stoichiometry of Forest Nutrient Limitation Melany Fisk, Miami University.
Advertisements

Can microbial functional traits predict the response and resilience of decomposition to global change? Steve Allison UC Irvine Ecology and Evolutionary.
Contrasting tissue strategies explain functional beta diversity in Amazonian trees C. Fortunel, C.E.T. Paine, N. Kraft, P.V.A. Fine, C. Baraloto*
Modelling Australian Tropical Savanna Peter Isaac 1, Jason Beringer 1, Lindsay Hutley 2 and Stephen Wood 1 1 School of Geography and Environmental Science,
Peter S. Curtis Department of Evolution, Ecology, and Organismal Biology The Ohio State University Managing Great Lakes Forests for Climate Change Mitigation.
Land Carbon Sink and Nitrogen Regulation under Elevated CO 2 : Central Tendency Yiqi Luo University of Oklahoma NCEAS Working group: William Currie, Jeffrey.
Data-model assimilation for manipulative experiments Dr. Yiqi Luo Botany and microbiology department University of Oklahoma, USA.
Functional traits, trade-offs and community structure in phytoplankton and other microbes Elena Litchman, Christopher Klausmeier and Kyle Edwards Michigan.
Light capture and Plant architecture determine Co-existence and Competitive Exclusion in Grassland Succession how grazing modifies succession Marinus J.A.
Soil-mediated effects of a CO 2 gradient on grassland productivity: Interactions with resources and species change. Philip A. Fay USDA-ARS Grassland, Soil,
Sensitivity of water-optimal root depth to precipitation constant rain frequency, variable mean depth constant mean depth, variable frequency Multiple.
1 Mathematical Models of Plant Growth for Applications in Agriculture, Forestry and Ecology Paul-Henry Cournède Applied Maths and Systems, Ecole Centrale.
Null models and observed patterns of native and exotic diversity: Does native richness repel invasion? Rebecca L. Brown, 1,2 Jason D. Fridley, 1 and John.
Assessing Douglas-fir water-use history using stable isotope ( 13 C and 18 O) in tree rings: principles and potential J. Renée Brooks Western Ecology Division,
Climate Change and Douglas-fir Dave Spittlehouse, Research Branch, BC Min. Forest and Range, Victoria.
Source: IPCC 1.Reduced Biodiversity (rapid change) 2.Sea level rise and coastal flooding (melting ice and thermal expansion) 3.Expansion of tropical.
Modern and Future Forest Ecosystems Richard J. Norby Environmental Sciences Division Oak Ridge National Laboratory Snowbird, Utah December 8, 2001.
Plant material: 8-year-old saplings of European beech (Fagus sylvatica L.) and Norway spruce (Picea abies (L.) Karsten) were exposed for three growing.
Forest Sensitivity to Elevated Atmospheric CO 2 and its Relevance to Carbon Management Richard J. Norby Oak Ridge National Laboratory Aspen Global Change.
OUR Ecological Footprint …. Ch 20 Community Ecology: Species Abundance + Diversity.
Ph. Wipfler and G.Deckmyn Kranzberg Forest Experiment : upscaling to the forest. From the empirical approach to the mechanistic simulation of ozone effects.
Statistical averaging
6 CO H 2 O --- LIGHT + chlorophyll ---> C 6 H 12 O O H 2 O GLOBE Carbon Cycle Plant-A-Plant: Hands-on Photosynthesis Experiments What.
FACE Network * Presented by:Bob Nowak Stan Smith Assistance from:Hormoz BassiriRad Terri Charlet Dave Ellsworth Dave Evans Lynn Fenstermaker Eric Knight.
Integrating Forages into Multi-Functional Landscapes: Enhanced Soil Health and Ecosystem Service Opportunities Douglas L. Karlen USDA-ARS Presented at.
Plant physiological responses to precipitation in the Amazon forest, an isotopic approach Universidade de São Paulo: Jean Pierre Ometto; Luiz Martinelli;
Modeling climate change impacts on forest productivity with PnET-CN Emily Peters, Kirk Wythers, Peter Reich NE Landscape Plan Update May 17, 2012.
Is It True? At What Scale? What Is The Mechanism? Can It Be Managed? 150 Is The New 80: Continuing Carbon Storage In Aging Great Lakes Forests UMBS Forest.
A process-based, terrestrial biosphere model of ecosystem dynamics (Hybrid v. 3.0) A. D. Friend, A.K. Stevens, R.G. Knox, M.G.R. Cannell. Ecological Modelling.
1 UIUC ATMOS 397G Biogeochemical Cycles and Global Change Lecture 15: Biosphere and Nutrients Don Wuebbles Department of Atmospheric Sciences University.
BIOME-BGC estimates fluxes and storage of energy, water, carbon, and nitrogen for the vegetation and soil components of terrestrial ecosystems. Model algorithms.
How are physiological constraints which govern biomass scaling and vascular architecture maintained in managed orchard systems? - “a tree is a tree” -
Methods Model. The TECOS model is used as forward model to simulate carbon transfer among the carbon pools (Fig.1). In the model, ecosystem is simplified.
The Fate of the Land Carbon Sink Stephen W. Pacala Director, Princeton Environmental Institute Petrie Professor of Ecology.
PHOTO BY S. MANZONI Eco-hydrological optimality to link water use and carbon gains by plants Manzoni S. 1,2, G. Vico 2, S. Palmroth 3, G. Katul 3,4, and.
Transpiration. the release of water vapor by plants to the atmosphere “is not an essential or an active physiological function of plants” a largely passive.
Hemiparasitism: a way station to holoparasitism or an evolutionary stable strategy? Prof. Joseph E. Armstrong Illinois State University Behavior, Evolution,
By: Karl Philippoff Major: Earth Sciences
Introduction: Globally, atmospheric concentrations of CO 2 are rising, and are expected to increase forest productivity and carbon storage. However, forest.
Forest response to elevated [CO 2 ] depends on the potential for an ecosystem to meet productivity and carbon storage demands. If soil N is limiting, PNL.
Extension of the forest ecosystem simulation model FORECAST: incorporating mountain pine beetle, fire, climate change, and wildlife Hamish Kimmins, Kim.
Sharon Stanton & FIA National Indicator Leads RECOMMENDATIONS FOR ENHANCED FOREST INDICATORS.
Background The extent to which terrestrial ecosystems are able to store excess carbon is debated in literature. Soils accumulate two thirds of all carbon.
Nitrogen-use efficiency of a sweetgum forest in elevated CO 2 Richard J. Norby 1 and Colleen M. Iversen 2 1 Oak Ridge National Laboratory, Oak Ridge, TN;
ChEAS 2005 D.S. Mackay June 1-2, 2005 Reference canopy conductance through space and time: Unifying properties and their conceptual basis D. Scott Mackay.
Welcome Grant from National Science Foundation: Fire, Atmospheric pCO 2, and Climate as Alternative Primary Controls of C 4 -Grass Abundance: The Late-Quaternary.
Effects of Intensive Fertilization on the Growth of Interior Spruce Presentation to: Interior Fertilization Working Group February 5/13 (revised March.
Mortality over Time Population Density Declines through Mortality.
Response of Luzula arctica and Luzula confusa to warming in Barrow and Atqasuk, Alaska Kelseyann Kremers and Dr. Robert D. Hollister Grand Valley State.
300 Years of NEP Caused By Land Use, CO 2 Fertilization and Climate Change According to LM3 Shevliakova, Malyshev, Hurtt and Pacala.
Ecology 8310 Population (and Community) Ecology The effects of diversity Background Tilman and Downing 1994 Species vs. functional diversity Foodwebs (instead.
Sirius wheat simulation model: development and applications Mikhail A. Semenov Rothamsted Research, UK IT in Agriculture & Rural Development, Debrecen,
MODELLING CARBON FLOWS IN CROP AND SOIL Krisztina R. Végh.
Ecosystem carbon storage capacity as affected by disturbance regimes: a general theoretical model Introduction Disturbances can profoundly affect ecosystem.
Ecology & Abiotic Factors Ecosystems Consist of living things, called organisms, and the physical place they live 12.1 Abiotic and Biotic Factors Examples:
The GLOBE-Carbon Cycle project joins NASA carbon cycle science with the International GLOBE Education program to bring the most cutting edge research and.
Diversity Productivity Relationships Species Richness Seminar October 21, 2003.
Production.
Functional Traits and Niche-based tree community assembly in an Amazonian Forest Kraft et al
Yan Sun Advisor: Professor Shilong Piao College of Urban and Environment Sciences, Peking University PKU-LSCE meeting, 15 MAY 2014 Water-use Efficiency.
Center for Advanced Forestry Systems 2014 Meeting Do Below Ground Processes Explain Differences in Growth, Productivity and Carrying Capacity of Loblolly.
대기 중 CO 2 변화에 따른 토양 CO 2 방출량 변화 ( DYNAMICS OF SOIL CO 2 EFFLUX UNDER VARYING ATMOSPHERIC CO 2 CONCENTRATIONS ) Dohyoung Kim Duke University July
Old and Not-So-Old Research Progress/Plans for Ankur Desai Penn State University, Department of Meteorology Cheas 2003 Meeting, Woodruff, WI, 29 June –
3-PG The Use of Physiological Principles in Predicting Forest Growth
Group Matyssek Introduction to the Kranzberg site,
Ecosystem Demography model version 2 (ED2)
Finding efficient management policies for forest plantations through simulation Models and Simulation Project
AGU meeting 2014 LM3-PPA: scaling from individuals to ecosystems with height-structured competition for light Ensheng Weng1, Sergey Malyshev1, Jeremy Lichstein2,
By: Paul A. Pellissier, Scott V. Ollinger, Lucie C. Lepine
Diversity and function of terrestrial ecosystems under global changes
Presentation transcript:

Accurate scaling requires mechanistic understanding: using experimental manipulations and tractable models as a testing ground for improving global land models Caroline Farrior, Princeton University CLIMMANI/INTERFACE Conference, Czech Republic 5 June 2013

CO 2 fertilization experiments: Leaf level effects consistent Ainsworth and Long (2005) meta-analysis of 15 years of FACE experiments Light saturated CO 2 uptake (photosynthetic efficiency) Instantaneous transpiration efficiency (leaf-level water-use efficiency) Duke FACE

Stand level predictions from leaf level responses. Leaf level response: CO 2  Increased leaf-level water use efficiency (WUE) Increased WUE only increases productivity if plants are water limited. Stand-level prediction: Places or years with greater water stress should have stronger responses to enhanced CO 2.

Extrapolation of leaf level effects does not explain FACE (Free Air CO 2 Enrichment) results Duke FACE, McCarthy et al Water availability Ambient CO 2 Enhanced CO 2 Water availability CO 2 effect Similar results in other FACE experiments (Norby et al (review)) Ambient CO 2 Enhanced CO 2 CO 2 effect

What are we missing?

Fine roots (R) Leaves (L) Woody biomass (W) ~1 year ~100 years ~ 2 years Changes in allocation patterns have large effects on carbon storage Residence time Individual allocation patterns

Individual trees Leaves Woody biomass Fine roots Simplified plant physiology Z, W, S all grow allometrically with diameter. Diameter growth rate = f(resource availability, l, r )

CO 2 Water Nitrogen Water N Leaves Woody biomass Fine roots Simplified plant physiology Nitrogen uptake Water uptake Carbon assimilation Water-saturated plant Water-limited plant

Simplified plant physiology: carbon conservation Tissue respiration, maintenance and growth Investment in reproduction Water uptake Carbon assimilation Water-saturated plant Water-limited plant Nitrogen uptake

Sparsely rooted plants Competition for water and nitrogen. Uptake depends on community root density Nitrogen Water Densely rooted plants

Competition for light: forest dynamics model Purves et al. 2007, Strigul et al Canopy individuals in full sun Understory individuals in the shade The perfect plasticity approximation This simplicity allows analytical predictions Individuals are good at foraging horizontally for light

Light level constant. Nitrogen mineralization rate constant. Rainfall variable. Environmental conditions Day of the growing season Rainfall Rainfall while water limited Time in water saturation Note: This abstraction is analogous to a model with stochastic rainfall (Farrior, Rodriguez-Iturbe, Pacala in prep). Water saturation level

Individual properties Growth rates = f(allocation, resource availability) Mortality Fecundity Stand level properties Height of canopy closure (Z*) Expected lifetime reproductive success (LRS, fitness) PPA Population dynamics

Allocation strategy (e.g.: allocation to fine roots) Allocation strategy (e.g.: allocation to fine roots) 1 Resident strategy Competitive dominant/ Evolutionarily stable strategy (ESS) Successful invaders Predicting the dominant allocation strategy: Evolutionarily Stable Strategy (ESS) Expected lifetime reproductive success (LRS) of invader in monoculture of the resident ESS – a strategy that when in monoculture prevents invasion by all other strategies

Nitrogen-limited plants Competitive (ESS) allocation strategies Dybzinski et al. AmNat 2011 N

Water-limited plants Competitive (ESS) allocation strategies Time in water saturation Water available during water limitation Farrior et al. AmNat 2013 W

Dybzinski et al Farrior et al Nitrogen limitation Water limitation Comparisons to data – Fluxnet sites across the globe

Application to CO 2 fertilization

ESS allocation example: N-limited plant N Root cost (gC/year) Competitive dominant (ESS) Leaf productivity (gC/year) More roots Holds leaves more costly than they are worth Less roots Missing productive leaves Competitive, nitrogen-limited plants invest in fine roots at a level that cancels the productivity of the least productive leaf.

LRS of invader in monoculture of the resident. +CO 2 ESSNew ESS Plant response Resident strategy Invading strategy Enhanced [CO 2 ] perturbs the environment, changing the competitive landscape and the ESS

+CO 2 (photosynthetic efficiency) New ESS Immediate Plant Response Plant level responses to enhanced [CO 2 ]: N-limited plants ESS Root cost (gC/year) Leaf benefit (gC/year) N Dybzinski et al. In Prep CO2 fertilization in nitrogen-limited plants promotes growth of fine-root and woody biomass.

ESS New ESS If plants are water limited, when CO 2 is added, if there is a productivity response, it is due to the increase in water use efficiency. With this increase, competitive plants increase fine-root biomass but there is no increase in biomass allocated to wood (yellow – brown area). New ESS Plant level responses to enhanced [CO 2 ]: Water-limited plants +CO 2 (leaf-level water use efficiency) Immediate Plant Response W CO 2 fertilization in water-limited plants promotes growth of fine-roots biomass without increases in tree growth. Root cost (gC/year) Leaf benefit (gC/year) Farrior et al. 2013

Enhanced CO 2 for water and nitrogen limited plants lead to opposite effects on carbon sinks.

36, 32 species plots planted in 1994 (Cedar Creek, Dave Tilman) 4 years of factorial additions – Nitrogen (ambient, +7g/m 2 /yr +14g/m 2 /yr) – Water (ambient, ~double) Resource addition experiment Fine roots Coarse rootsFarrior et al. In Press Ecology

Leaves increase with N Roots increase with water addition but only at low N Roots decrease with N addition but only at high water * * Simple experiment yields some confusing results * Significant effect of the water treatment Farrior et al. In Press Ecology

Grassland model of competition for light, water, and nitrogen Individual plant CO 2 Water Nitrogen Allocation to reproduction, Measure of fitness Farrior et al. In Press Ecology

Nitrogen ESS +N New ESSPlant Response Root investment decreases with nitrogen addition because marginal returns of nitrogen uptake are negative. Effect of nitrogen addition on biomass allocation Root cost (gC/year) Leaf productivity (gC/year) N

Water ESSNew ESS Plant Response + water during water limitation Root cost Root investment increases with water addition because marginal returns of water uptake are constant. Effect of water addition on allocation Water-limited leaf productivity W

ESS root investment = + time in water saturationtime in water limitation water ESSnitrogen ESS * * ESS allocation to fine roots: a weighted average Explicit interaction between water and nitrogen  Nitrogen additions should have a greater effect at high water.  Effect of water additions should decrease with nitrogen level.

ESS allocation to fine roots: a weighted average * * Effect of water additions decrease with nitrogen additions because the nitrogen limitation strategy becomes more important with water additions.

Experimental additions of nitrogen and water results consistent with a model where nitrogen-limited and water-limited plants respond in opposing ways to CO 2 fertilization.

Height-structured competition for light in a global land model Weng et al. In prep Shevliakova et al LM3V LM3/PPA

Predicting successional dynamics Weng et al. In prep Model Data

Current directions – Using ESS allocation strategies into forest tiles. – Including realistic rainfall regime (Farrior, Rodriguez- Iturbe, Pacala In Prep) To infinite diversity in a land model

In summary * * If possible, tractable models can make it easier to determine and test basic mechanisms and their importance. Climate crisis demanding of a young science Must make and improve predictive models At the same time, important to rebuild/reinvent the basis of these models. Scaling from small plots to landscapes and regions: what works, and what doesn't?

Collaborators Steve Pacala Ray Dybzinksi Simon Levin Dave Tilman Peter Reich Ensheng Wang Elena Shevliakova Sergey Malyshev Jeremy Lichstein Funding Sources Princeton Carbon Mitigation Initiative USDA Forest Service NSF Graduate Fellowship Legislative-Citizen Commission on Minnesota Resources. Acknowledgements