A Training Course on CO 2 Eddy Flux Data Analysis and Modeling Parameter Estimation: Practice Katherine Owen John Tenhunen Xiangming Xiao Institute of.

Slides:



Advertisements
Similar presentations
J. Ogée – N. Viovy – P. Friedlingstein – P. Ciais G. Krinner – N. deNoblet J. Polcher (IPSL) Evaluation of the global biospheric model ORCHIDEE against.
Advertisements

Why gap filling isn’t always easy Andrew Richardson University of New Hampshire Jena Gap Filling Workshop September 2006.
Reducing Canada's vulnerability to climate change - ESS Variation of land surface albedo and its simulation Shusen Wang Andrew Davidson Canada Centre for.
The C budget of Japan: Ecosystem Model (TsuBiMo) Y. YAMAGATA and G. ALEXANDROV Climate Change Research Project, National Institute for Environmental Studies,
Comprehensive evaluation of Leaf Area Index estimated by several method Comprehensive evaluation of Leaf Area Index estimated by several method ― LAI-2000,
The Earth’s Global Energy Balance
Plant Canopy Analysis Gaylon S. Campbell, Ph.D. Decagon Devices and Washington State University.
Water Vapor and Cloud Feedbacks Dennis L. Hartmann in collaboration with Mark Zelinka Department of Atmospheric Sciences University of Washington PCC Summer.
Light capture and Plant architecture determine Co-existence and Competitive Exclusion in Grassland Succession how grazing modifies succession Marinus J.A.
6/2/2015 A GAP-FILLING MODEL (GFM) FOR TOWER-BASED NET ECOSYSTEM PRODUCTIVITY MEASUREMENTS Zisheng Xing a, Charles P.-A. Bourque a, Fanrui Meng a, Roger.
Life: levels of organization – organism (individuals): any form of life – population: a group of interacting individuals of same species – community: populations.
PREFER 1 st Annual Review Meeting, 5-6 Dec 2013, Milano-Italy PREFER WP3.1 - Information Support to Preparedness/Prevention Phase Product: “Daily Fire.
Raw data Hz HH data submitted for synthesis Flux calculation, raw data filtering Additional filtering for footprint or instrument malfunctioning.
Outline Further Reading: Chapter 04 of the text book - global radiative energy balance - insolation and climatic regimes - composition of the atmosphere.
Visualizing Physical Geography Copyright © 2008 John Wiley and Sons Publishers Inc. Chapter 2 The Earth’s Global Energy Balance.
Remote Sensing Data Assimilation for a Prognostic Phenology Model How to define global-scale empirical parameters? Reto Stöckli 1,2
Unit of Biosystem Physics 1. O BJECTIVES To analyze impacts of grazing on carbon dioxide (CO 2 ) fluxes (F) exchanged by a meadow. 2. E XPERIMENTAL SITE.
An empirical model of stand GPP with LUE approach: analysis of eddy covariance data at several contrasting sites A. Mäkelä 1, M. Pulkkinen 1, P. Kolari.
Introduction To describe the dynamics of the global carbon cycle requires an accurate determination of the spatial and temporal distribution of photosynthetic.
Abstract Carbon Fluxes Across Four Land Use Types in New Hampshire Sean Z. Fogarty, Lucie C. Lepine, Andrew P. Ouimette — University of New Hampshire,
BIOME-BGC estimates fluxes and storage of energy, water, carbon, and nitrogen for the vegetation and soil components of terrestrial ecosystems. Model algorithms.
Long term weather and flux data: treatment of discontinuous data. Bart Kruijt, Wilma Jans, Cor Jacobs, Eddy Moors Loobos.
Enhanced Ecosystem Productivity in Cloudy or Aerosol-laden Conditions Xin Xi April 1, 2008.
Integrating Remote Sensing, Flux Measurements and Ecosystem Models Faith Ann Heinsch Numerical Terradynamic Simulation Group (NTSG) University of Montana.
Advanced Hydrology Lecture 1: Water Balance 1:30 pm, May 12, 2011 Lecture: Pat YEH Special-appointed Associate Professor, OKI Lab., IIS (Institute of Industrial.
A Training Course on CO2 Eddy Flux Data Analysis and Modeling
How Do Forests, Agriculture and Residential Neighborhoods Interact with Climate? Andrew Ouimette, Lucie Lepine, Mary Martin, Scott Ollinger Earth Systems.
Earth System Model. Beyond the boundary A mathematical representation of the many processes that make up our climate. Requires: –Knowledge of the physical.
Earth’s Energy Balance Complexity, climate change and human systems HCOL 185.
Earth’s Energy Balance 100 units of solar radiation hits the top of the atmosphere 100 units of solar radiation hits the top of the atmosphere Surface.
Integration of biosphere and atmosphere observations Yingping Wang 1, Gabriel Abramowitz 1, Rachel Law 1, Bernard Pak 1, Cathy Trudinger 1, Ian Enting.
A FIRST LOOK AT THE MODIS 8-DAY PSN DATA FOR 2001 MODIS Science Team Mtg 19 December 2001 Steven W. Running NTSG, Univ. of Montana.
The Soil-Plant-Atmosphere (SPA) Model Multilayer canopy and soils, 30 minute time-step Standard components –Radiative transfer scheme (sun/shade) –Soil.
Liebermann R 1, Kraft P 1, Houska T 1, Müller C 2,3, Haas E 4, Kraus D 4, Klatt S 4, Breuer L 1 1 Institute for Landscape Ecology and Resources Management,
A parametric and process- oriented view of the carbon system.
Water stress sites Site nameYear DE-Gri- Grillenburg2005 DE-Hai- Hainich2000,2001,2002,2003,2004,2005 ES-LMa-Las Majadas del Tietar2004,2005 DK-Sor-Soroe1996,1997,1998,1999,2000,2001,
The PILPS-C1 experiment Results of the first phase of the project Complementary simulation to be done Proposition for the future.
Energy Balance and Circulation Systems. 2 of 12 Importance Energy from Sun (Energy Budget) –“Drives” Earth’s Atmosphere  Creates Circulation Circulation.
CAMELS CCDAS A Bayesian approach and Metropolis Monte Carlo method to estimate parameters and uncertainties in ecosystem models from eddy-covariance data.
What is temperature? Measure of the average random kinetic energy of the molecules of a substance Physical property that determines the direction of heat.
How Do Forests, Agriculture and Residential Neighborhoods Interact with Climate? Andrew Ouimette, Lucie Lepine, Mary Martin, Scott Ollinger Earth Systems.
Landscape-level (Eddy Covariance) Measurement of CO 2 and Other Fluxes Measuring Components of Solar Radiation Close-up of Eddy Covariance Flux Sensors.
Biases in land surface models Yingping Wang CSIRO Marine and Atmospheric Research.
Goal: to understand carbon dynamics in montane forest regions by developing new methods for estimating carbon exchange at local to regional scales. Activities:
Recursive Calibration of Ecosystem Models Using Sequential Data Assimilation Mingshi Chen¹, Shuguang Liu¹, Larry L. Tieszen², and David Y. Hollinger 3.
Evapotranspiration Estimates over Canada based on Observed, GR2 and NARR forcings Korolevich, V., Fernandes, R., Wang, S., Simic, A., Gong, F. Natural.
Model-Data Synthesis of CO 2 Fluxes at Niwot Ridge, Colorado Bill Sacks, Dave Schimel NCAR Climate & Global Dynamics Division Russ Monson CU Boulder Rob.
Uncertainty in eddy covariance data and its relevance to gap filling David HollingerAndrew Richardson USDA Forest ServiceUniversity of New Hampshire Durham,
Using AmeriFlux Observations in the NACP Site-level Interim Synthesis Kevin Schaefer NACP Site Synthesis Team Flux Tower PIs Modeling Teams.
University of California, Berkeley
Towards a robust, generalizable non-linear regression gap filling algorithm (NLR_EM) Ankur R Desai – National Center for Atmospheric Research (NCAR) Boulder,
Xiangming Xiao Institute for the Study of Earth, Oceans and Space University of New Hampshire, USA The third LBA Science Conference, July 27, 2004, Brasilia,
Estimating the Reduction in Photosynthesis from Sapflow Data in a Throughfall Exclusion Experiment. Rosie Fisher 1, Mathew Williams 1, Patrick Meir 1,
Development of an Ensemble Gridded Hydrometeorological Forcing Dataset over the Contiguous United States Andrew J. Newman 1, Martyn P. Clark 1, Jason Craig.
Natural Environments: The Atmosphere
Assessing the climate impacts of land cover and land management using an eddy flux tower cluster in New England Earth Systems Research Center Institute.
Influence of tree crown parameters on the seasonal CO2-exchange of a pine forest in Brasschaat, Belgium. Jelle Hofman Promotor: Dr. Sebastiaan Luyssaert.
Comparison of GPP from Terra-MODIS and AmeriFlux Network Towers
Field Data & Instrumentation
Global Carbon Budget. Global Carbon Budget of the carbon dioxide emitted from anthropogenic sources) -Natural sinks of carbon dioxide are the land.
3-PG The Use of Physiological Principles in Predicting Forest Growth
Planetary albedo (a) is the average reflectivity of the Earth = 107/342  0.3 Earth’s global, annual mean energy balance.
Conghe Song Department of Geography University of North Carolina
Ecosystem Demography model version 2 (ED2)
Jianmin Zhang1, Timothy J. Griffis1 and John M. Baker2
Energy Balance and Circulation Systems
Comparing Simulated and Observed Gross Primary Productivity
Thermodynamics Atmosphere
Climate Control of Terrestrial Carbon Sequestration
Presentation transcript:

A Training Course on CO 2 Eddy Flux Data Analysis and Modeling Parameter Estimation: Practice Katherine Owen John Tenhunen Xiangming Xiao Institute of Geography and Natural Resources, Chinese Academy of Sciences, Beijing, China Institute for the Study of Earth, Oceans and Space, University of New Hampshire, USA Department of Plant Ecology, University of Bayreuth, Germany The Institute of Geography and Natural Resources, CAS, Beijing, China July 25, 2006

Practice: Parameter Estimation Many available methods. I will show: Hyperbolic Light Response Model Physiological Carboxylase-based Process Model both from Owen et al. 2006, Global Change Biology, submitted Outline 1. Inputs: data preparation 2. Running the program and potential problems 3. Outputs and potential problems 4. Examples

Practice: Parameter Estimation Inputs: Data preparation Input files for parameter estimation with the Hyperbolic Light Response Model (1): 1. Half-hourly meteorological and gas flux data (output file from flux partitioning and gap filling - “HE2001Processed.txt”)

Practice: Parameter Estimation Inputs: Data preparation Input files for parameter estimation with the Physiological Carboxylase-based Process Model (2): 1. Half-hourly meteorological and gas flux data (output file from flux partitioning and gap filling - “HE2001Processed.txt”) 2. Leaf Area Index (LAI) - either constant value or seasonally changing file (“HE2001.lai”) 3. Latitude & Longitude- to calculate sun angle 4. Physiological parameters - previously published values (eg. Leaf angle, Michaelis-Menton constant for oxygenation, Maximum rate of electron transport, etc.) for different vegetation types (“coni.gfx”)

Practice: Flux Partitioning & Gap Filling Inputs: Data preparation Review daily outputs from flux partitioning and gap filling - Are there problems? Do the results make sense? LAI file gfx file

Practice: Parameter Estimation Potential problems in running the program The Hyperbolic Light Response Model stops running: Fitter gets “stuck in a local minima” or can not converge on a solution due to high scatter in data (typical for winter or in periods with cut or harvests) - skip parameter estimation for the period The Physiological Carboxylase-based Process Model stops: Latitude & longitude were not defined LAI data file has a different number of days than meteorological and gas flux input file Fitter gets “stuck in a local minima” - skip parameter estimation for the period

Practice: Parameter Estimation How the Hyperbolic Light Response Model (1) works Use PPFD & un-gap filled NEE and non-linear least trimmed squares regression technique to iteratively calculate the , , and  for 10 day periods Set initial random values of , , and  Read in half- hourly meteorological & flux input file Output: optimal , , and  parameters for 10 day periods

Practice: Parameter Estimation Hyperbolic Light Response Model (1) Outputs Parameters:  Standard error of  and  Slope, intercept & r 2 of observed NEE vs. calculated NEE

Practice: Parameter Estimation: Outputs & Potential Problems: Hyperbolic Light Response Model (1) “abnormal”  results can be due to: Winter periods with little light response Strong scatter in NEE & PPFD relationship (due to cut or harvest) Poor starting values of  - results stuck in local minima We chose to eliminate “abnormal” results with:relative standard error > 0.6,  > 0.17,  > 100,  > 15

Practice: Parameter Estimation: How the Physiological Carboxylase-based Process Model (2) works Define LAI: constant or seasonally changing from file Calculate static geometric attributes of the canopy (diffuse & direct radiation on leaf surfaces-sunlit & shaded) Iteratively calculate energy balance throughout canopy (leaf temperature, incoming and outgoing shortwave & longwave radiation, estimated GPP) Define latitude, longitude, vegetation type gfx input file Read in half- hourly meteo & flux input file Output: (Vc uptake2* and alpha) or (Vc uptake1* ) parameters for 10 day periods

Practice: Parameter Estimation Carboxylase-based Process Model (2) Outputs Parameters: Vc uptake & alpha Standard error of Vc uptake & alpha Slope, intercept & r 2 of observed GPP vs. calculated GPP

Practice: Parameter Estimation Outputs & Potential Problems Carboxylase-based Process Model (2) “Abnormal” Vc uptake & alpha results can be due to: LAI of 0 Poor estimates of seasonal LAI harvests or cuts scatter or errors in data We chose to eliminate “abnormal” results with:relative standard error > 0.6, Vc uptake > 350, alpha > 0.17 Easter Bush, UK, 2005, LAI too low

Hesse, France Deciduous Beech Forest Fagus sylvatica experienced drought in 2003 Practice: Parameter Estimation Examples: Hesse, France

Practice: Parameter Estimation Examples: Hesse, France

Takayama, Japan Mountain Deciduous Forest Quercus crispula Blume, Betula ermanii Cham., Betula platyphylla Sukatchev var. japonica Hara Storm damage in 2004 Practice: Parameter Estimation Examples: Takayama, Japan

Practice: Parameter Estimation Examples: Takayama, Japan

Barrow, Alaska, USA Tundra Carex aquatilis spp. Stans, Eriophorum angustifolium, Dupontia fisheri, Poa artica Practice: Parameter Estimation Examples: Barrow, Alaska, USA

Practice: Parameter Estimation Examples: Barrow, Alaska, USA

Grillenburg, Germany Grassland Festuca pratensis, Alopecurus pratensis, Phleum pratensis Cut 2 or 3 times per year No grazing experienced drought in 2003 Practice: Parameter Estimation Examples: Grillenburg, Germany

Practice: Parameter Estimation Examples: Grillenburg, Germany