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.

Slides:



Advertisements
Similar presentations
Plant Canopies and Carbon Dioxide Flux At night: - flux directed from canopy to the atmosphere - respiration from leaves, plant roots, soil Daytime:-
Advertisements

Why gap filling isn’t always easy Andrew Richardson University of New Hampshire Jena Gap Filling Workshop September 2006.
The mechanism of productivity formation of alpine meadow ecosystem Dr Xinquan Zhao Northwest Plateau Institute of Biology, The Chinese Academy of Sciences,
A NEW LAND-LAKE SENSOR NETWORK FOR MEASURING GREENHOUSE GAS, WATER, AND ENERGY EXCHANGES: USE IN EDUCATION AND OUTREACH 1. Introduction Stepien, Carol.
The C budget of Japan: Ecosystem Model (TsuBiMo) Y. YAMAGATA and G. ALEXANDROV Climate Change Research Project, National Institute for Environmental Studies,
Global change impact on ecosystems Reinhart Ceulemans and Ivan Nijs University of Antwerp, Department of Biology (UA-PLECO)
Soil CO 2 Efflux from a Subalpine Catchment Diego A. Riveros-Iregui 1, Brian L. McGlynn 1, Vincent J. Pacific 1, Howard E. Epstein 2, Daniel L. Welsch,
Carbon flux at the scale up field of GLBRC. The Eddy Covariance cluster towers Terenzio Zenone 1 Jiquan Chen 1 Burkhard Wilske 1 and Mike Deal 1 Kevin.
Jun-Aug/annual mean T precip.sum (degC) (mm) / / / / / / / /810 Jun-Aug/annual mean.
Individual organism: How do structure, physiology, and behavior lead to the individual’s survival and reproduction? Population: What determines the number.
1.The effects of reduced tillage resulted in lower microbial R during the interval between fall plowing and the onset of winter. Carbon gain from the oats.
Carbon sequestration in China’s ecosystems, Jingyun Fang Department of Ecology Peking University Feb. 14, 2008.
PLATE 9-1 Tropical forests have the highest annual NPPs of any terrestrial ecosystem.
The Flow of Energy: Primary Production
OC211(OA211) Phytoplankton & Primary Production Dr Purdie SOC (566/18) LECTURE 6 Week 6 (i) Photosynthesis & Light (ii) Critical.
Comparison of Carbon Fluxes Over Three Boreal Black Spruce Forests in Canada O. Bergeron §, H.A. Margolis §, T.A. Black †, C. Coursolle §, A.L. Dunn ф,
Trends in Terrestrial Carbon Sinks Driven by Hydroclimatic Change since 1948: Data-Driven Analysis using FLUXNET Trends in Terrestrial Carbon Sinks Driven.
Titel Gap Filling of CO 2 Fluxes of Frequently Cut Grassland Christof Ammann Agroscope ART Federal Research Station, Zürich Gap Filling Comparison Workshop,
Optimising ORCHIDEE simulations at tropical sites Hans Verbeeck LSM/FLUXNET meeting June 2008, Edinburgh LSCE, Laboratoire des Sciences du Climat et de.
Paul R. Moorcroft David Medvigy, Stephen Wofsy, J. William Munger, M. Dietze Harvard University Developing a predictive science of the biosphere.
Introduction Stomatal conductance regulates the rates of several necessary processes in plants including transpiration, carbon dioxide assimilation, and.
Ecosystem ecology studies the flow of energy and materials through organisms and the physical environment as an integrated system. a population reproduction.
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,
Nelius Foley, Matteo Sottocornola, Paul Leahy, Valerie Rondeau, Ger Kiely Hydrology, Micrometeorology and Climate Change University College Cork, IrelandEnvironmental.
OUR Ecological Footprint The hierarchical nature and processes of different levels of ecological systems:
Enhanced Ecosystem Productivity in Cloudy or Aerosol-laden Conditions Xin Xi April 1, 2008.
Carbon Sequestration in US Midwest Region and GLBRC: Lessons from the flux towers Terenzio Zenone 1 Jiquan Chen 1 Mike Deal 1 Burkhard Wilske 1 Poonam.
Seasonal and Inter-Annual Variability in Net Ecosystem CO 2 Exchange at Six Forest Flux Sites in Japan Y. Ohtani* 1, Y. Yasuda* 1, Y. Mizoguchi* 1, T.
Reducing Canada's vulnerability to climate change - ESS J28 Earth Science for National Action on Climate Change Canada Water Accounts AET estimates for.
Unit of Biosystem Physics Jérôme Elisabeth 1, Beckers Yves 2, Bodson Bernard 3, Moureaux Christine 3, Aubinet Marc 1 1 University of Liege, Gembloux Agro-Bio.
Xin Xi March 13, Basis 1. Photosynthesis (gross photosynthesis minus photorespiration) C3/C4/ CAM (Crassulacean Acid Metabolism) 2. Ecosystem Respiration.
New tool for CO 2 flux partitioning with soil chamber flux implementation as a solution for site in topographically complex terrain Šigut, L., Mammarella,
Potential impact of climate change on growth and wood quality in white spruce Christophe ANDALO 1,2, Jean BEAULIEU 1 & Jean BOUSQUET 2 1 Natural Resources.
The Flow of Energy: Primary Production What we need to learn: What is primary production, and how is it measured? How are primary and ecosystem productivity.
Ecosystem component Activity 1.6 Grasslands and wetlands Jean-François Soussana Katja Klumpp, Nicolas Vuichard INRA, Clermont-Ferrand, France CarboEurope,
Flux observation: Integrating fluxes derived from ground station and satellite remote sensing 王鹤松 Hesong Wang Institute of atmospheric physics, Chinese.
Application of the ORCHIDEE global vegetation model to evaluate biomass and soil carbon stocks of Qinghai-Tibetan grasslands Tan Kun.
U.S. Department of the Interior U.S. Geological Survey Normalized Difference Vegetation Index for Restoration Monitoring Bruce K. Wylie 1, Steve Boyte.
Carbon balance in a heterogeneous cutover bog in the Jura Mountains. Estelle Bortoluzzi, Daniel Epron, Daniel Gilbert, Alexandre Buttler.
NEW TRANSFER FUNCTIONS FOR CORRECTING EDDY COVARIANCE FLUXES OF WATER VAPOUR Unit of Biosystem Physics – Gembloux Agricultural University – Belgium A.
Variations in Continental Terrestrial Primary Production, Evapotranspiration and Disturbance Faith Ann Heinsch, Maosheng Zhao, Qiaozhen Mu, David Mildrexler,
Landscape-level (Eddy Covariance) Measurement of CO 2 and Other Fluxes Measuring Components of Solar Radiation Close-up of Eddy Covariance Flux Sensors.
This research was funded by The FRS-FNRS, Belgium October October 2012 Contact Person: Goffin Stéphanie- University of Liege – Gembloux Agro-Bio.
Effects of parent material and land use on soil phosphorus forms in Southern Belgium Renneson 1 M., Dufey 2 J., Bock 1 L. and Colinet 1 G. 1 University.
MonthDayTopic Nov.8Individuals to populations 10Holiday! 13Populations to communities 15Community patterns 17Ecosystems 20Film-1 st showing 22Film-2 nd.
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.
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.
(a) (b) Fig. S1 Monthly rainfall (mm mo -1 ) measured at (a) TNF from 2002 to 2004 and (b) CAX from 2001 to 2008 (red line and symbols). The black line.
Gap Filling Comparison Workshop, September 18-20, 2006, Jena, Germany Corinna Rebmann Olaf Kolle Max-Planck-Institute for Biogeochemistry Jena, Germany.
1 Carbon Dioxide in the Atmosphere: CO 2 - Parametric Analysis - Differential Equations Chris P. Tsokos Department of Mathematics and Statistics University.
R ESULTS Management and development of the crop Seasonal course of the fluxes R ESULTS Management and development of the crop Seasonal course of the fluxes.
Whats new with MODIS NPP and GPP MODIS/VIIRS Science Team Meeting May 20, 2015 Steven W. Running Numerical Terradynamic Simulation Group College of Forestry.
Seasonal variations in C and H 2 O cycling of a tropical transitional forest George L Vourlitis 1, Nicolau Priante Filho 2, José de Souza Nogueira 2, Luciana.
Production.
Unit of Biosystem Physics Jérôme Elisabeth 1, Beckers Yves 2, Beekkerk van Ruth Joran 1, Bodson Bernard 3, Dumortier Pierre 1, Moureaux Christine 3, Aubinet.
Figure 10. Improvement in landscape resolution that the new 250-meter MODIS (Moderate Resolution Imaging Spectroradiometer) measurement of gross primary.
Influence of tree crown parameters on the seasonal CO2-exchange of a pine forest in Brasschaat, Belgium. Jelle Hofman Promotor: Dr. Sebastiaan Luyssaert.
Taylor Conte1, Elizabeth Burakowski2
CARBON, WATER, LAND USE & CLIMATE
Conclusions on methanol controls
Colin Michel1, C. Amelynck3, M. Aubinet1, A. Bachy1, P. Delaplace2, A
Jianmin Zhang1, Timothy J. Griffis1 and John M. Baker2
By: Paul A. Pellissier, Scott V. Ollinger, Lucie C. Lepine
What is Productivity? Amount of solar energy provided to an ecosystem
Comparing Simulated and Observed Gross Primary Productivity
Climate Change and Agriculture
Climate Control of Terrestrial Carbon Sequestration
Enhanced seasonal CO2 exchange caused by amplified plant productivity in northern ecosystems by Matthias Forkel, Nuno Carvalhais, Christian Rödenbeck,
Presentation transcript:

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 Situation: Belgium, Dorinne Terrestrial Observatory (l50° 18’ 44’’ N; 4° 58’ 07’’ E; 248 m asl.). Climate: temperate oceanic. Mean annual temperature: 10°C. Annual precipitation: 800 mm. Type: permanent grassland. Surface: 4.2 ha. Slope: moderate (1 to 2 %). Ruminant livestock system: intensive (≈ 2 LU ha -1 ). Breed of cattle: Belgian Blue. 3. M ETHODS 3.1 Long term and short term effects of grazing Long term effects: result from biomass consumption by the cattle and from the cattle effluents that modify assimilation and respiration fluxes. This could only be quantified by comparing fluxes before and after grazing periods. Short term effects: due to cattle respiration that is a part of Total Ecosystem Respiration (TER) and should be measured during its presence in the field Data sets Data set I: long term effects  2 complete years of eddy covariance measurements made at DTO: 12 May 2010 – 12 May 2012 (data from vegetative periods). Data set II: short term effects  livestock confinement experiments (summer 2012). Impacts of grazing on carbon dioxide fluxes of an intensively grazed grassland in Belgium Jérôme Elisabeth 1, Beckers Yves 2, Bodson Bernard 3, Dumortier Pierre 1, Moureaux Christine 3, Aubinet Marc 1 1 University of Liege, Gembloux Agro-Bio Tech, Unit of Biosystem Physics, 8 Avenue de la Faculté, B-5030 Gembloux, Belgium 2 University of Liege, Gembloux Agro-Bio Tech, Animal Science Unit, 2 Passage des Déportés, B-5030 Gembloux, Belgium 3 University of Liege, Gembloux Agro-Bio Tech, Crops Science Unit, 2 Passage des Déportés, B-5030 Gembloux, Belgium. This research was funded by The « Direction Generale opérationnelle de l’Agriculture, des Ressources naturelles et de l’Environnement - Région Wallonne » Project n° D , January December 2013 Contact Person: Jérôme Elisabeth - University of Liege – Gembloux Agro-Bio Tech (GxABT) - Unit of Biosystem Physics, 8 Avenue de la Faculté Gembloux - Belgium Tel : +32 (0) Fax : +32 (0) R ESULTS 4.1 Long term effects 5. C ONCLUSIONS We found a long term and a short term impact of grazing on CO 2 fluxes exchanged by a meadow. 3.3 Long term effects Analyzing and comparing fluxes between grazing and non grazing periods  data set I divided into different intervals corresponding to grazing or non-grazing periods. 1. Response of cumulated gap filled F CO2 calculated for each period to grazing intensity  could be blurred by the flux variability due to responses to meteorological drivers. 2. Response of differences between parameters of interest of the last and the first 5-day window of each grazing or non-grazing period to grazing intensity. Parameters of interest were obtained by fitting a 5-day window F CO2 - PPFD relationship on daytime eddy covariance measurements: 3.4 Short term effects Figure 1: Schematic representation of Dorinne Terrestrial Observatory. Localization of the micro- meteorological station and eddy- covariance set-up. Black area represents the confinement zone used to analyze short term impacts of grazing on carbon dioxide fluxes. GPP max (µmol m -2 s -1 ) = gross primary productivity at light saturation; R d (µmol m -2 s -1 ) = dark respiration; α (µmol µmol -1 ) = apparent quantum efficiency. R d,10 (µmol m -2 s -1 ) = dark respiration normalized at 10°C; T ref = reference temperature set to 10°C; T S (°C) = average soil temperature at 2 cm depth for the considered 5- day window; E 0 (K) = respiration sensitivity to temperature. E 0 values were deduced from the annual response of nighttime half-hourly filtered CO 2 fluxes to T S (353 K and 359 K for the 5 days windows in Year 1 and Year 2, respectively). Figure 3: a) Nighttime CO 2 flux evolution and b) daytime CO 2 flux response to radiation of two successive days with or without cattle for confinement experiment II. Average stocking rate for day with cattle was 27 livestock unit ha -1. Data set II was filtered for u * and stationarity and environmental conditions were equivalent between the two successive days. Errors bars are the random error of measurement. Table 1: Results of confinement experiments. R l is the livestock respiration. Figure 2: a) Cumulated carbon dioxide flux (F CO2 ), and b), c), responses of difference of the last and the first 5 days window day fitting regression parameters for specific periods to grazing intensity. a) b) c) a) b) 4.2 Short term effects Figure 2a: cumulated F CO2 ↑ with grazing intensity but the trend was not significant  response blurred by responses to other driving variables (radiation, soil temperature, drought, etc.). Figure 2b: ∆GPP max significantly ↓ with grazing intensity: above-ground biomass ↓ due to defoliation by grazing  ↓ plant assimilation. Figure 2c: No significant impact of grazing intensity on R d,10 : net impacts of grazing on R d,10 less important than those of climate and seasonality  due to the combination of contradictory effects: ↓ autotrophic plant respiration and ↑ heterotrophic respiration.  Discrimination of indirect impacts of grazing on CO 2 fluxes from flux response to climate only possible after gathering and treating two years of measurements taken under various climatic conditions. Figure 3, Table 1: Nighttime and daytime fluxes always higher with cattle on the plot than without. Confinement experiment: 2 days 1. First day: cattle (27 LU ha -1 ) confined in the main wind direction area of the eddy covariance set-up (1.76 ha); 2. Second day: removed from the plot. 3 independent estimations of livestock respiration (R l ): 1. Nighttime eddy covariance measurements; 2. Daytime eddy covariance measurements;  Comparison of filtered half-hourly data made at 24h interval, in presence of cattle or not (considering equivalent environmental conditions: air temperature within 3°C - wind speed within 3 m s -1 - radiation within 75 µmol m -2 s -1 - wind direction within confinement area). 3. Carbon intake measurements. Table 1: -R l estimations around 2 kg C LU -1 d -1 and not significantly different between the two experiments and data sets.  confidence in estimates based on F CO2 measurements. -R l estimations > HM measurements confirms partially R l estimations > F CO2 measurements. Short term impacts Increase of CO 2 fluxes in presence of cattle. Could be quantified and observed only thanks to confinement experiment. Confinement experiment: only way to study short term impacts of grazing. Long term impacts Decrease of photosynthetic capacity due to cattle consumption of vegetation. Discrimination from flux response to climate only after treating two years of measurements.