Carbon cycle assessment Patricia Cadule Jean-Louis Dufresne Institut Pierre Simon Laplace, Paris. CCI-CMUG, 27 May 2015.

Slides:



Advertisements
Similar presentations
Emissions in GEMS Data on emissions are needed for the 4 sub-systems GHG, GRG, AER and RAQ GEMS Project has dedicated tasks for emissions and surface fluxes.
Advertisements

Allan Spessa 1,2, Kirsten Thonicke 3, Colin Prentice 3 Simulating Climate-Vegetation-Fire Interactions & Emissions: Regional Applications of the LPJ-SPITFIRE.
Short Background on Climate Change and Greenhouse Gases Dr Ruth Nussbaum ProForest Presentation to the RSPO GHG WG2 meeting in Feb 2010.
The global Carbon Cycle - The Terrestrial Biosphere Dr. Peter Köhler Monday, , 11:15 – 13:00 Room: S 3032.
Reducing Canada's vulnerability to climate change - ESS Variation of land surface albedo and its simulation Shusen Wang Andrew Davidson Canada Centre for.
Global Fire Emissions and Fire Effects on Biophysical Properties and the Associated Radiative Forcing Yufang Jin 1, James Randerson 1, G. R. van der Werf.
Science questions How will source-receptor relations change due to expected changes in emissions? How should future emission scenarios be constructed?
Carbon Cycle and Ecosystems Important Concerns: Potential greenhouse warming (CO 2, CH 4 ) and ecosystem interactions with climate Carbon management (e.g.,
Summary Terrestrial ECV’s Alexander Loew, Silvia Kloster Max-Planck-Institute for Meteorology.
03/06/2015 Modelling of regional CO2 balance Tiina Markkanen with Tuula Aalto, Tea Thum, Jouni Susiluoto and Niina Puttonen.
Climate change, fires, and carbon aerosol over N. America with preliminary detour to discuss GCAP model development (GCAP= Global change and air pollution)
Carbon sequestration in China’s ecosystems, Jingyun Fang Department of Ecology Peking University Feb. 14, 2008.
Anthropocene Introduction to Meteorology, spring 2011 Observations –Trace gases –Temperature, land and ocean –Precipitation –Sea level Attribution Models.
Evaluating the Impact of the Atmospheric “ Chemical Pump ” on CO 2 Inverse Analyses P. Suntharalingam GEOS-CHEM Meeting, April 4-6, 2005 Acknowledgements.
Evaluating the Role of the CO 2 Source from CO Oxidation P. Suntharalingam Harvard University TRANSCOM Meeting, Tsukuba June 14-18, 2004 Collaborators.
The Role of Aerosols in Climate Change Eleanor J. Highwood Department of Meteorology, With thanks to all the IPCC scientists, Keith Shine (Reading) and.
Impact of Reduced Carbon Oxidation on Atmospheric CO 2 : Implications for Inversions P. Suntharalingam TransCom Meeting, June 13-16, 2005 N. Krakauer,
Image: NASA ECHAM5/6 projects by Quentin Bourgeois, Junbo Cui, Gabriela Sousa Santos, Tanja Stanelle C2SM’s research group - Isabelle Bey.
Climate Change and Forestry Allan L. Carroll, Ph.D. Natural Resources Canada Canadian Forest Service Pacific Forestry Centre Victoria, Canada Senior Research.
Anthropogenic Influences on the Global Carbon Cycle and its Implications for the Future Abstract Carbon makes up approximately 50% of the dry weight of.
Terrestrial ECV assessment [WP3.4] Aim -to use CCI fire and soil moisture observations to derive functional relationships to optimize fire model parameters.
Climate Change – 1: Background
Fires and the Contemporary Global Carbon Cycle Guido van der Werf (Free University, Amsterdam, Netherlands) In collaboration with: Jim Randerson (UCI,
European capacity building initiativeecbi Climate Change: an Introduction ecbi Workshops 2007 Claire N Parker Environmental Policy Consultant european.
Preparatory work on the use of remote sensing techniques for the detection and monitoring of GHG emissions from the Scottish land use sector P.S. Monks.
ECOSYSTEM STRUCTURE AND FUNCTION +How do we define ecosystem structure +Importance of ecosystem structure +Factors controlling ecosystem structure +Drivers.
I. I.Climate Change – Greenhouse Gases A. A.Background Greenhouse Effect Gases absorb heat Natural Greenhouse Effect Mean planetary temperature = 15 o.

Development of the Temperate Shrub Submodel for the Community Land Model-Dynamic Global Vegetation Model (CLM-DGVM) Xubin Zeng Xiaodong Zeng Mike Barlage.
1 A Carbon Cycle Data Assimilation System at LSCE using multiple data streams (CARBONES / GEOCARBON EU-project ) Philippe Peylin, Natasha MacBean, Cédric.
How Does Climate Change Affect Biomass Accumulation in Boreal Ecosystems? Earth Science B Period 2012.
1 Remote Sensing and Image Processing: 9 Dr. Hassan J. Eghbali.
The Merton Report an AIMES/IGBP-ESA partnership As Earth System science advances and matures, it must be supported by robust and integrated observation.
(Mt/Ag/EnSc/EnSt 404/504 - Global Change) Biogochemistry & Climate (from IPCC WG-I, Chapter 7) Biogeochemistry & Climate Primary Source: IPCC WG-I Chapter.
Possibilities for C / GHG mitigation in agricultural lands Pete Smith Professor of Soils & Global Change School of Biological Sciences, University of Aberdeen,
Translation to the New TCO Panel Beverly Law Prof. Global Change Forest Science Science Chair, AmeriFlux Network Oregon State University.
Impact of climate Change on forest ecosystems in India Rajiv Kumar Chaturvedi National Environmental Sciences Fellow Indian Institute of Science Bangalore.
Spatial and temporal patterns of CH 4 and N 2 O fluxes from North America as estimated by process-based ecosystem model Hanqin Tian, Xiaofeng Xu and other.
Model Intercomparisons and Validation: Terrestrial Carbon, an Arctic Emphasis Andrew Slater.
Introduction to CMUG assessments, SST and plans for phase 2 Roger Saunders 4 th Integration Meeting.
WP11 highlights: introduction and overview EU FP6 Integrated Project CARBOOCEAN ”Marine carbon sources and sinks assessment” 5 th Annual & Final Meeting.
Land cover & fire at high latitudes: model-data comparison and model modification NCEO Land Science Meeting, February 2012, Sheffield, UK E.Kantzas,
TEMIS User Workshop, Frascati, Italy October 8-9, 2007 Formaldehyde application Derivation of updated pyrogenic and biogenic hydrocarbon emissions over.
Land use change and terrestrial carbon cycle Xiaojuan Yang April 17,2003.
Climate Change: an Introduction ecbi Workshops 2007 Claire N Parker Environmental Policy Consultant european capacity building initiative initiative européenne.
Simulating global fire regimes & biomass burning with vegetation-fire models Kirsten Thonicke 1, Allan Spessa 2 & I. Colin Prentice
I. I.Climate Change – Greenhouse Gases A. A.Background Greenhouse Effect Gases absorb heat (not light) Natural Greenhouse Effect Mean planetary temperature.
GlobEmission (ITT 6721) new ESA contract starting on Oct. 11 KNMI/BIRA/FMI/TNO/VITO.
Earth system model of INM RAS Volodin E.M., Galin V.Ya., Diansly N.A., Gusev A.V., Smyshlyaev S.P., Yakovlev N.G. Institute of Numerical Mathematics RAS.
Dr. Monia Santini University of Tuscia and CMCC CMCC Annual Meeting
Anthropogenic Causes: Land Use & Land Cover Current Weather Changes in Surface Albedo and Land Cover Radiative Forcing of Land Cover Changes Begin Climate.
Casey McCabe Global Change: Biome Perspective. (Illustration by Nicolle Rager Fuller, National Science Foundation.)
Hauglustaine et al. - HYMN KO Meeting th October Forward modelling with the LMDz-INCA coupled climate-chemistry model; Inverse modelling and data.
CMUG meeting – March 2016 Fire_cci phase 2 progress. Interactions with other ECVs Phase 2 of the Climate Change Initiative Fire_cci project Emilio.
Response of the mean global vegetation distribution to interannual climate variability Michael Notaro Associate Scientist Center for Climatic Research.
ESF workshop on methane, April 10-12, years of methane : from global to regional P. Bousquet, S. Kirschke, M. Saunois, P. Ciais, P. Peylin, R.
Schematic framework of anthropogenic climate change drivers, impacts and responses to climate change, and their linkages (IPCC, 2007).
Role of ECVs in climate-carbon feedback assessment Claire Magand Patricia Cadule, Jean-Louis Dufresne Institut Pierre Simon Laplace CMUG Integration Meeting,
Carbon Sequestration Akilah Martin Fall 2005.
Demographic scenarios
CARBON, WATER, LAND USE & CLIMATE
Department of Atmospheric Sciences
Model Summary Fred Lauer
Anthropogenic Causes: Land Use & Land Cover
CRG BoG: Main topics Consistency CCI data
Adam Butler & Glenn Marion, Biomathematics & Statistics Scotland •
Discussion After Coffee
Anthropocene physical basis of climate spring 2011
Dr. Matthias Lüdeke, Potsdam Institut für Klimafolgenforschung
Presentation transcript:

Carbon cycle assessment Patricia Cadule Jean-Louis Dufresne Institut Pierre Simon Laplace, Paris. CCI-CMUG, 27 May 2015

Regional CO 2 fluxes [IPCC AR5] Inversions [Peylin et al] Veget. models

CMIP5 Models vs Inversions (PgC/yr) Month (PgC/yr) Month (PgC/yr) Month (PgC/yr) Month (PgC/yr) Month Regional CO 2 fluxes Grey shading: inversions Color lines: CMIP5 models

Evaluations of the atmospheric CO 2 concentration of the 23 CMIP5 models Alert (Canada) Comparing models with carbon flux estimates (inversions) CO2 concentration in a few locations (transport of surface CO 2 flux) Over 11 CO2 stations Regional CO 2 fluxes

Fires produce Greenhouse gases (CO 2, CH 4, N 2 O, …) that impact the radiation budget CO, non-methane hydrocarbons, and NO x altering the oxidation capacity of the atmosphere Aerosols (OC, BC) having an impact on the radiation budget Ward et al., 2012 Project - Added value of CCI variables - Consistencies amongst variables - Focus on fires

Fires and vegetation models ORCHIDEE-SPITFIRE modeling framework, coupled with the LMDZ climate model SPITFIRE (Thonicke et al., 2010) Project - Added value of CCI variables - Consistencies amongst variables - Focus on fires

Emission (carbon and other gases) BA (Burned Area) CF (Combustion Fraction) EF (Emission Factor) ESA fire_cci Fuel (biomass, litter etc.) DGVM Atmospheric model Vegetation model Transport and Inversion models Observation Bottom-up approach of emissions estimation (aided by vegetation models )

Consistency fires vs precipitation Low precipitation: limited by fuel (vegetation) amount High precipitations: limited by the degree of drought Mean annual precipitation (mm/yr) ( ) Mean burn area

Annual burned area ESACCI ≈ 2x GFED4, despite many tiles still missing in ESACCI ESACCI GFED4 ESACCI/GFED Burned area: ESA fire_cci vs. GFED4

Experiments: Land cover data LC_CCI Current land cover map Outdated land cover inputs IGBP land cover (Belward et al. 1999) and, Olson vegetation map with 96 classes (1983) Land cover Köppen-Geiger climate zones Phenology & Physiognomy Plant Functional Types Land Cover -> PFT Conversion Tool (BEAM) ESA LC_CCI PFT datasets

Increase in BoNE Increase in Bare Soil Decrease in BoNS increase decrease Decrease in tundra C3 grass cover Increase in BoBS at expense of BoNE PFT differences – high latitudes (LC_CCI – Olson)

PFT differences – tropics (LC_CCI – Olson) GV2M Avignon - February 2014 Increase in C4 crops Decrease in TrRG Decrease in TrEV

Carbon budget evaluation Mauna Loa (Pacific)

Carbon budget evaluation Barrow (Alaska)

Complementary studies towards assessment of carbon cycle and fires in coupled climate model: Identify (in)consistencies amongst related datasets Determine the origins of added values of CCI Improve knowledge and understanding processes

Study 1 Dataset analysis Using the following datasets: SST, SI, LC, GHG, FIRE, SM, ALB Look for fires (region, spread/extent, duration) Identify corresponding pre-fire conditions (availability of fuel, climate conditions, ignition source, …) Identify corresponding post-fire conditions (climate conditions, emissions, albedo, land cover) Objectives –Propose to the extent possible improvement margins for future datasets (e.g., spatial and temporal resolutions) in case of inconsistencies between fires and pre/post conditions –Categorize fires for use in Study 2

Thank you for your attention

increase decrease Decrease in C3 croplands replaced by C3 grasslands Increases in C4 grasslands due to use of Koppen-Geiger climate zones C3 C4 PFT differences (1) – crops (LC_CCI – Olson) 1 - Bare soil 2 – TrBE : tropical broad-leaved evergreen 3 – TrBR : tropical broad-leaved raingreen 4 – TeNE : temperate needleleaf evergreen 5 – TeBE : temperate broad-leaved evergreen 6 – TeBS : temperate broad-leaved summergreen 7 – BoNE : boreal needleleaf evergreen 8 – BoBS : boreal broad-leaved summergreen 9 – BoNS : boreal needleleaf summergreen 10 – NC3 : C3 grass 11 – NC4 : C4 grass 12 – AC3 : C3 agriculture 13 – AC4 : C4 agriculture