Modelling dynamic vegetation within the Earth System models Victor - - PowerPoint PPT Presentation

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Modelling dynamic vegetation within the Earth System models Victor - - PowerPoint PPT Presentation

Modelling dynamic vegetation within the Earth System models Victor Brovkin Max-Planck-Institut f r Meteorologie KlimaCampus, Hamburg NEESPI Workshop, CITES Conference, Krasnoyarsk, 15 July 2009 Climate system Ocean Land surface after John


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Modelling dynamic vegetation within the Earth System models

Victor Brovkin

Max-Planck-Institut für Meteorologie KlimaCampus, Hamburg

NEESPI Workshop, CITES Conference, Krasnoyarsk, 15 July 2009

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SLIDE 2

Climate system

after John Osborn, NOAA

Land surface Ocean

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SLIDE 3

Sellers et al., Science, 1997

Interactions between the land surface and the atmosphere that have direct impacts on the physical climate system.

(A) Surface radiation budget. (B) Effect of heat fluxes on the atmosphere.

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Atmospheric gas composition Climate Terrestrial ecosystems

after Foley et al. (2003)

Biogeochemical effects

Changes in ecosystems affect sources and sinks of:

  • Greenhouse gases
  • Aerosols
  • Other gases (e.g. oxygen)

Biogeophysical effects

Changes in ecosystems affect:

  • Heat fluxes
  • Water fluxes
  • Wind (direction and

magnitude)

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SLIDE 5

Purves et al., Life: The Science of biology

Climatic control of terrestrial vegetation

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SLIDE 6

Köppen climate zones

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SLIDE 7

Vegetation models

  • Biogeography models (climate-vegetation classifications)

– classifications by Köppen, Holdridge – plant functional type (PFT) concept: species are lumped into several PFTs, such as evergreen needleleaf trees (BIOME1) – Biogeography + carbon cycle models (BIOME4)

  • Dynamic Global Vegetation Models (DGVMs)

– Fractional land cover representation (plant functional type) – Temporal dynamics – Disturbances as driving forcing of vegetation succession (explicitly or implicitly)

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SLIDE 8

DGVM

Cramer et al., Glob. Change Biol., 2001

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SLIDE 9

Vegetation cover: models vs present-day reconstruction

Cramer et al., Glob. Change Biol., 2001

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SLIDE 10

JSBACH Jena Scheme for Biosphere-Atmosphere Coupling in Hamburg

Atmosphere horizontal dynamics Atmosphere vertical dynamics MPIOM Ocean

vertical structure land surface processes

vertical atmosphere column

communication interface AOGCM ECHAM5/MPIOM

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SLIDE 11

Dynamic land biosphere Stomata Model: BETHY

  • Transpiration (CO2-sensitive stomatal cond.)
  • Photosynthesis: Carbon assimilation (NPP)

Phenology model: (LoGro-P)

  • dynamic Leaf Area Index (LAI)

Soil model: ECHAM5-scheme:

  • surface/soil hydrology
  • energy balance
  • mosaic approach for surface properties

Soil scheme Carbon Flow Model: Cbalance

  • heterotrophic (soil) respiration
  • net CO2-exchange with atmosphere (NEP)
  • Carbon accounting for plants and soil (C-pools)

Modules of JSBACH

Dynamic land cover:

  • tiling land approach; 8 PFTs
  • veget dynamics based on NPP and climate
  • anthropogenic land cover change

Albedo model:

  • visible and NIR surface albedo
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SLIDE 12

FPC1 FPC2 FPCi

Land area excluded from vegetation dynamics (e.g. crops & pastures, glaciers)

FPCn

Fast variable: Bare soil, Bs Slow variable: Desert or bare ground, Bg

Tiling of land surface

ECHAM land grid cell

damaged i burnt i i i i

FPC FPC FPC MORT FPC EST dt dFPC − − − = ) ( ) (

Bare soil fraction is diagnostic:

Simple model for dynamic vegetation: concept

ODE for FPC (fractional projected cover) solved daily:

) ( 1

∑ ∑

+ − =

woodyPFT i grassPFT i s

FPC FPC B

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damaged i burnt i i i i

FPC FPC FPC MORT FPC EST dt dFPC − − − = ) ( ) (

⋅ =

woodyPFT k k i i rel i

FPC NPP FPC NPP NPP

α α

) ( ) (

i i

PFT rel i

NPP FPC EST τ = ) (

mort PFT i i

i

FPC FPC MORT τ = ) (      < − + ≥ =

crit crit crit b i crit i burn PFT

q q if q q q k q q if

i

), 1 ( ,

max max

τ τ τ

burn PFT i burnt i

i

FPC FPC τ = )) ) 1 ( 1 , (max(

* 5 . 20

− − =

allPFT LAI i yr g

i

e FPC ave B

Desert fraction: FPC fraction burnt: q – rel. air humidity

Model equations

FPC dynamical equation solved daily: Mortality: Establishment: Relative NPP advantage:

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Model topology

       − = − − − = (...) (...)

, i i i i i i i a i i

MORT EST dt dFPC D B R GPP dt dB τ

potential equilibrium in absence

  • f climate variability

actual „mixed“ equilibrium induced by disturbances 1 FPC(PFT1) – dominant PFT FPC(PFT2) 1

Carbon dynamics is done by JSBACH carbon cycle module FPC dynamics is simulated by dynamic veget module

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Wildfire disturbance

SPITFIRE model (Thonicke et al., submitted)

Fraction burnt (yr-1)

Coupled model ECHAM5-MPIOM- JSBACH

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Tree fraction

Observed, MODIS data (Hansen et al., 2006) Interactive ECHAM5-MPIOM- JSBACH

Brovkin et al., GRL, 2009

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SLIDE 17

Desert/bare ground fraction

Observed, MODIS data (Hansen et al., 2006) Interactive ECHAM5-MPIOM- JSBACH

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SLIDE 18

Climate-vegetation feedbacks: interactive loop

Vegetation cover Atmosphere/

  • cean

Temperature, precipitation Albedo, transpiration, runoff, surface roughness

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SLIDE 19

Global annual mean temperature,°C

fixed vegetation interactive vegetation

Climate response to global forest

  • r grass cover

forest grass

Brovkin et al., GRL, 2009

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°C

Temperature changes (°C) relative to CTRL simulation

Winter (DJF) Summer (JJA) FOREST world GRASSLAND world

Brovkin et al., GRL, 2009

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Jones et al., Nature Geoscience, 2009

Projected changes in boreal forest cover in the Hadley Centre model

potential dynamic

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Perspective on vegetation modelling

  • Going beyond PFT concept

– Increased representativeness of species, modelling on the patches level (e.g. LPJ-GUESS) – Flexible reclassification of PFTs for paleo-applications – Direct modelling of climate-relevant plant traits (albedo) response to climate change without PFT step

  • Better representation of spatial and temporal

heterogenuity of vegetation cover & climate variabilty

– Accounting for formation of vegetation patterns – Rainfall intermittency in drylands – Disturbances regimes

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TERRABITES – new European biospheric network (COST Action ES0805)

The main objective of the Action is a cross-disciplinary assessment of our current understanding of the terrestrial biosphere from an Earth system perspective to improve the reliability of future Earth system projections in coupled climate-biosphere simulations Bringing together biospheric modellers, ecologists, and data gathering community 4 working groups:

  • WG 1: Modeling plant functioning
  • WG 2: Modeling carbon and nutrient cycling
  • WG 3: Modeling plant ecology
  • WG 4: Modeling human land use

Chair of Action MC: Christian Reick, MPI for Meteorology (Hamburg) Action duriation: June 2009 – June 2013 Participants: 14 COST countries; 4 non-COST countries & institutions Russian participants invited: Leonid Golubyatnikov (IAP), Dmitry Luri (IG) Open Symposium: 9-11 February 2010, Hamburg www.terrabites.net (not yet available!)