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Influence of the spatial resolution of climate on tree range simulations

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HAL Id: hal-02747225

https://hal.inrae.fr/hal-02747225

Submitted on 3 Jun 2020

HAL is a multi-disciplinary open access archive for the deposit and dissemination of sci-entific research documents, whether they are pub-lished or not. The documents may come from teaching and research institutions in France or abroad, or from public or private research centers.

L’archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des établissements d’enseignement et de recherche français ou étrangers, des laboratoires publics ou privés.

Influence of the spatial resolution of climate on tree range simulations

Nicolas Martin-Stpaul, Julien Ruffault, Christophe François, Marc Stéfanon, P. Drobinsky, Kamel Soudani, Eric Dufrene, Serge Rambal, Florent Mouillot,

Paul Leadley

To cite this version:

Nicolas Martin-Stpaul, Julien Ruffault, Christophe François, Marc Stéfanon, P. Drobinsky, et al.. Influence of the spatial resolution of climate on tree range simulations. EGU General Assembly 2013, 2013, Vienne, Austria. �hal-02747225�

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Influence of the spatial

resolution of climate on tree

range simulations

Drawing of a dying beech, ink (200x250 cm) Adeline Carrion Reyna

Martin-StPaul NK., Ruffault J., Francois C., Stéfanon M., Drobinsky P.,

Cheaib A., Soudani K., Dufrêne E., Rambal S., Mouillot F. & Leadley P.

EGU 2013 Vienna April 04

(3)

Introduction

The footprint of climate change on forests

Migration toward higher elevation

Penuelas et al., 2003 GCB

1945 1995

(4)

3

Introduction

The footprint of climate change on forests

Increase tree dieback

Penuelas et al., 2003 GCB

Allen et al., 2009 FEM

1945 1995

Migration toward higher elevation

(5)

4

Introduction

The footprint of climate change on forests

Increase forest defoliation

Carnicer et al., 2012 PNAS Penuelas et al., 2003 GCB

Allen et al., 2009 FEM

Beech upward shift (70m) to the top of the mountains

1945 1995

Increase tree dieback

(6)

Introduction

Anticipacting climate change effects on trees and forest

Climate projection (Resolution 300 to 50 km)

(7)

Impact model

Process or correlative

Introduction

Anticipacting climate change effects on trees and forest

Climate projection (Resolution 300 to 50 km)

(8)

Impact model

Process or correlative

Thullier et al., 2005 PNAS

Introduction

Anticipacting climate change effects on trees and forest

Biodiversity Losses 2080-2100 Compared to 1970-1990 Using 50km Resolution climate Climate projection (Resolution 300 to 50 km)

(9)

Very large biodiversity losses in

europe >60% !

Impact model

Process or correlative

Introduction

Anticipacting climate change effects on trees and forest

Thullier et al., 2005 PNAS

Biodiversity Losses 2080-2100 Compared to 1970-1990 Using 50km Resolution climate Climate projection (Resolution 300 to 50 km)

(10)

Impact model

Process or correlative

Introduction

Anticipacting climate change effects on trees and forest

Thullier et al., 2005 PNAS

Biodiversity Losses 2080-2100 Compared to 1970-1990 Using 50km Resolution climate

Very large biodiversity losses in

europe >60% !

A matter of resolution ?

Randin et al., 2009 (GCB) …

Climate projection (Resolution 300 to 50 km)

(11)

Does the spatial resolution of climate affect the simulations of the

productivity of beech and oak forest over France?

Introduction

A matter of spatial scale ?

(12)

Does the spatial resolution of climate affect the simulations of the

productivity of beech and oak forest over France?

Introduction

A matter of spatial scale ?

Steep climatic gradient

(13)

Does the spatial resolution of climate affect the simulations of the

productivity of beech and oak forest over France?

Introduction

A matter of spatial scale ?

Pedunculate Oak European Beech

Two wide spread

tree species

Steep climatic gradient

(14)

Does the spatial resolution of climate affect the simulations of the

productivity of beech and oak forest over France?

Introduction

A matter of spatial scale ?

Pedunculate Oak European Beech

Two wide spread

tree species

Steep climatic gradient

Hyp:

Most changes should appear in

montainous regions

(15)

Materials & Methods

The model CASTANEA

Solar radiation temperature Water vapour Interception Photosynthesis Precipitations Canopy interception Throughfall Stem flow Litter Surface Root zone Soil evaporation Carbon Allocation C Root C F.Root C surface CO2 Canopy Evaporation drainage Stomatal Cond. GPP C Stem C Stor. Transpiration C litter C deep Heterotrophic Respiration C leaves Autotrophic Respiration Reco ETR

 Process based model

 Monospecific

 Average tree

Daily time step

-C, H

2

O Fluxes

-NPP, Growth, wood

production

-Presence

Dufrêne et al. 2005 14

(16)

Materials & Methods

The model CASTANEA

Solar radiation temperature Water vapour Interception Photosynthesis Precipitations Canopy interception Throughfall Stem flow Litter Surface Root zone Soil evaporation Carbon Allocation C Root C F.Root C surface CO2 Canopy Evaporation drainage Stomatal Cond. GPP C Stem C Stor. Transpiration C litter C deep Heterotrophic Respiration C leaves Autotrophic Respiration Reco ETR

 Process based model

 Monospecific

 Average tree

Daily time step

Daily climatic input

- Rainfall ; Temperature;

Radiation ; Wind speed

Humidity

-C, H

2

O Fluxes

-NPP, Growth, wood

production

-Presence

Stand and species

parameters

LMA, Photosynthetic

capacity

, C Allocation…

Soil available water

content

Dufrêne et al. 2005

(17)

Materials & Methods

The model CASTANEA

Solar radiation temperature Water vapour Interception Photosynthesis Precipitations Canopy interception Throughfall Stem flow Litter Surface Root zone Soil evaporation Carbon Allocation C Root C F.Root C surface CO2 Canopy Evaporation drainage Stomatal Cond. GPP C Stem C Stor. Transpiration C litter C deep Heterotrophic Respiration C leaves Autotrophic Respiration Reco ETR

 Process based model

 Monospecific

 Average tree

Daily time step

-C, H

2

O Fluxes

-NPP, Wood production

-Presence

Stand and species

parameters

LMA, Photosynthetic

capacity

, C Allocation…

Soil available water

content..

Daily climatic input

- Rainfall ; Temperature;

Radiation ; Wind speed

Humidity

Dufrêne et al. 2005

(18)

Climate :

Analysis at different resolution : SAFRAN Period (1989-2010) × 7 : Forest rotation

8 km

Materials & Methods

Databases & simulations

Solar radiation temperature Water vapour Interception Photosynthesis Precipitations Canopy interception Throughfall Stem flow Litter Surface Root zone Soil evaporation Carbon Allocation C Root C F.Root C surface CO2 Canopy Evaporation drainage Stomatal Cond. GPP C Stem C Stor. Transpiration C litter C deep Heterotrophic Respiration C leaves Autotrophic Respiration Reco

ETR European Beech

Deciduous Oak

Process model CASTANEA

Dufrêne et al. 2005

(19)

Climate :

Analysis at different resolution : SAFRAN Period (1989-2010) × 7 : Forest rotation

8 km

Materials & Methods

Databases & simulations

Soil AWC

8km

Solar radiation temperature Water vapour Interception Photosynthesis Precipitations Canopy interception Throughfall Stem flow Litter Surface Root zone Soil evaporation Carbon Allocation C Root C F.Root C surface CO2 Canopy Evaporation drainage Stomatal Cond. GPP C Stem C Stor. Transpiration C litter C deep Heterotrophic Respiration C leaves Autotrophic Respiration Reco

ETR European Beech

Deciduous Oak

Process model CASTANEA

Dufrêne et al. 2005

(20)

20 km

8 km

50 km

Materials & Methods

Databases & simulations

Soil AWC

8km

Solar radiation temperature Water vapour Interception Photosynthesis Precipitations Canopy interception Throughfall Stem flow Litter Surface Root zone Soil evaporation Carbon Allocation C Root C F.Root C surface CO2 Canopy Evaporation drainage Stomatal Cond. GPP C Stem C Stor. Transpiration C litter C deep Heterotrophic Respiration C leaves Autotrophic Respiration Reco

ETR European Beech

Deciduous Oak

Process model CASTANEA

Dufrêne et al. 2005

Climate :

Analysis at different resolution : SAFRAN Period (1989-2010) × 7 : Forest rotation

(21)

20 km

8 km

50 km

Materials & Methods

Databases & simulations

Soil AWC

8km

Solar radiation temperature Water vapour Interception Photosynthesis Precipitations Canopy interception Throughfall Stem flow Litter Surface Root zone Soil evaporation Carbon Allocation C Root C F.Root C surface CO2 Canopy Evaporation drainage Stomatal Cond. GPP C Stem C Stor. Transpiration C litter C deep Heterotrophic Respiration C leaves Autotrophic Respiration Reco

ETR European Beech

Deciduous Oak

Process model CASTANEA

Oak Dufrêne et al. 2005 Beech Climate 50km Climate 20km Climate 8km Wood production (gC m-²)

Climate :

Analysis at different resolution : SAFRAN Period (1989-2010) × 7 : Forest rotation

(22)

Results

Beech and oak productivity at variable climate resolution

Beech Oak Unbiased at France scale NPP8km vs. NPP50km (gC m-2 y-1) The effect of spatial resolution is 0 200 400 600 800 1000 0 200 400 600 800 1000 -200 0 200 400 600 800 -2 0 0 0 200 400 600 800

NPP 50km

NPP

8km

21

(23)

Results

Beech and oak productivity at variable climate resolution

Beech

Oak

Unbiased at France scale

Important locally Not only in the mountain

       fine fine coarse -100 NPP NPP NPP NPP8km vs. NPP50km (gC m-2 y-1) The effect of spatial resolution is 0 200 400 600 800 1000 0 200 400 600 800 1000 -200 0 200 400 600 800 -2 0 0 0 200 400 600 800

NPP 50km

NPP

8km

(24)

Results

Beech and oak productivity at variable climate resolution

Beech

Oak

Unbiased at France scale

Important locally Not only in the mountain

       fine fine coarse -100 NPP NPP NPP NPP8km vs. NPP50km (gC m-2 y-1) The effect of spatial resolution is 0 200 400 600 800 1000 0 200 400 600 800 1000 -200 0 200 400 600 800 -2 0 0 0 200 400 600 800

NPP 50km

NPP

8km

At the edge of the species range Wood Production (gC m-²)

(25)

Results

What resolution do we need and where ?

<-10

>10 -10 - 10

European beech Deciduous oak

20 km 50 km Wood Production 20 km 50 km

Difference (%) to fine resolution

(26)

Results

What resolution do we need and where ?

<-10

>10 -10 - 10

European beech Deciduous oak

20 km 50 km 20 km 50 km 50 km 20 km 8 km Best resolution Wood Production Difference (%) to fine resolution 25

(27)

Summary

& Conclusion & Perspectives

Climate resolution affects the simulation of beech & Oak productivity

Not only in mountainous area… At the edge of species range

Patterns of the optimal resolution differ between species :

Summary

(28)

Summary &

Conclusion

& Perspectives

Summary

Conclusion

Difficult to assess if there is an optimal resolution :

The finer the better…

Climate resolution affects the simulation of beech & Oak productivity

Not only in mountainous area… At the edge of species range

Patterns of the optimal resolution differ between species :

(29)

Summary & Conclusion &

Perspectives

Simulations at 1km resolution using statistical downscaling

Other species; Climate change scenarii

Summary

Conclusion

Perspectives

Difficult to assess if there is an optimal resolution :

The finer the better…

Climate resolution affects the simulation of beech & Oak productivity

Not only in mountainous area… At the edge of species range

Patterns of the optimal resolution differ between species :

(30)

Thank you for your attention

Drawing of a dying beech, ink (200x250 cm) Adeline Carrion Reyna

(31)

Results

What resolution do we need and where ?

50km 20km 8km NPP 50km 50km 20km 8km

fine fine coarse

-100

NPP

NPP

NPP

30

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