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LDAS-Monde sequential assimilation of satellite-derived vegetation and soil moisture products

Toulouse – 22 mars 2018 Albergel C.

1

Munier S.

1

, Leroux D.

1

and Calvet J.-C.

1

With help from many others !

1CNRM UMR 3589, Météo-France/CNRS, Toulouse, France

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Study the vegetation and terrestrial water cycles

Current fleet of Earth Satellite missions holds an unprecedent potential to quantify land surface variables [Lettenmaier et al., 2015]

 Spatial and temporal gaps

 Cannot observe all key Land Surface Variables (LSVs)

Land Surface Models (LSMs) provide LSVs estimates at all time/location based on physical laws

 Both observations and LSMs suffer from uncertainties

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Study the vegetation and terrestrial water cycles

Current fleet of Earth Satellite missions holds an unprecedent potential to quantify land surface variables [Lettenmaier et al., 2015]

 Spatial and temporal gaps

 Cannot observe all key Land Surface Variables (LSVs)

Land Surface Models (LSMs) provide LSVs estimates at all time/location based on physical laws

 Both observations and LSMs suffer from uncertainties

Through a weighted combination of both, LSVs can be better estimated than by either source of information alone [Reichle et al., 2007]

Data assimilation : spatially and temporally integrates the observed information

into LSMs in a consistent way to unobserved locations, time steps and variables

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LDAS-Monde : Global capacity integration of satellite observations into SURFEX, fully coupled to hydrology

Study the vegetation and terrestrial water cycles

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LDAS-Monde : Global capacity integration of satellite observations into SURFEX, fully coupled to hydrology

 ISBA-A-gs : simulates the diurnal cycle of water and carbon fluxes, plant growth and key vegetation variables on a daily basis

(Calvet et al., 1998, 2007, Gibelin et al., 2006)

Study the vegetation and terrestrial water cycles

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Titre abrégé

LDAS-Monde : Global capacity integration of satellite observations into SURFEX, fully coupled to hydrology

 CTRIP : TRIP based river routing system with CNRM developments for global hydrological applications

(Oki and Sud, 1998, Decharme et al., 2008, 2010)

Study the vegetation and terrestrial water cycles

ISBA to CTRIP :

runoff, drainage, groundwater and floodplain recharges

CTRIP to ISBA :

water table depth/rise, floodplain fraction, flood potential infiltration

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Titre abrégé Study the terrestrial water cycle

LDAS-Monde : Global capacity integration of satellite observations into SURFEX, fully coupled to hydrology

 ‘Update’ Soil Moisture and LAI

Study the vegetation and terrestrial water cycles

SSM

LAI

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Titre abrégé Study the terrestrial water cycle Study the vegetation and terrestrial water cycles

LAI (m2m-2)

Model Domaine Atm. Forcing DA

Method Assimilated

Obs. Observation

Operator Control

Variables Additional Option

ISBA Multi-layer soil model CO2-responsive version

(Interactive veg.)

Global (2000-2013, 1°)

EartH2Observe project (Schellekens et

al., 2017)

SEKF

SSM (ESA-CCI,

ASCAT) (GEOV1)LAI

Second layer of soil (1-4cm)

LAI

Layers of soil 2 to 8 (1-100cm)

LAI

Coupling with CTRIP (0.5°)

USA, Europe, Western & Austral

Africa, Australia (2007-06/2017, 0.5°)

ERA-Interim

(Dee et al., 2011) Coupling with

CTRIP (0.5°)

France (2007-2016,

8kmx8km)

SAFRAN (Quintena-Segui,

et al., 2008)

Offline coupling with

MODCOU Spain

(2008-07/2014 5kmx5km)

SAFRAN-Spain (Quintena-Segui,

et al., 2017

Offline coupling with RAPID

Page 8

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Titre abrégé Study the terrestrial water cycle Study the vegetation and terrestrial water cycles

LAI (m2m-2)

LAI (m2m-2)

LAI (m2m-2)

LAI (m2m-2)

Model Domaine Atm. Forcing DA

Method Assimilated

Obs. Observation

Operator Control

Variables Additional Option

ISBA Multi-layer soil model CO2-responsive version

(Interactive veg.)

Global (2000-2013, 1°)

EartH2Observe project (Schellekens et

al., 2017)

SEKF

SSM (ESA-CCI,

ASCAT) (GEOV1)LAI

Second layer of soil (1-4cm)

LAI

Layers of soil 2 to 8 (1-100cm)

LAI

Coupling with CTRIP (0.5°)

USA, Europe, Western & Austral

Africa, Australia (2007-06/2017, 0.5°)

ERA-Interim

(Dee et al., 2011) Coupling with

CTRIP (0.5°)

France (2007-2016,

8kmx8km)

SAFRAN (Quintena-Segui,

et al., 2008)

Offline coupling with

MODCOU Spain

(2008-07/2014 5kmx5km)

SAFRAN-Spain (Quintena-Segui,

et al., 2017

Offline coupling with RAPID

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Titre abrégé Study the terrestrial water cycle Study the vegetation and terrestrial water cycles

LAI (m2m-2)

Model Domaine Atm. Forcing DA

Method Assimilated

Obs. Observation

Operator Control

Variables Additional Option

ISBA Multi-layer soil model CO2-responsive version

(Interactive veg.)

Global (2000-2013, 1°)

EartH2Observe project (Schellekens et

al., 2017)

SEKF

SSM (ESA-CCI,

ASCAT) (GEOV1)LAI

Second layer of soil (1-4cm)

LAI

Layers of soil 2 to 8 (1-100cm)

LAI

Coupling with CTRIP (0.5°)

USA, Europe, Western & Austral

Africa, Australia (2007-06/2017, 0.5°)

ERA-Interim

(Dee et al., 2011) Coupling with

CTRIP (0.5°)

France (2007-2017,

8kmx8km)

SAFRAN (Quintena-Segui,

et al., 2008)

Offline coupling with

MODCOU Spain

(2008-07/2014 5kmx5km)

SAFRAN-Spain (Quintena-Segui,

et al., 2017

Offline coupling with RAPID

Page 10

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Titre abrégé Study the terrestrial water cycle Study the vegetation and terrestrial water cycles

LAI (m2m-2)

Model Domaine Atm. Forcing DA

Method Assimilated

Obs. Observation

Operator Control

Variables Additional Option

ISBA Multi-layer soil model CO2-responsive version

(Interactive veg.)

Global (2000-2013, 1°)

EartH2Observe project (Schellekens et

al., 2017)

SEKF

SSM (ESA-CCI,

ASCAT) (GEOV1)LAI

Second layer of soil (1-4cm)

LAI

Layers of soil 2 to 8 (1-100cm)

LAI

Coupling with CTRIP (0.5°)

USA, Europe, Western & Austral

Africa, Australia (2007-06/2017, 0.5°)

ERA-Interim

(Dee et al., 2011) Coupling with

CTRIP (0.5°)

France (2007-2017,

8kmx8km)

SAFRAN (Quintena-Segui,

et al., 2008)

Offline coupling with

MODCOU Spain

(2008-07/2014 5kmx5km)

SAFRAN-Spain (Quintena-Segui,

et al., 2017

Offline coupling with RAPID

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LAI [m2m-2]

First results using ECMWF latest atmospheric re-analysis era-5, 0.25x0.25º, 2010-2016[17] to force LDAS-Monde : Leaf Area Index

Page 12

Study the vegetation and terrestrial water cycles

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Titre abrégé Study the terrestrial water cycle using SODA LDAS-Monde assessment over North America

Model Domaine Atm. Forcing DA

Method Assimilated

Obs. Observation

Operator Control

Variables Additional Option

Multi-layer soil modelISBA CO2-responsive version

(Interactive veg.)

(2007-2016, 0.5°) USA ERA-Interim

(Dee et al., 2011) SEKF SSM

(ASCAT) (GEOV1)LAI

Second layer of soil (1-4cm)

LAI

Layers of soil 2 to 8 (1-100cm)

LAI

Coupling with CTRIP (0.5°)

http://land.copernicus.eu/global/

(C-band microwave sensor, 0.1o) (SPOT-VGT / PROBA-V, 1km) (seasonal bias correction)

2 experiments over 2007-2016: open-loop (i.e. model run), analysis (i.e. assimilation)

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Titre abrégé Study the terrestrial water cycle using SODA LDAS-Monde assessment over North America

Analysis Impact is evaluated by comparing performance improvement relative to the open- loop

Assimilated SSM & LAI

(analysis has to be closer to them than the open-loop !) https://land.copernicus.eu/

In situ measurements of soil moisture from USCRN

network https://www.ncdc.noaa.gov/crn

River discharge from USGS https://waterdata.usgs.gov/nwis

FLUXNET measurements : H, LE and NEE http://fluxnet.fluxdata.org/data/fluxnet2015-dataset/

Evapotranspiration from the GLEAM project http://www.gleam.eu Gross Primary Production from the FLUXCOM project http://www.fluxcom.org

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5th iLEAPS Science Conference, 11-14 September, Oxford, UK

Titre abrégé Study the terrestrial water cycle using SODA LDAS-Monde assessment over North America

SSM : Averaged maps and seasonal scores over 2007-2016

Open-loop Analysis

[m3m-3]

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5th iLEAPS Science Conference, 11-14 September, Oxford, UK

Titre abrégé Study the terrestrial water cycle using SODA LDAS-Monde assessment over North America

LAI : Averaged maps and seasonal scores over 2007-2016

Open-loop Analysis

[m2m-2]

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Titre abrégé Study the terrestrial water cycle using SODA LDAS-Monde assessment over North America

Soil moisture from USCRN network, 2009-2016 (April-September, tri-hourly data)

Correlations N stations

(significant Correlations values) 108

% stations

R(Analysis) >= R(Open-loop) 74%

Stars : open-loop provides better Correlations (R) Circles : no impact at all

Downward-pointing triangles : analysis provide better Correlations (R)

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Titre abrégé Study the terrestrial water cycle using SODA LDAS-Monde assessment over North America

FLUXNET 2015 data, 2007-2016 (daily data if at least 2-yr of data)

H LE NEE

N stations

(significant R values) 44 44 40

N stations (%)

R(Analysis) > R(Open-loop) 30

(68%) 32

(72%) 31

(77%) N stations (%)

RMSD(Analysis) < RMSD(Open-loop) 32

(72%) 33

(75%) 29

(72%)

Analysis better compare to the FLUXNET stations than the open-loop

Blue : R(analysis) is better than R(open-loop)

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Titre abrégé Study the terrestrial water cycle using SODA LDAS-Monde assessment over North America

River discharge from USGS

NSE values are computed for each stations (monthly values scaled to the drainage area)

Normalised Information Contribution used to quantify improvment/degradation

N stations

>4-yr of data

3155 N stations

>4-yr of data

Analysis impact > |3 %|

503 (16 %) Impact is

+3 % Impact is -3 %

354 (70 %) 149 (30 %) Neutral to positive impact from the analysis on river discharge

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10th HyMeX Workshop, 4-7 July 2017, Barcelona, Spain

Evapotranspiration from the GLEAM project (Martens et al., 2017, GMD)

Open-loop Analysis

LDAS-Monde assessment over North America

Page 20

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Gross Primary Production from the FLUXCOM project (Jung et al., 2017)

Open-loop Analysis

LDAS-Monde assessment over North America

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Does analysis provide better initial conditions that last in time ?

Use analysis initial conditions at 01/04/2016 to start a 8-month simulation

Persistence for several weeks / months on LAI

LDAS-Monde assessment over North America

Initial conditions from analysis (USA 01/2007 to 04/2016)

Averaged LAI over North America

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LDAS-Monde over France Analysis – Model (2017)

EVAPC RUNOFFC DRAINC (kg/m²/d)

LAI (m

2

m

-2

)

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Study the vegetation and terrestrial water cycles

Towards a ‘SIM2-like’ LDAS

 Run SURFEX over 9892 grid points, over 3878 mountainous grid points

(Save RUNOFFC, DRAINC)

 Mix the results of mountains elevation tiles to the original grid France, two different water transfer for mountainous cells and for plain areas outside aquifers simulated by MODCOU (mix_res)

 Neutral impact on river discharge / Positive impact on vegetation

 Re-activate this activity (coll. S. Munier CNRM/GMME/SURFACE)

Page 24

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Page 25

Study the terrestrial water cycle using SODA

Evaluation of analysis impact 2000-2010: grain yield over France vs. above- ground biomass 45 sites (Agreste portal, http://agreste.agriculture.gouv.fr)

 Inter-annual variability

 Analysed Biomass shows better R and RMSD than that of the open-loop

Study the vegetation and terrestrial water cycles

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LDAS-Monde : Conclusions and perspectives

Integration of satellite observations into SURFEX, fully coupled to hydrology

Now the only system able to sequentially assimilate vegetation products together with soil moisture observations

Positive impact on terrestrial water cycle, vegetation cycle

Powerful tool to monitor land surface variables, droughts

Foster link to applications

Climate reanalysis

From monitoring to forecasting

(Analysis provides better initial conditions than a model run)

PhD for 2018 : Assimilation of satellite data for monitoring and forecasting agricultural drought ans water ressources (funding ? MF/ED/MOPGA)

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LDAS recent publications :

Albergel, C., S. Munier, D. J. Leroux, H. Dewaele, D. Fairbairn, A. L. Barbu, E. Gelati, W. Dorigo, S. Faroux, C. Meurey, P. Le Moigne, B. Decharme, J.-F. Mahfouf, J.-C. Calvet : Sequential assimilation of satellite-derived vegetation and soil moisture products using SURFEX_v8.0 : LDAS-Monde assessment over the Euro-Mediterranean area, Geosci. Model Dev., Geosci. Model Dev., 10, 3889–3912, 2017.

Fairbairn, D., Barbu, A. L., Napoly, A., Albergel C., Mahfouf, J.-F., and Calvet, J.-C. : The effect of satellite-derived surface soil moisture and leaf area index land data assimilation on stramflow simulations over France, Hydrol. Earth Syst. Sci., 21, 2015–2033, 2017.

Fairbairn, D., Barbu, A.L., Mahfouf, J.-F., Calvet, J.-C., and Gelati, E. : Comparing the ensemble and extended Kalman filters for in situ soil moisture assimilation with contrasting conditions, Hydrol. Earth Syst. Sci., 19, 4811–4830, 2015.

Barbu, A. L., Calvet, J.-C., Mahfouf, J.-F., and Lafont, S. : Integrating ASCAT surface soil moisture and GEOV1 leaf area index into the SURFEX modelling platform : a land data assimilation application over France, Hydrol. Earth Syst.

Sci., 18, 173-192, 2014.

Barbu, A. L., Calvet, J.-C., Mahfouf, J.-F., Albergel, C., and Lafont, S. : Assimilation of Soil Wetness Index and Leaf

Contact : clement.albergel@meteo.fr

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Page 28

Study the terrestrial water cycle using SODA LDAS-Monde processing chain

SURFEX ldasPre.py

Prépare les observations (e.g. CDF matching SSM)

ldasPost.py

Visualisation & Statistiques prepareForcing.py

Ajuste le domaine Fichiers journaliers

e.g. SAFRAN,

ERA-Interim

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Study the terrestrial water cycle using SODA LDAS-Monde processing chain

monthly files (year 1 for spinup)

daily files (open-loop and analysis)

Open-loop outputs

Remotely sensed Observations

Analysis Outputs

Run pgd_prep Run

PrepareForcing

Run job_spinup Run Open-Loop

Run LdasPre

Run Analysis

Run LdasPost

PGD, PGD_fractown,

PREP, TRIP_PREP

1

2

3

4

5

6

sxvgo1 Hendrix Beaufix

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