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Dario Papale

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New FLUXDATA collection Aim of the presentation: get feedbacks and suggestions from you in the next days
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Page 1: Dario Papale

New FLUXDATA collection

Aim of the presentation: get feedbacks and suggestions from you in the next days

Page 2: Dario Papale

The LaThuile 2007 collection

The LaThuile 2007 data collection gave a lot of visibility to FLUXNET and the eddy covariancetechnique in general. This visibility can be also useful to support the regional networks,critical for the FLUXNET success.

A good number of synthesis papers based on the data collection have been published and alot are under preparation. This scientific activity gave also the possibility to establish newcollaborations and links between scientists and networks.

However we also learned in these years what should be improved respect to the LaThuile2007 collection in particular in the view of the new collection under preparation:

- Additional methods should be used in the data processing

- PI’s version should be added if different from the others provided

- Different data sharing positions between PIs exist, so different policies could beproposed in particular given the interest from external communities.

- Ancillary data are important. Very important.

- Gaps in some region should be filled

- Uncertainties need to be estimated and added.

Page 3: Dario Papale

Fluxdata.org – Dataset Development

Individual Sites

Regional Networks

Flux/MetData

Fluxdata.org

BADMData Flux/Met

DataBADM Data + Flux/MetGap-Filled/QA/Products

Page 4: Dario Papale

New sites in the next collection

LaThuile 2007 New data submitted New sites (90)

Page 5: Dario Papale

Data processing and uncertainty estimation

Half hourly data

u* threshold selection- 3/5 different methods

u* filtering - 3/4 possibility

Gapfilling- 2 methods

Partitioning- 3 methods

3 methods, bootstraping…

Also daytime, also data after low turb., …

MDS and ANN

Reichstein, Lasslop, van Gorsel

Page 6: Dario Papale

Methods comparison

u* threshold LaThuile 2007

u*

thre

sho

ld N

ew m

eth

od

s

Originalre-implemented

Forward 2 points

Back 2 points

Ustar threshold selection, different methods

Page 7: Dario Papale

Data left after filtering

Page 8: Dario Papale

-1000 0 1000 2000 3000

Flux derived from GL2009 [gC m-2

yr-1

]

-1000

0

1000

2000

3000

Flu

x d

eriv

ed

fro

m M

R2

00

5 [

gC

m-2 y

r-1]

1

2

34

5

67

12

345

67

1

2

34

5

67

12

345

671

234

567

12

345

671

234

567

12

345

671

234

567

12

345

671

234

567

12

345

67

1

2

34

5

67

0 1000 2000 3000 4000

TER from GL2009 [gC m-2

yr-1

]

0

1000

2000

3000

4000

TE

R f

ro

m M

R2

00

5 [

gC

m-2 y

r-1]

R2 =0.87 (y=11.47+1.00x, p=0.000, N=144)

AT-Neu

AU-Tum

BR-Ji2

JP-TefUS-Goo

US-NC2

VU-Coc

BR-Sa1

BR-Sa2

BR-Sa3

IT-LavIT-Lec

US-Dk3

-1500 -1000 -500 0 500

NEE from GL2009 [gC m-2

yr-1

]

-1500

-1000

-500

0

500

NE

E f

ro

m M

R2

00

5 [

gC

m-2 y

r-1]

R2 =0.79 (y=-15.99+0.90x, p=0.000, N=144)

AT-Neu

BR-Ji2

US-Goo

US-NC2

US-SP2

US-SP3 BR-Sa3FR-Lq2

IT-Lav

IT-Lec

UK-PL3

US-Dk3

0 1000 2000 3000 4000

GPP from GL2009 [gC m-2

yr-1

]

0

1000

2000

3000

4000

GP

P f

ro

m M

R2

00

5 [

gC

m-2 y

r-1]

R2 =0.97 (y=-3.64+1.01x, p=0.000, N=144)

AT-NeuAU-Tum

AU-Wac

JP-Tef

BR-Ma2

BR-Sa2

BR-Sa3

IT-Lec

US-Dk3

The different methodsdeveloped give in generalhigher threshold valuesrespect to the LaThuile07.

However comparing night-time and day-time basedpartitioning methods(day-time almost notinfluenced by u*) theagreement is high in mostof the cases.

Climate zones

Ustar threshold selection

Page 9: Dario Papale

Reichstein et al in prep.

Uncertainty quantification

Barr et al in prep.

Ustar and partitioning – NEE, GPP, Reco

Ustar methods and uncertainty – NEE

Page 10: Dario Papale

Gapfilling

Gapfilling is not the mainsource of uncertainty andthe methods used (MDSand ANN) have beentested in the Moffat et al.2007 comparison.

Long gaps remain aproblem, in particular ifoccur during criticalphenological phases(spring).

When multiple years areavailable, gapfilling modelparameterization can usethe information aboutrelations drivers-fluxesfrom others years.

Trotta et al in prep.

Artificial gap length

Methods comparison (MultiYear vs Single Year)

Artificial gap length

Artificial gap lengthArtificial gap length

Page 11: Dario Papale

Annual cumulative plots – NEE – full factorial

Preliminar, Trotta et al in prep.

Page 12: Dario Papale

Annual cumulative plots – GPP – full factorial

Preliminar, Trotta et al in prep.

Page 13: Dario Papale

Data processingHalf hourly data

u* threshold selection- 3/5 different methods

u* filtering - 3/4 possibility

Gapfilling- 2 methods

Partitioning- 3 methods

1 dataset

3/5 datasets

9/20 datasets

18/40 datasets

Between 54 and 120 different “versions” of the same dataset, all valid, it is uncertainty.

3 methods, bootstraping…

Also daytime, also data after low turb., …

MDS and ANN

Reichstein, Lasslop, van Gorsel

?What do we distribute?

NEE

Freq

uen

cy

1 5 25 50 75 95 99

Percentiles

Ok for the uncertainy, but weneed also a “reference value”and using the median wouldaffect the variability.Suggestion from you NEEDED!!

Page 14: Dario Papale

You should register, it if fast and easy, in this way we can better identify whoproposed what. However, if the registration is the limiting factor for you, use myaccount:

USER ID: fluxnet PASSWORD: meteo_tests

http://fluxnet.betaboard.ca/f1-ideas-for-meteo-checks

Meteo data QAQC and others feedbacks

There are a lot of tests that can be implemented to identify potential problems with themeteo data that would lead to an accurate check. Examples are:

- Check that the diffuse radiation is not greater than total radiation

- Check that the relation between global incoming radiation and incoming PAR is stable intime

- Check that below canopy PAR is not greater than incoming PAR

- Check that after rain (> of a threshold) there is a change in SWC and the other way round

- Check that the relations between air temperature and different soil temperatures arestable (monthly because phenology would affect this)

Your contribution and ideas are fundamental. Antje Moffat created a site where you can suggest tests or comment proposed tests.

Page 15: Dario Papale

Ancillary data and metadata

Ancillary data are very important and their availability would permit new studies andsynthesis activities. At the moment these data are not available for most of the sites.

In addition, information about the tower building, sensors setup, raw data processing, PIversion of fluxes calculation methods, are important to correctly interpret the data.

These info are sometimes collected at regional level using different formats and schemes andnot continuously updated.

The BADM is now an international standard, it is used also in EU projects and it will be usedalso in ICOS. A new version, with a different organization for an easier filling will be releasedsoon.

A metadata template, with the same BADM structure, has been prepared and it is under test.It will be used to transmit and register all the info about the site setup and data processing ina standard and structured way.

First tests at some sites show that although at the beginning it looks a lot of work, it is notdifficult and help to store info that otherwise would be lost. Do you remember all about yoursite?

Page 16: Dario Papale

• Derived variables (ecosystem parameters and climatic indices)

• Footprint calculation (Kljun model, but different inputs are needed)

• Long term daily meteorology at site level from ECMWF downscaling

• Time-scale separation of variables

Additional products

Together with the processed fluxes and meteo data, the ancillary data and the metadata, anumber of additional derived products will be released for each site. These could include forexample:

Mahecha et al. (2010), JGR-Biogeo

• Solar time, Sun position, modelled diffuse radiation fraction

• Remote sensing products cutout– Modis cutouts

– Stöckli fPAR/LAI

– MERIS

– Parasol/Polder

• Meteorogical cutouts– ECMWF

– WATCH

– SHEFFIELD NCEP

Do you have codes ready?

Lat: 50°, Long: 0°

Page 17: Dario Papale

New data policies

The community is quite heterogeneous in terms of data sharing and data use policy to beapplied. For this reason three different data policies have been created:

LaThuile policy: sharing only with data contributors

- Data are shared only with others data contributors

- Data access is possible only with a synthesis proposal accepted

- It is mandatory to invite all the data contributors to give additionalintellectual inputs to the paper and become coauthors

- Strict rules in terms of communications between paper leader and site Pis

- Group coauthorship and site paper citation when possible.

Opened policy: sharing openly but under control

- Data are shared also with external communities

- Data access is possible only with a synthesis proposal accepted

- Encuraged but not enforced to invite data contributors to give additionalintellectual inputs. Mandatory if few sites or many ancillary data.

- Group coauthorship and site paper citation when possible,

Free Fair-use policy: simply sharing openly

Full policies texts available on www.fluxdata.org

Different years of the same site can have different policies

Login in the fluxdata.org system and do your selection for your sites

Today, 965 site/years, 496 LaThuile policy, 86 Open and 383 Free

Page 18: Dario Papale

Deadline for new data submission passed and we are preparing the processing. Last chance toparticipate is submitting the data before the end of the month.

The objective is to have the new data collection ready this year, possibly before summer.

New collection plan, how to contribute

Fluxes and meteo data submission:

Ameriflux sites and sites in US in general: Tom Boden

Canadian sites: CCP database

European sites and sites managed by EU institutions: Dario Papale

African and Russian sites: Dario Papale

All others sites: Bob Cook

BADM and Metadata

All sites directly to fluxdata.org

Fluxes, meteo, BADM and metadata processing

All sites will be processed by the fluxdata.org team between Europe and US


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