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Gap Filling Comparison Workshop, September 18-20, 2006, Jena, Germany Corinna Rebmann Olaf Kolle Max-Planck-Institute for Biogeochemistry Jena, Germany.

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Presentation on theme: "Gap Filling Comparison Workshop, September 18-20, 2006, Jena, Germany Corinna Rebmann Olaf Kolle Max-Planck-Institute for Biogeochemistry Jena, Germany."— Presentation transcript:

1 Gap Filling Comparison Workshop, September 18-20, 2006, Jena, Germany Corinna Rebmann Olaf Kolle Max-Planck-Institute for Biogeochemistry Jena, Germany Eddy covariance measurements and their shortcomings for the determination of the net ecosystem exchange of carbon dioxide

2 Outline Introduction of measurement site and advection experiment Reasons for data gaps  Special features of open path analyser Consequences for final flux data Summary

3 Measurement Site: Wetzstein, Thuringia, Germany, flux measurements established end of 2001 main tower tower C tower B tower D tower A measuring heights: Main tower: 30.0m Tower C: 29.4m ADVEX’06 (April 11– June 19, 2006) flux measurements for , H, E, CO 2 CO 2, wind and temperature profiles

4 The ADVEX Experiment Advection experiment CarboEurope-IP: 4 towers around the main tower: A, B, C, D: profiles of [CO 2 ], T, u‘, v‘, w‘, T‘, tower B with CO 2 -fluxes below canopy, tower C and main tower with CO 2 -fluxes above canopy 60m

5 Why care about advection? Eddy covariance theory is derived from tracer conservation equation with many simplifications which are only valid under homogeneous conditions

6 Flux Calculation All fluxes are calculated in the following steps: Calculation of planar fit planes (Wilzcak et al., 2001) → comparison with 2D-rotation Determination of CO 2 - and H 2 O-lags for closed path analysers Determination of H 2 O-lag dependency on VPD → modelling Determination of spectral correction according to Eugster & Senn (1995) for closed path analysers, Webb et al. (1980) correction for open path analysers

7 Data gaps are due to Maintenance interruptions, power failures, ice coating Instrumental problems Non-turbulent conditions Unfavoured wind directions (tower effects, heterogeneous terrain) Precipitation, fog events (open path analyser) high wind speeds

8 Wetzstein, main tower data gaps (closed-path analyser) Jan 1 – Aug 24, 2006

9 Wetzstein, main tower and tower C Apr 11 – Jun 19, 2006 data gaps caused by maintenance, power failures etc.

10 stepMain tower (TM) Tower C (TC) 1 (maintenance etc) 3.6%4.8% 2 (after pre-selection) 3 (after stationarity test 1)

11 Wetzstein, main tower and tower C Apr 11 – Jun 19, 2006 time series of CO 2 -fluxes after pre-selection (eg Vickers & Mahrt 1997, JAOT14)

12 Wetzstein, main tower and tower C Apr 11 – Jun 19, 2006 data gaps after pre-selection stepMain tower (TM) Tower C (TC) 1 (maintenance etc) 3.6%4.8% 2 (after pre-selection) 4.5%30.2% 3 (after stationarity test 1) 30.2%

13 Wetzstein, main tower and tower C which data are rejected in case of open path-analyser? 24 of 624 half-hours (3.8%) rejected April 30 – May 12, 2006, dry period

14 Wetzstein, main tower and tower C which data are rejected in case of open path-analyser? 263 of 630 half-hours (41.7%) rejected!!! May 13 – 28, 2006, rainy period

15 Wetzstein, main tower and tower C Apr 11 – Jun 19, 2006 consequences for dependencies on meteorological variables Michalis-Menten-relationship: see Falge et al. 2001, AFM107 NEE: net ecosystem exchange (µmol CO 2 m −2 s −1 ) PPFD: photosynthetic photon flux density (µmol quantum m −2 s −1 ) a: ecosystem quantum yield (µmol CO 2 ) / (µmol quantum) F GPP,sat : gross primary productivity at saturating light (µmol CO 2 m −2 s −1 ) R day : ecosystem respiration during the day (µmol CO 2 m −2 s −1 ) TMTC a0.0570.061 F GPP,sat 24.627.6 R day 5.44.1 r2r2 0.660.58

16 Wetzstein, main tower and tower C Apr 11 – Jun 19, 2006 consequences for dependencies on meteorological variables Michalis-Menten-relationship: see Falge et al. 2001, AFM107 NEE: net ecosystem exchange (µmol CO 2 m −2 s −1 ) PPFD: photosynthetic photon flux density (µmol quantum m −2 s −1 ) a: ecosystem quantum yield (µmol CO 2 ) / (µmol quantum) F GPP,sat : gross primary productivity at saturating light (µmol CO 2 m −2 s −1 ) R day : ecosystem respiration during the day (µmol CO 2 m −2 s −1 ) TMTM, TC av TC a0.0570.0630.061 F GPP,sat 24.623.227.6 R day 5.45.14.1 r2r2 0.660.590.58

17 Wetzstein, main tower and tower C time series of CO 2 -fluxes with stationarity tests May 8 – 14, 2006

18 Wetzstein, main tower and tower C Apr 11 – Jun 19, 2006 When do instationaries occur? Instationarities occur mainly at low or zero radiation conditions

19 Wetzstein, main tower and tower C Apr 11 – Jun 19, 2006 data gaps summary stepMain tower (TM) Tower C (TC) 13.6%4.8% 2 (after pre-selection) 4.5%30.2% rainy, moist conditions 3 (after stationarity test 1) 9.8%33.2% Low radiation conditions

20 Do we have perfect data now? Are these data reliable as input for gap filling procedures? Still missing: advective processes night flux treatment reliability check

21 Hainich Drainage/advective fluxes Data from W. Kutsch

22 Night-flux problem Weak turbulence Instrumental problems, large footprints, gravity waves Turbulent flux is influenced by other transport/storage processes →Site dependent see eg: Lee, 1998 Aubinet et al, 2003, 2005 Staebler and Fitzjarrald, 2004 Feigenwinter et al, 2004

23 Night-flux corrections Empirical: Separate calm and turbulent periods, remove calm periods, fill the gap u*-criterion mostly used

24 Aubinet et al. AER30, 2000 NEE night versus u*

25 Wetzstein NEE 2005, unrealistic high night-time fluxes

26 Wetzstein when do high fluxes occur? u*>0.4m s-1 wind direction between 200° and 280° or 30° and 40° neutral atmospheric conditions: stability parameter: -0.0625<ζ<0.0625 (determined by M. Zeri) → turbulent upwind mixing from the valley

27 Wetzstein NEE 2005 after application of MZ criteria for 2005: 72% data available 58% data available

28 Wetzstein NEE 2005 after application of MZ criteria

29 Wetzstein night-time NEE 2005 after application of MZ criteria R 10 =3.9 R 10 =3.0

30 Wetzstein NEE comparison during advection experiment after application of MZ criteria

31 Summary Amount of data gaps strongly depending on: site type of quality check (still no common agreement in CarboEurope-IP!) type of analyser, weather pattern threshold criteria for u* (have to be objective, Gu et al. AFM128, 2005) Derived dependencies on meteorological variables vary with data left after selection → biased datasets Reliability has to be tested against chamber and biometric measurements

32 Thanks for your attention! Questions?


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