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Interannual Variability in the ChEAS Mesonet

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A simple model with explicit phenology can capture the IAV across sites only ... step: Simple model with fixed phenology. Limited convergence on IAV from ... – PowerPoint PPT presentation

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Title: Interannual Variability in the ChEAS Mesonet


1
Interannual Variability in the ChEAS Mesonet
ChEAS XI, 12 August 2008 UNDERC-East, Land O
Lakes, WI Ankur Desai Atmospheric Oceanic
Sciences, University of Wisconsin-Madison
2
Whats the Deal?
  • Interannual variation (IAV) in carbon fluxes from
    land to atmosphere are significant at most flux
    sites
  • Key to understanding how climate affects
    ecosystems comes from modeling IAV
  • IAV (years-decade) is currently poorly modeled,
    while hourly, seasonal, and even successional
    (century) are better

3
Can we simulate this?
4
Sipnet
  • A simplified model of ecosystem carbon / water
    and land-atmosphere interaction
  • Minimal number of parameters
  • Driven by meteorological forcing
  • Still has gt60 parameters
  • Braswell et al., 2005, GCB
  • Sacks et al., 2006, GCB added snow
  • Zobitz et al., 2008

5
Results
6
2 years 7 years
1997
1998
1999
2000
2001
2002
2003
2004
2005
7
Ricciuto et al.
8
Ricciuto et al.
9
Our region
10
Any coherence?
Desai et al, 2008, Ag For Met
11
Cross-site IAV
  • Hypothesis IAV in flux towers in the same region
    are coherent in time
  • Hypothesis Simple climate driven models can
    explain this IAV
  • Growing season length
  • Climate thresholds
  • Mean annual precip

12
A whole bunch of data
13
Coherence?
14
Growing season and IAV
  • Does growing season start explain IAV?
  • Can a very simple model be constructed to explain
    IAV?
  • Hypothesis growing season length explains IAV
  • Can we make a cost function more attuned to IAV?
  • Hypothesis MCMC overfits to hourly data

15
Hello again
16
The model
  • Driven by PAR, Air and Soil T, VPD, (Precip)
  • LUE based GPP model f(PAR,T,VPD)
  • Three respiration pools f(T, GPP)
  • Output NEE, ER, GPP, LAI
  • Sigmoidal GDD function for leaf out
  • Sigmoidal Soil T function for leaf off
  • 17 parameters, 3 are fixed
  • Desai et al., in prep (a)

17
The optimizer
  • All flux towers with multiple years of data
  • Estimate parameters with Markov Chain Monte Carlo
    (smart random walk)
  • Written in IDL

18
MCMC
  • MCMC is an optimizing method to minimize
    model-data mismatch
  • Quasi-random walk through parameter space
    (Metropolis)
  • Start at many random places (Chains) in prior
    parameter space
  • Move downhill to minima in model-data RMS by
    randomly changing a parameter from current value
    to a nearby value
  • Avoid local minima by occasionally performing
    uphill moves in proportion to maximum
    likelihood of accepted point
  • Use simulated annealing to tune parameter space
    exploration
  • Pick best chain and continue space exploration
  • Requires 100,000-500,000 model iterations (chain
    exploration, spin-up, sampling)
  • End result best parameter set and confidence
    intervals (from all the iterations)
  • Cost function compared to observed NEE

19
New cost function
  • Original log likelihood computes sum of squared
    difference at hourly timestep
  • What if we also added monthly and annual squared
    differences to this likelihood?
  • Have to scale these less frequent values
  • Have to deal with missing data

20
I like likelihood
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26
Regional IAV
  • How well do we know regional (scaled-up) IAV?
  • Do top-down and bottom-up regional flux
    estimation techniques agree on IAV (if not
    magnitude)?
  • What controls regional IAV?
  • Wetland IAV vs Upland IAV
  • Step 1 Scale the towers

27
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28
Heterogeneous footprint
29
Scaling with towers
  • NEP (-NEE) at 13 sites
  • Stand age matters
  • Ecosystem type matters
  • Is interannual variability coherent?
  • Are we sampling sufficient land cover types?

30
Desai et al., 2008, AFM
  • Multi-tower synthesis aggregation
  • parameter optimization with minimal 2 equation
    model

31
Tall tower downscaling
  • Wang et al., 2006

32
Scaling evaluation
  • Desai et al., 2008

33
Next step
  • Use our IAV model with all 17 (19) flux towers -
    estimate parameters for each
  • Use better landcover and better age distribution
    from NASA project
  • Upscale again - this time over long time period
  • This experiment for Northern Highlands 1989-2007
    (Buffam et al., in prep)

34
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36
Many years of flux
37
Regional coherence?
  • Desai et al., in prep

38
Regional coherence?
39
Conclusions
  • There is some coherence in IAV across ChEAS
  • Better statistical method to show this?
  • A simple model with explicit phenology can
    capture the IAV across sites only with a better
    likelihood function
  • Next step Simple model with fixed phenology
  • Limited convergence on IAV from regional methods

40
Other things
  • Sulman et al., in prep - the role of wetlands in
    regional carbon balance
  • Lake Superior carbon balance from ABL budgets
    (Atilla, McKinley) - Urban et al, in prep
  • Small lakes in the landscape (Buffam, Kratz)
  • Successional trends and modeling (Dietze)
  • Hyperspectral remote sensing (Townsend, Serbin,
    Cook)
  • Top-down CO2 budgets in valeys and complex
    terrain (Stephens, Schimel, Bowling, deWekker)
  • CH4 (pending), advection (pending - Yi), urban
    micromet and biogeochem (pending)
  • NEON? (Schimel, UNDERC)

41
Thanks
  • Desai lab http//flux.aos.wisc.edu
  • Ben Sulman, Jonathan Thom, Shelly Knuth
  • DOE NICCR, NSF, UW, DOE, NASA, USFS, Northern
    Research Station, Kemp NRS
  • All the tower people

42
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