Estimating the carbon fluxes of forests with an individual-based forest model

HIGHLIGHTS

• who: Edna Rödig from the clay loam soil type as in Maidment (1993)The calibrated parameterization (M2) is based on parameters derived from a numerical calibration against the NEE, GPP and respiration data (Lehmann and Huth, see Additional file , for details). The filter-based parameterization (M3) arose from filtering the EC data (same data as used for calibration of, ) for optimal climatic conditions (see Field data and data filtering) to isolate individual processes. Model functions were directly fitted through filtered data to derive new parameter values and a new temperature reduction curve (Eq., ). All model setups . . .
  

   

  

  If you want to have access to all the content you need to log in!

  Thanks :)

  Username or Email

  Password

  Remember me

  Lost your password?

  If you don't have an account, you can create one here.