Insights on the role of accurate state estimation in coupled model parameter estimation by a conceptual climate model study

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Abstract

The uncertainties in values of coupled model parameters are an important source of model bias that causes model climate drift. The values can be calibrated by a parameter estimation procedure that projects observational information onto model parameters. The signal-to-noise ratio of error covariance between the model state and the parameter being estimated directly determines whether the parameter estimation succeeds or not. With a conceptual climate model that couples the stochastic atmosphere and slow-varying ocean, this study examines the sensitivity of state-parameter covariance on the accuracy of estimated model states in different model components of a coupled system. Due to the interaction of multiple timescales, the fast-varying "atmosphere" with a chaotic nature is the major source of the inaccuracy of estimated state-parameter covariance. Thus, enhancing the estimation accuracy of atmospheric states is very important for the success of coupled model parameter estimation, especially for the parameters in the air-sea interaction processes. The impact of chaotic-to-periodic ratio in state variability on parameter estimation is also discussed. This simple model study provides a guideline when real observations are used to optimize model parameters in a coupled general circulation model for improving climate analysis and predictions.

Figures

  • Table 1. List of the successful (S) and failed (F) parameter estimation (PE) cases with partial state estimation (SE) in eight PE experiments (in the parenthesis is the experiment serial number).
  • Table 2. List of root mean square errors of the state variable and the parameter during the last 100 TUs in eight PE experiments.
  • Figure 1. Time series of the ensemble mean (solid line) of the estimated parameter a2 using observations of w (i.e., w-to-a2) with state estimation (SE) of (a) both the atmosphere (x1,2,3) and ocean (w) from x2 and w observations and (b) only w with the w observations. The dashed line marks the “true” value of the parameter a2 and the shaded area represents the range of ensemble.
  • Figure 2. Time series of ensemble means (solid line) of the estimated parameter a2 in three experiments, (a) x2-to-a2 (using x2 observations to estimate a2) with SE for both x1,2,3 and w, (b) x2-to-a2 with SE for x1,2,3 only, (c) w-to-a2 with SE for x1,2,3 only. Any other notations are the same as in Fig. 1.
  • Figure 3. Time series of ensemble means of the estimated parameter c2 in three experiments, (a) w-to-c2 (using w observations to estimate c2) with SE for both x1,2,3 and w, (b) x2-to-c2 (using x2 observations to estimate c2) with SE for x1,2,3 only, (c) w-to-c2 with SE for x1,2,3 only. Any other notations are the same as in Fig. 1.
  • Figure 4. Time series of the state variables from the w-to-c2 PE experiment, for (a) and (d) x2, (b) and (e) w, (c) and (f) η. The upper panels (a), (b) and (c) are from the successful case with SE for x1,2,3, and the lower panels (d), (e) and (f) are from the failed case with SE for w. Any other notations are the same as in Fig. 1.
  • Figure 5. Time series of the ensemble of parameter c6 from the η-to-c6 (using η observations to estimate c6) PE experiment in four different state estimation settings: (a) x1,2,3, w and η; (b) x2 only; (c) w and η only; and (d) η only. Any other notations are the same as in Fig. 1.
  • Figure 6. Wavelet analyses for (a) x2 and (b) w in the truth model run.

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Yu, X., Zhang, S., Lin, X., & Li, M. (2017). Insights on the role of accurate state estimation in coupled model parameter estimation by a conceptual climate model study. Nonlinear Processes in Geophysics, 24(2), 125–139. https://doi.org/10.5194/npg-24-125-2017

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