1 / 16

Examples for the trial-and-error method

Examples for the trial-and-error method. gravity modeling. Waveform modeling. Sidao Ni et al. Science 296 , 1850 (2002). Chen et al. 2007. SA exmaple. F(x,y) has its global maximum value of 1.0 at x = 0, y = 0. However, it also has several secondary maxima. Error function.

saratdavis
Télécharger la présentation

Examples for the trial-and-error method

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Examples for the trial-and-error method • gravity modeling

  2. Waveform modeling Sidao Ni et al. Science 296, 1850 (2002)

  3. Chen et al. 2007

  4. SA exmaple F(x,y) has its global maximum value of 1.0 at x = 0, y = 0. However, it also has several secondary maxima Error function global maximum at (0, 0)

  5. Effect of T on pdf distribution T = 1 T = 10 T = 0.1 T = 0.01 The effect of this temperature T is to exaggerate or accentuate the differences between different values of the error function.

  6. Figure 4.5. For a model with 8 model parameters (each having 8 possible values) heat bathalgorithm starts with a randomly chosen model shown by shaded boxes in (a). Each modelparameter is then scanned in turn keeping all others fixed. (b) shows scanning through themodel parameter m 2. Thus m26 is replaced with m23 and we have a new model described byshaded boxes in (c). This process is repeated for each model parameter.

  7. Figure 4.6. Model generation probabilities (left) and their corresponding cumulativeprobabilities (right) at different temperatures. At high temperature, the distribution is nearly flatand every model parameter value is equally likely. At intermediate temperature, peaks start toappear and at low temperature, the probability of occurrence of the best solution becomes veryhigh. A random number is drawn from a uniform distribution and is mapped to the cumulativedistribution (fight) to pick a model.

  8. Application of heat bath SAseismic waveform inversion Tk = T0(0.99)k (k: number of iteration) 100 iterations

  9. Real data inversion: SA

  10. 11 models that gave a correlation value of 0.74 or greater

  11. Neighborhood Algorithm(Sambridge, 1999, GJI)

More Related