So after a saga of resolving issues that I will not bore you with we finally have some results for the concentration runs! (The emission driven runs are having some issues with convergence). Anyways before thinking about what the calibration results tell us about the models I wanted to check to check the following…
Well the first thing I wanted to do was see if the optim runs even worked by checking the convergence.
How many models did we calibrate to?
## [1] 35
How many were actually successful?
## [1] 21
Which models were unsuccessful? What did their final characterization look like before optim gave up?
| model | S | alpha | diff | volscl |
|---|---|---|---|---|
| ACCESS1-3 | 38.81 | 1.99 | 16.20 | 1.81 |
| CESM1-BGC | 2.21 | 1.47 | 0.00 | 0.51 |
| CESM1-FASTCHEM | 3.13 | 0.68 | 539.59 | 5.00 |
| CESM1-WACCM | 1.91 | 1.06 | 0.00 | 0.27 |
| CMCC-CESM | 1.90 | 2.48 | 0.00 | 0.04 |
| EC-EARTH | 2.11 | 1.81 | 0.00 | 0.54 |
| FGOALS-g2 | 1.68 | 2.12 | 0.00 | 0.04 |
| GISS-E2-H-CC | 23.02 | -0.81 | 190.59 | 4.66 |
| GISS-E2-R-CC | 32.05 | 0.40 | 218.55 | 3.59 |
| IPSL-CM5B-LR | 4234.96 | -0.44 | 252.13 | 4.50 |
| MPI-ESM-MR | 2.18 | 1.84 | 0.02 | 0.46 |
| MPI-ESM-P | 3.02 | 0.29 | 394.35 | 4.43 |
| MRI-CGCM3 | 755.60 | 1.64 | 49.26 | 1.99 |
| MRI-ESM1 | 0.24 | 3.23 | 0.19 | 1.32 |
Some of these values are what I call ridiculous, like sure Hector could have a Hector climate sensitivity of 4,234 but that seems unlikely to me. Some of these models that failed have what I presume to be a related model converge. For example ACESS1-3 failed to converge but ACCESS1-0 converged. I think that I could try using the parameterization of ACESS1-0 to see if that would be a better initial parameter guess for optim.
For the models that do not have parameter values from a related converged optim run, like EC-Earth, FGoals-g2, and the MRI-models I wonder if the calibration before we added the volscl parameter would be a useful starting point.
Did the parameterization before the volscl work?
How many times did the calibration fail to converge?
## [1] 0
:rock_on:
So to me this means that we can use the before volscl calibration results as starting initial param values.
So the reason why we added the the volcanic scalar was because we were saw Hector was underestimating global mean temperature because it had no mechanism to emulate the ESM response to volcanoes. Did adding the volscl to the calibration help with the under estimation of CMIP Tgav during the historical period?
These plots compare the hector (with the volsc calibrated), the CMIP5 comparison data being calibrated to and hector novolsc (an earlier version of hector where volsc was not a hector parameter yet.) I only plotted the comparison data for the historic period where we are seeing all the problems with the volcanoes.
It looks like the two hector runs (the less with the less squiggles) are different from one another and typically there is one of these lines closer to the CMIP models than the others. It will probably be more useful to look a the individual comparison plots on the next tab.
For the most part the hector calibrated with the volscl looks better than the hector calibrated without. However that does not seem to be the case for the CMCC model family or NorESM1-ME. Which is interesting.
How does adding the volsc change the values for the other parameters? (Only for the calibration that converged).
| param | calibration | min | mean | max | sd |
|---|---|---|---|---|---|
| alpha | novol | -0.15 | 1.57 | 2.45 | 0.58 |
| vol | -0.21 | 1.51 | 2.29 | 0.58 | |
| diff | novol | 0.00 | 2.95 | 20.41 | 4.50 |
| vol | 0.00 | 16.99 | 265.98 | 57.31 | |
| S | novol | 0.67 | 3.46 | 18.93 | 3.18 |
| vol | 0.22 | 5.50 | 44.19 | 9.04 | |
| volscl | vol | -0.36 | 1.09 | 3.60 | 0.84 |
Hmmmm the there a really large diff value for the experiments that use the volscl I wonder if that is an outlier or is expected?
Looks that that diff value is an outlier, what model has that large diff value and what does the rest of the distribution.
## model calibration param value
## 1 inmcm4 vol diff 265.9785
When we subset the diff parameter space so that is excludes the outlier, it looks like the hector calibration with the volscl also has larger values of diff where as hector calibrated without the volsc is skewed closer to 0.
What happens to S when we remove the outliers?
The IQR is warmer for the S values from the vol calibration experiment.