He ran an energy model with built-in learning curves and showed that with exactly the same model (same equations, all same data inputs, costs, etc.) you can get radically different energy pathways with similar total costs:
Case 1 is coal-heavy while Case 2 has lots of PV. They cost roughly the same.
Case 2 is different because large investments get triggered early for PV and other technologies, which take them down the learning curve, saving costs later in the simulation:
This phenomenon, that technology investments and learning now can save costs later, was well understood by the fathers of the German renewable subsidies programmes, Hermann Scheer and @HJFell, which brought down the costs of PV.
How can the same model deliver such different results?
Because learning curves introduce non-convexities into the optimisation.
This leads to local optima in the solution space.
Depending on where the solver starts looking (green/blue), you end up in different optima:
If the solver starts its search on the left and looks for decreasing cost, it lands at the blue low-PV, high-coal optimum.
If it starts on the right, it lands in the green high-PV optimum.
It's hard to build solvers to find these different solutions, so they're often ignored.
This diversity often goes unacknowledged in the energy modelling world where models that have endogenous learning curves aren't used to explore all solutions. (Please correct me if I'm wrong.)
Policy-wise, this general phenomenon of path dependency shows how we can choose (within limits) how we steer our technology investment towards solutions that society wants (e.g. high acceptance, high co-benefits, etc.).
Conclusion: there are lots of different possible low-cost low-emission energy systems out there, depending on which technologies we choose to invest in.
Now for some more technical details.
This is NOT the same as the near-optimal solutions that crop up in the Method to Generate Alternatives, since those solutions are convexly connected to the global optimum. Here we're talking about far-away distinct near-optimal solutions.
Niclas has some comments on this:
What about models that approximate the non-linear learning curves with a piecewise linearisation to turn it into a MILP? (A technique Niclas co-invented with Sabine Messner)
Niclas has a trick to find the local optima by forcing constraints and seeing if they become non-binding:
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I'd also be interested in the question posed the other way round: what is the value of "firm" clean generation in the presence of VRE, batteries and long-term storage?
E.g. how much does system cost reduce by adding nuclear/CCS etc. to wind+solar+batteries+hydrogen.
Either way, the system costs of all these options is in a similar ball park, which throws up the question:
What do we actually want?
What can we build quickly, with wide public approval?
- end of coal
- efficiency
- electrification
- renewables (he developed first hydro power)
- open data
- technological learning ("tendency of progress is to quicken progress")
Electrolysis was also the means of making heavy water (D2O), a neutron moderator, from its discovery in the 1930s until the GS process replaced it in the mid-1940s.
Heavy water was crucial for making the atomic bomb.
This made electrolysis of great military importance in WWII.
"VRE cannibalisation is a policy artefact, not a physical system constraint"
Short version:
Some studies show that average revenues for wind and solar go down with rising share.
We show that the studies have an implicit assumption that variable renewable energy (VRE) are forced into the system, which depresses prices and their own market value (MV).
This toy model meets a constant demand over a year of weather data
The default setting is to use wind, solar, batteries and hydrogen storage only; further technologies can be added, as can H2 demand (for heavy transport and industry)
In this example for a 100 MW demand in Germany, when wind (blue) and solar (yellow) generation exceed demand (black line), electricity is stored (negative values) in batteries (grey) or used to electrolyse water to hydrogen (cyan), which is then stored underground