Temperature Shocks: Growth and Unemployment in the EU
There are lots of shocks hitting the European Union (EU), for example Energy Shocks and Floods, Drought and Heat Waves. In this post, I'm going to look at the effect of Surface Temperature shocks on the EUL20 Model.
The EUL20 Model has three component state variables: EU1 = (Growth), EU2 = (CO2-LU) and EU3 = (LU-GDP-N), that is, Overall Growth, a controller for CO2 Emissions-Unemployment (LU) and a controller for Unemployment-Output-Population. From the shock decomposition diagram above, a global temperature shock has negative effects on all three state variables (see the EUL20 TEMP Model below). In each case, the system responds positively after a few years but does not return to full equilibrium until around ten years. In other words, repeated yearly temperature shocks will cumulate and continue damaging the economy over time.
Additionally, over time, surface temperatures in the EU are expected to keep rising above 1930 levels, amplifying shock effects--even thought the shocks themselves, in standard deviation units, are small.
Also, the EUL20 TEMP Model below has one unstable component, the Unemployment-Output-Population, while the CO2-LU controller is stable and explains more variation.
Notes
You can run the EUL20 Model yourself using R-code on my Google Site. The EUL20 Model itself is stable and forecast to reach a steady state around 2046.
- NY Times, Aug 14, 2026 Heat Is Hammering Europe, Again. Here's What That Looks Like. Extreme temperatures and repeated wildfires are pushing infrastructure to the limit and testing the continent's resolve.
- NY Times, Aug 15, 2026 In One Week During Europe's Record Heat Wave, Deaths Increased by 16,000.
- NY Times, Aug 14, 2026 Why Europe Keeps Being Pummeled by Heat Waves The whole planet is warming, but changes in weather patterns could help explain why the continent is suffering so many bouts of severe heat.
- Nature, 21 November 2024 Heat stress and the labour force.
- Blog Roll: The European Union (EU) More postings of interest.
Questions
Use the Direct Graph above (based on the Kaya Identity) to understand the effects of positive and negative feedback effects (dashed lines) from a Global Temperature (T) SHOCK.
- How might the (CO2-LU) controller work in the face of a Global Temperature shocks?
- How might the (LU-GDP-N) controller work in the face of Global Temperature shocks?
- How might instability (a > 1.0, unstable economic growth) affect the Unemployment-Output-Population controller?
- How else might increasing Global Temperature levels affect the EU economies?
- What might be done to mitigate the effects of Heat Waves? Consider modifying the "intensive coefficients" (n,u=normal rate of unemployment,q,e,c,t and a=growth rate of production).
EUL20 Measurement Model
EUL20 TEMP Model
The EUL20 TEMP Model (above) is unstable from the unstable Unemployment-Output-Population controller. Notice that the TEMP coefficients in the G matrix are all negative meaning that increases in global temperature have a negative effect in the EU model.
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