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oscarbranson committed Feb 9, 2024
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Expand Up @@ -19,7 +19,7 @@ As air parcels are transported by meandering jets and eddies, they trace out cha

Our goal in this section is to build a mathematical model for the temperature of the atmosphere as a function of latitude and time. Since we will be relating changes in temperature to heat, we need to introduce the heat capacity of the atmosphere, $C_a$. Changes in heat, $\Delta Q$, are then related to changes in temperature, $\Delta T$ according to $\Delta Q=C_a \Delta T$.

```{figure} ../figures/atmosphere_flux_sketch.png
```{figure} ../figures/atmosphere_flux_fig.png
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name: fig:atmosphere_flux_sketch
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