What you’re seeing is differences in air density caused by updrafts and downdrafts over the hot ground. The actual air patterns, which you can’t directly see, look something like a [Rayleigh-Taylor instability](https://en.wikipedia.org/wiki/Rayleigh%E2%80%93Taylor_instability) – you can imagine a heat shimmer as something like “anything in the purple bit of that diagram gets deflected a bit”.
Since these updrafts form mostly vertical columns, the number of different columns you go through depends on your horizontal angle. More horizontal lines of sight and more distant objects pass through more columns and therefore are more distorted, while more vertical lines of sight and closer-by objects pass through fewer and are less distorted.
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