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Working demo including extracting the timeseries for positions within…
… the field. No doublecheck on the realism yet. At a glance it looks like our spatial variance is very small, because we assume a 1 second spatiotemporal resolution. That means our crosswind distances for large cloud velocities are actually very large, which is to say that many along-wind spaced points get the exact same time series with only temporal shifting. That could be good or bad depending on your point of view. Maybe "it is what it is" for the Lave scaling case, but this could be a contribution that I make to the methodology.
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