My suggestion would simply be to see if yours can be compared to a known one, perhaps in yacht-club, flying-club or similar.
I have read a description of the use of a vane-type anenometer used in an unusual experiment, that in turn led me to consider a particular aspect of wind behaviour. It exploited the point that such a vane will indicate direction as well as force, but only while the wind is moving perpendicularly to the vane.
You sometime hear art-critics waffling about the "resonance" of an auditorium or cathedral – the same people who muddle "acoustic" (adj.) with "acoustics" (noun) – when clearly they mean "reverberation". Yes, the air in the hall can resonate, just as the air in a bottle resonates when you blow across its top, but at fractional-Hz frequency. It can also happen in Nature…
The experiment, carried out in America, investigated the resonance in a cave observed to have a regularly reversing draught in a fairly narrow passage leading from the entrance to a large chamber. The vane, made from a sheet of plastic, was suspended from a spindle carrying a potentiometer as the transducer for a data-logger, so that it would read the wind's direction as a polarity oscillation, as well as its relative speed by displacement.
The acoustics did indeed match the nature predicted by theory, treating the cave as a flue-type organ-pipe with closed end, to reasonable certainty. I think they tried it in other caves but these were more complicated, giving less certain results.
I had noticed the same effect in a cave I helped discover in Norway, a single passage descending steeply to an air-tight choke of sand; and breathing" due to the wind blowing across its entrance. Indeed, we named it "Breathing Cave" , or "Pustehohle" if I recall its translation correctly.
So I tried to apply the American results to an exploration project in which I am involved on the Mendip Hills, but the same fairly simple maths predicted a volume too large to fit under the hill! Despite the apparent regularity of the draught reversals, we decided the cause was simply fluctuations in the wind blowing across the open top of the vertical entrance shaft; lined with concrete pipes for its first 30 feet depth from their rim a little above the field level.
This does though raise an intriguing question:
– Does the wind itself, blowing over a suitable edge, create a high-amplitude, sub-Hertz sound, different from the irregular gusts? In that location the edge is created by the steep SW face of the Mendip Hills, rising from a plain to a gently-undulating plateau surface. (The cave is not far to the East of Cheddar Gorge, so fairly close to the edge of the range; and the Gorge itself could also act as an acoustic lip.) So the cave's draught was influenced by the acoustic wave rather than the simple gusts marking turbulence in the air stream.
As our "dig" has progressed gradually downwards through an interminable mass of irregular boulders the "breathing" effect has largely disappeared; and the very chilly draught now, although weather-controlled, is generally fairly steady in direction and force.
Further to my thoughts are the shapes of some types of cloud cover, forming quite regular, parallel ridges of fluffy vapour separated by clear air. Though I have not often flown, I have seen from aeroplanes, strikingly regular swell effects on cloud cover lying below the flight path. Again, a very low frequency sound marked in clouds either by piling the vapour mass into waves analogous to sea-swells, or perhaps, by the sound-waves' compression and rarefaction controlling the vapour's condensation into concentrated regions.
'
That cave dig has an unlikely model-engineering link. We made for it a simple winch, revolving on plastic bushes on a cross-bar on a scaffolding tripod. The hexagonal side-frames about 3 feet across-corners, are welded from flat steel bar originally rails from a dismantled miniature railway!