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The Wind Vane: Measuring Direction and Gust
Karen

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Karen

23. september 2026SE
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The Wind Vane: Measuring Direction and Gust

The anemometers already published here measure how fast the wind blows. This rung measures where it comes from — which, for forecasting, is the more useful half. A vane is a fin on a bearing with more area behind the pivot than in front, so it weathercocks into the wind. That sounds trivial and is not: a vane that is too light chases every eddy and never settles, one that is too heavy lags real shifts, and one balanced wrongly sits at an angle in a steady breeze. The behaviour you want is a specific amount of damping, and it is a design choice. By convention the direction reported is where the wind comes FROM. A northerly is cold and from the north; the same air moving would be called a southward flow by anyone else. It is a genuine trap and it has reversed more amateur observations than any other rule.
Miðlungs
1 day

Leiðbeiningar

1

Get the balance and the area right

Make the tail broad and the nose short and weighted, then balance the whole assembly on the pivot so it sits level with no wind. Area behind the pivot produces the turning moment; mass in front brings the centre of gravity onto the pivot so gravity does not bias it. An unbalanced vane reads a false direction that changes as the mast settles out of plumb — and because the bias is constant, it looks exactly like a genuine prevailing wind.

Efni fyrir þetta skref:

KrossviðarplataKrossviðarplata1 plata
TrétappiTrétappi2 stykki

Nauðsynleg verkfæri:

HandsögHandsög
SandpappírSandpappír
2

Use a real bearing, mounted vertically

Run the spindle in a ball bearing, or at minimum a hard point in a cup, and mount the mast truly vertical. Friction sets the lightest wind the vane can respond to — the starting threshold — and a stiff bearing means your record simply has no data below about 2 metres per second. A mast out of plumb makes the vane drift toward the downhill side whenever the wind drops, which fills calm periods with a fictitious direction.

Efni fyrir þetta skref:

KúlulegaKúlulega2 stykki

Nauðsynleg verkfæri:

ReglustikaReglustika
3

Orient the fixed points to TRUE north

Fix the cardinal markers by true north, found from the sun at local noon or from a compass corrected for your local magnetic declination. Declination reaches well over ten degrees in many places and it changes slowly year on year. An uncorrected vane reports every wind rotated by that amount, consistently, and no amount of careful reading will reveal it. Write the declination you used and the date in the station notebook.

Efni fyrir þetta skref:

KartonpappírKartonpappír4 stykki

Nauðsynleg verkfæri:

ÁttavitiÁttaviti
4

Mount it high and clear, and say how high

The standard is 10 metres above open ground. Few gardens allow that; mount as high and as clear as you safely can, and record the actual height and the surroundings. Wind speed and direction both change with height and with obstacles, so a reading at 3 metres in a garden is a real measurement of a different thing, not a bad measurement of the standard one. The notebook turns it from an anecdote into data by saying exactly what was measured.

Efni fyrir þetta skref:

TrétappiTrétappi2 stykki
Galvaníseraðir naglarGalvaníseraðir naglar20 stykki

Nauðsynleg verkfæri:

MálbandMálband
KlóhamarKlóhamar
5

Record the mean and the range, over a stated period

Watch for a full ten minutes, and record both the average direction and the range it swung through — for example 'WSW, varying 230 to 270'. A single instantaneous direction is nearly meaningless because wind is gusty by nature. The RANGE is itself information: a narrow range means a steady airstream and often a settled situation, while a wide, wandering range often means light winds and a col, where the next day is hardest to forecast.

Nauðsynleg verkfæri:

SkeiðklukkaSkeiðklukka
6

Damping, thresholds and reading a wind rose

Hleð Jupyter-vinnubók…

Efni

5

Nauðsynleg verkfæri

7
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