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Lesson 07 of 0920 minBeyond SKYWARN

Proving rotation

The technique that separates rotation from drift, the minimum time it takes, and why a photograph can never be a rotation report.

By the end of this lesson
M4.7.aApply a fixed-reference-point method to assess apparent motion.
M4.7.bState a minimum observation window before reporting rotation.
M4.7.cDistinguish rotation from horizontal scud drift.
M4.7.dExplain why time-lapse is a review tool and not a basis for a real-time report.

Pick something that cannot move

The eye is bad at this. A whole storm base translating across the sky, seen against nothing, reads as motion in whatever direction you were already expecting. The fix is to stop judging the cloud against itself and judge it against something fixed: a power pole, a tower, the corner of a roof, a tree on the horizon.

Two panels of the same storm base with a power pole in the foreground. In the left panel, marked drift, three cloud fragments all travel the same direction past the pole. In the right panel, marked rotation, a lowering hangs beneath the base with its far side travelling right past the pole and its near side travelling left, so the two sides disagree.
The test in one picture. Everything going the same way is drift. Two sides going opposite ways, converging on a point, is rotation.WxAlerts
  1. Choose the reference before you start watching. Choosing it afterwards means choosing it to fit what you already believe.
  2. Watch for a full minute or two. Not a glance. Not one photograph.
  3. Look for the near and far sides disagreeing. A vertical-axis rotation seen from the side shows its far side tracking one way across your reference while its near side tracks the other. Everything travelling together is drift, however fast it looks.
  4. Look for convergence. Material tightening toward a single point, not just circling, is what distinguishes a developing funnel from a ragged base being blown along.
  5. Check it is still doing it. Persistence is the discriminator. One apparent turn is not a report.

How long is long enough

A minute or two feels like a long time with a storm in front of you, and it is the difference between a report an office trusts and one that costs your network credibility. The Field Guide's instruction when you are unsure is simply to continue to observe the feature. There is no shame in a delayed report; there is real cost to a wrong immediate one.

What a camera cannot do

A still photograph contains no motion, so it cannot show rotation. It can show a shape that a person then describes as rotating, which is not the same thing and is how a great many bad reports get corroborated after the fact.

Time-lapse is genuinely useful and genuinely misleading. Speeding footage up reveals rotation the eye misses in real time, which makes it a good review tool for learning what you missed. It is not a basis for a live report, because by the time you have shot and played back a sequence, the report is late and the office needed it during the warning.

Knowledge checkNot graded · the exam draws a fresh variant of this item

A ragged lowering is moving quickly across the sky. Every part of it, near side and far, travels left to right at about the same speed. Rotation?

Rotation requires two parts of a feature to disagree about which way to go.
Sources for this lessonNWS Northern Indiana, "Low hanging clouds mistaken for Funnel Clouds and Tornadoes"NWS Weather Spotter's Field Guide (YPA-201154, June 2011)Branick, A Comprehensive Glossary of Weather Terms for Storm Spotters, NOAA Technical Memorandum NWS SR-145

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