E-Sensor

Wind Speed Sensor Performance

The E-Sensor anemometer was evaluated against a reference-grade anemometer, Climomaster 6501 (probe 6543-21, hot-wire), as the true-value standard, covering accuracy, linearity, response, variability, and directional dependence. The measurement range is 0.0 – 5.0 m/s.

The values on this page are one example measured for unit 97B15211 in a wind tunnel. They vary somewhat with the individual unit, mounting, and air temperature. Use them as a guide for educational / indoor-environment measurement.

Accuracy & Linearity

Correlation between E-Sensor and Climomaster 6501 (parity plot)

The horizontal axis is the reference reading (Climomaster 6501); the vertical axis is the E-Sensor reading. The closer the points lie to the diagonal (1:1), the more accurate the sensor. R² = 0.998 indicates high linearity.

Speed rangeAccuracy (vs. reference)
0.5 – 2.5 m/swithin about ±5%
below 0.5 m/s (low speed)about 0.1 m/s in absolute terms
LinearityR² = 0.998 (E ≈ 0.96 × reference + 0.05)

Staircase up / down

Record of increasing the wind speed in steps (ascending) and then decreasing it (descending). The E-Sensor tracks the reference well, and the difference between the ascending and descending paths (hysteresis) is small.

Tracking during staircase up/down of wind speed

The leading spike (pulse) at the start of the graph is a transient from the wind-tunnel fan start-up as the measurement begins after warm-up; it is not a behavior of the E-Sensor.
Sampling interval: the reference (Climomaster 6501) updates every 1 s, while the E-Sensor updates about every 0.2 s (4–5 times per second) — this is why the E-Sensor trace is finer.

Response & Stability

ItemResult
Trackingfollows wind changes without lag (lag ≈ 0 vs. reference), overshoot under 1%
Hysteresis≤ 0.03 m/s (difference between up and down; negligible)
Noisecomparable to the actual airflow fluctuation (little sensor-added noise)
Zero0.004 m/s at no wind; stable (negligible drift)

Being a hot-wire type, the reading stabilizes after a warm-up of a few tens of seconds. Immediately after power-on, while still cold, it reads slightly low.

Repeated high / low

Record of repeatedly switching between high (about 1.1 m/s) and low (about 0.2 m/s) wind speeds. The E-Sensor follows each change without lag and returns to the same value on every cycle (high repeatability).

Repeated high/low wind-speed steps

Continuous change (ramp)

Record of continuously increasing and then decreasing the wind speed (ramp). The E-Sensor tracks the reference almost exactly.

Ramp tracking

Directional Dependence

Because the detector has a flat shape, the reading changes slightly with the horizontal wind direction. In the figure below, each speed's reading is normalized to its mean; the deviation from the dashed circle (= 1.0) is the directional variation.

Directionality (normalized polar plot)
ItemResult
Directional variationabout ±8% around the mean (nearly constant across speeds)
Most accurate orientationblue face facing the wind (= the orientation giving the maximum output)
Absolute errorabout 0.1 m/s at low speed; larger at higher speed

Keeping the orientation constant largely avoids the directional effect.

Method

The reference (Climomaster 6501, probe 6543-21) and the E-Sensor were measured sequentially with the same fan-drive schedule (warm-up → staircase up/down → repeated steps → holds → gentle ramp) and compared with the time bases aligned (tunnel 1, single unit). Directionality was measured at 8 azimuths in 45° steps.