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Time:2026-01-02 10:38:18 Popularity:914
Quick answer: Automatic weather station accuracy depends on both the instruments and their exposure, installation and recording. A calibrated sensor can still report an unrepresentative value beside a hot roof, behind an obstruction or through an incorrectly scaled logger channel. Diagnose the kind of error before changing a calibration or replacing the station.

A station used for photovoltaic performance analysis does not have exactly the same exposure objective as one measuring conditions inside a crop canopy. Both can produce valid observations, but their heights and surroundings must be understood before comparing them with a regional weather report. For engineers accepting a NiuBoL automatic weather station, the first task is to distinguish a bad instrument from a measurement point that is answering a different question.
| Error type | Typical sign | Useful check |
|---|---|---|
| Instrument or calibration error | A difference persists under a controlled comparison with a suitable reference. | Inspect the sensor, verify its configuration and arrange the relevant calibration check. |
| Exposure or representativeness error | The difference changes with sunshine, wind direction, nearby activity or shading. | Inspect mounting height and surroundings; compare under more than one weather condition. |
| Acquisition or processing error | Local and remote values differ, units are implausible or events disappear from records. | Trace channel scaling, pulse counts, timestamps and aggregation through the logger and application. |
These errors can occur together. An air-temperature probe above a heated roof may have a valid calibration while its logger also applies the wrong decimal scale. Correcting one does not remove the other. Start with an annotated photograph, mounting dimensions and the channel configuration. Record when the disagreement occurs. A problem limited to sunny, low-wind afternoons points to different causes from a constant factor-of-ten error at all hours.
Air-temperature measurement requires the sensing element to follow air temperature rather than solar heating of the instrument or nearby surfaces. Keep the specified radiation shield clean and unobstructed, with airflow around it. Exhaust outlets, sun-heated walls and equipment cabinets can introduce local effects. An exposed reference thermometer placed beside a shielded sensor is not a valid test of the shielded air measurement merely because the instruments are close together.
The U.S. National Weather Service siting guidance treats temperature, precipitation and wind exposure separately. Use the requirements appropriate to the intended observation network or project. At a roadside installation, inspect the effects of paving, the mounting base and adjacent vegetation. Those surroundings may suit a local monitoring objective, but differences from open-field exposure must be considered when comparing observations. Do not apply a permanent numerical offset to correct surface heating: the effect changes with radiation, wind and the condition of the surface.

For a modular weather station, specify each measurement channel rather than applying one accuracy statement to the entire system. The following NiuBoL examples show why range, accuracy and resolution must be read separately. Select the electrical output and supply version when ordering. The availability of several output options does not mean that one delivered instrument provides them all at the same time.
| Measurement and model | Range and stated accuracy | Configuration detail |
|---|---|---|
| Wind speed, NBL-W-SS | 0-45 or 0-70 m/s; +/- (0.3 + 0.03V) m/s, where V is wind speed in m/s; resolution 0.1 m/s | Selected pulse, 4-20 mA, voltage or RS485 version; IP65. |
| Wind direction, NBL-W-DS | 0-360 degrees; +/-3 degrees | Selected 4-20 mA, voltage or RS485 version; IP65. |
| Air temperature, NBL-W-LBTH | -40 to +80 degrees C; +/-0.5 degrees C; resolution 0.1 degrees C | Combined temperature, humidity and pressure assembly. |
| Relative humidity, NBL-W-LBTH | 0-100% RH; +/-5% RH; resolution 0.1% RH | Exposure, condensation and shield condition still require inspection. |
| Air pressure, NBL-W-LBTH | 10-1200 hPa; +/-1.5 hPa; resolution 0.1 hPa | Identify station pressure separately from pressure reduced to sea level. |
| Supply and output selection | SS and DS: selected 5 V or 12-24 V DC version; LBTH: 12-24 V DC | LBTH output options are RS485 or 4-20 mA; match the ordered version to the logger. |
At V = 10 m/s, the NBL-W-SS accuracy expression gives +/-0.6 m/s. This is a calculation from the sensor specification, not a total uncertainty guarantee for an installed mast. Turbulence behind a building can introduce a larger difference without indicating that the sensor has failed. Similarly, a temperature display resolving 0.1 degrees C does not establish an accuracy of +/-0.1 degrees C.
The wind sensors' starting speed is no more than 0.5 m/s. That is not a guarantee of meaningful direction in calm conditions. A vane can remain near its previous position when the airflow is too weak to orient it. Set a calm-data treatment for the application rather than interpreting every stationary direction value as a sustained wind from that bearing.

For conventional surface wind observations, 10 m above ground is a common reference height. It is not a reason to put every other sensor at 10 m. A crop study may intentionally measure closer to the canopy; a photovoltaic project may need the wind conditions affecting its array. State that objective and the actual sensor height. Two instruments at different heights or on opposite sides of a structure are not conducting a direct accuracy comparison.
Walk the wind sensor's surroundings and identify obstructions by direction. A building can disturb one sector while another remains more exposed. Check vane alignment and mounting security before investigating calibration. If a mast has rotated, a consistent directional offset may be mechanical. Circular directions also require appropriate processing: readings near north must not be averaged as though 359 degrees and 1 degree represented opposite winds.
When comparing stations, use the same averaging period and distinguish an instantaneous sample, a mean wind and a gust. A one-minute mean should not be judged against another application's daily maximum. No change to the sensor's accuracy setting can make those different statistics equivalent. The original time series and the averaging definitions are needed to decide whether the discrepancy is in exposure, the instrument or the calculation.
Keep the rain collector level and inspect the funnel, inlet screen and drainage path. Trees and roofs can intercept rain or direct additional water into the collector; hard nearby surfaces can cause splash. Cleaning a blockage restores collection but does not verify the bucket mechanism. Use a controlled-water procedure suited to the installed rain gauge if a volume-to-count check is required, with a flow rate appropriate to the test rather than an uncontrolled pour.
Separate collection accuracy from logger counting. Injecting or observing known pulses checks acquisition but does not prove that the funnel and bucket collect rainfall correctly. As an illustrative configuration only, 50 accepted tips at 0.2 mm/tip should produce 10 mm. This is not a specification for every NiuBoL rain gauge. Confirm the installed gauge's increment and ensure that counter resets, restart behavior and daily totals agree with that configuration.
Where a solar-radiation channel is fitted, inspect the sensing surface, its intended measurement plane and any time-dependent shadows. For horizontal irradiance, check leveling; for an array-plane measurement, record tilt and azimuth instead of assuming that horizontal is always correct. Dirt or a morning mast shadow can distort the irradiance record while the electrical output remains stable. A weather-station inspection should therefore follow the actual channels, not a single generic clearance rule.

For an RS485 / Modbus RTU installation, match addresses and serial settings, then confirm register data types and scales. Check a plausible channel value locally and remotely at matching acquisition times. A communicating instrument is not proof of correct engineering units. Pressure is a useful example: 1 kPa equals 10 hPa, and a regional sea-level pressure report is not automatically comparable with station pressure at an elevated site.
Record sampling and reporting intervals separately. A logger may acquire frequently but send less frequent summaries. If a storm occurs during a communication outage, determine whether records were sampled and stored locally before deciding that the missing remote rainfall represents no rain. Missing observations must not silently become zero. After reconnection, verify record order and any duplicate handling in the receiving application.
A dashboard is the end of this chain, not a calibration reference. Inspect unit labels, decimal places, time zone and the definition of each displayed statistic. Retain the acquisition timestamp where reception can be delayed. Before changing a sensor that "looks wrong" on a dashboard, compare the underlying register and stored record. This avoids replacing an instrument for an application conversion error.

Begin with the condition of the installation: shield cleanliness, freely moving wind components, collector level, cable support, enclosure seals and signs of water or insect entry. IP65 for the wind speed and direction sensors does not establish an identical rating for the data logger, connectors or complete cabinet. Nor does an ingress rating establish that rotating parts remain free in ice or that a rain gauge measures frozen precipitation without suitable equipment.
Next, compare selected channels with suitable references under equivalent exposure. Note the reference's calibration status and allow the instruments to stabilize. Repeat a temperature comparison across relevant conditions if solar heating is suspected; a single overcast reading may miss the problem. Record before-and-after results for cleaning or realignment. Avoid adjusting multiple settings together, which makes it difficult to identify which action corrected the fault.
Set the next inspection from what the visit reveals. Frequent insects in the rain inlet, deposits on a radiation surface or bearing resistance justify different work and intervals. A fixed calendar replacement of every sensor is not a substitute for these observations. If calibration is required, remove or isolate the affected instrument safely and retain a record of any gap in the weather series.
When asking NiuBoL to review an accuracy problem or configure an automatic weather station, include the sensor models and output versions, photographs of the surroundings, mounting heights and a short paired dataset with units and timestamps. State whether the observation is for crop conditions, photovoltaic analysis or a wider meteorological record. That evidence helps distinguish a different measurement objective from a faulty component and keeps the proposed work relevant.

No. Calibration assesses the instrument under defined conditions. It does not remove heating from a nearby roof, wind obstruction, collector blockage or an incorrect application conversion. Check those causes separately before accepting the installed record.
Not as a direct sensor accuracy test. Height, terrain and obstructions affect the wind. Record the actual exposure and intended use; any adjustment to a reference height needs an appropriate method and assumptions, not a fixed universal correction.
Investigate shield ventilation, nearby heated surfaces and the reference instrument's exposure. A persistent sensor offset is another possibility, but a weather-dependent difference should not be hidden by applying a constant calibration offset first.
The logger may use the wrong amount per tip, reset at an unintended time or lose counts during restart. Compare the cumulative counter with the daily calculation and timestamp convention. Separately inspect and test the collector; correct counting does not validate water collection.
Not on its own. Compare distance, elevation, exposure, sampling interval and the reported statistic. A local array or canopy measurement can legitimately differ from a regional station. Use an appropriate colocated comparison when checking the instrument itself.
No. The NBL-W-SS and NBL-W-DS wind sensors are specified here as IP65. The logger, enclosure and connections need their own ratings and installation checks. Select the complete outdoor arrangement for rain, condensation, temperature and site conditions.
Include channel identity and scaling, siting and alignment checks, relevant reference comparisons, rainfall-count verification and recorded timestamps. Add communication-loss and recovery checks when remote records are required. Define tolerances around the actual instruments and method rather than an unsupported accuracy figure for every channel.
Replacement becomes appropriate when inspection, configuration checks and a suitable reference test identify a failed or unsuitable instrument. First eliminate incorrect exposure and acquisition settings. If the site objective exceeds the sensor's range or accuracy, select a different specification rather than repeatedly recalibrating the same instrument.
Automatic weather station accuracy is an installed measurement problem. Use the individual sensor specifications, expose each instrument appropriately and verify the recorded engineering value. A useful acceptance or maintenance visit should identify which of those stages causes the error, so that the corrective work changes the measurement rather than merely changing its display.
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