All You Ever Wanted to Know About Choosing a Rain Gauge
/The Ultimate Guide to Rain Gauges
Practical guide to determining Rainfall Rate and Rain Intensity Error
WMO CIMO/TECO Guide to Instruments and Methods of Observation, 2018 edition - Volume V, chapter 6 on the Measurement of precipitation.
Aerodynamics of rain gauges and error due to wind (coming soon)
Rain Gauge Types by Measuring Principle
Rain gauge measuring principle (rain gauge type) determines the general accuracy, reliability and maintenance requirements of the rain gauge. There are many different measuring principles. Bellow we list the most popular ones. If you would like others listed, please let us know in the comments bellow:
Self-emptying tipping bucket rain gauges, or TBR for short, are the most popular type of rain gauge despite having some drawbacks, many of which may be a thing of the past with the introduction of a new self-balancing tipping-bucket mechanism in the new MeteoRain line of rain gauges by BARANI DESIGN Technologies. Historically very popular designs include Pronamic, Davis Instruments and RainWise rain gauges among the many types.
Weighing rain gauges have the advantage of being able to offer very high rain resolution, good rain accumulation accuracy and short term precipitation intensity measurement at least in the laboratory. Practical experience has shown that maintaining them can be quite burdensome and wind induced pressure errors and vibration errors along with non-horizontal mounting errors and most significantly debris (leaves, insects, …) that falls into the weighing pan errors are a source of endless problems and frequent maintenance is a must. Nevertheless they remain highly popular with meteorological offices since their single biggest benefit is their consistent measurement of rain accumulation not affected by rain intensity, which has been the pitfall of tipping bucket rain gauges until the MeteoRain IoT wireless series from BARANI, which feature a built in intensity correction factor for each tip of the tipping bucket which is transparently reported to the user.
Siphoning rain gauges have the advantage precise total rain measurement for long lasting rain storms. For short rainstorms they introduce a large error due to starting error from water left over from the previous storm that is stored in the siphon and consequently also larger evaporation of stored water from the siphon and the tipping-bucket. Since siphons accumulate and then flush water into their tipping bucket counter under the siphon, the siphoning flow rate and not the true rain rate is measured, thus all information about rainfall intensity is lost. It is also important to keep the siphon clean with regular dissassembly and maintenance, making them less desirable for remote installations. Some examples include Texas Electronics rain gauges or TB4 from Kisters that combine a siphon with a tipping bucket mechanism.
Acoustic precipitation measuring principle like Vaisala WXT520, WXT530, WXT532 and WXT536 use is a rough estimate of rain fall rate based on the impact strength of raindrops hitting a metal surface. Needless to say, accumulated rain amounts are only very rough estimates based on manufacturer calibration equations. With this principle the stated 5% accuracy will be quite hard to reach outside of a laboratory and I would put it in the same category of “rain sensors” with the following RG-11. (Vaisala has quietly acknowledged this by removing the "5% “rainfall cumulative accumulation accuracy 5%*” as found on the WXT520 from the follow-on Weather Transmitter WXT530/WXT532 datasheets. Subsequently they reintroduced the following without any upper limit on the error: Field accuracy for daily accumulation: Better than 5%, weather dependent). In an independent evaluation “The Impact of Wind on Precipitation Measurements from a Compact Piezoelectric Sensor” by Enrico Chinchella, Arianna Cauteruccio, and Luca G. Lanza, published in the Journal of Hydrometeorology in February 2024 (Vol. 25, No. 2, pp. 339–352; DOI 10.1175/JHM-D-23-0180.1). It analyzed the Vaisala WXT520 with computational fluid dynamics (CFD) and reported “measured precipitation is overestimated by up to 400% under the influence of wind.“ Thus it is only a rain sensor. Its advantage is however low maintenance and simple operation.
Optical rain sensor like the RG-11 Hydreon Optical Rain Sensor is not a rain gauge and for this purpose it is the least reliable form of accumulated rain measurement with errors of up to 37% recorded by our testing. It is a rain sensor. Its advantage is however low maintenance and simple operation.
Rain gauge sizes
Rain gauges are for the most part divided into the following size classes based on rain catchment opening area. The most popular size for professional meteorological use is 200 cm² which has been informally accepted as it is the minimum acceptable size with a circular opening for reasonably accurate precipitation measurement. A circular catchment opening for a rain gauge is the standardized shape since it presents a consistent catchment area shape to windblown precipitation independent of rain and wind direction.
200 cm² catchment area rain gauges seem to be most popular worldwide among meteorological departments and have a diameter of 15.96 cm (Ø 6.28 in). Examples include BARANI MeteoRain™ 200, Lambrecht, Pronamic Professional, Stevens and others.
8 inch diameter rain gauge (Ø 20.32 cm) is standard in the USA and recommend by the NWS. It has a 50.33 in² (324.7 cm²) opening catchment area (funnel orifice). Exmaples include Texas Electronics, RainWise, Hyquest SRG and others.
400 cm² catchment area rain gauges are required by many meteorological departments and have a diameter of 22.57 cm (Ø 8.89 in). Examples include BARANI MeteoRain™ 400 Aero, Delta-OHM HD2013, NESA PL400 and others.
500 cm² catchment area rain gauges are great, but more costly, thus less common and have a diameter of 25.23 cm (Ø 9.93 in). Examples include EML SBS500, MPS System TRwS514 and others.
533 cm² catchment area rain gauges are great, but more costly, thus less common and have a diameter of 25.23 cm (Ø 9.93 in). Examples include BARANI MeteoRain™ 533 Classic with a high resolution of 0.075 mm of rainfall, very comparable to weighing rain gauges. Other non-standardized sizes and shapes exist for agricultural and amateur meteorological use such as the EML Aerodynamic 7.87”, Davis Aerocone 214 cm², Pronamic Small Rain Sensor, Acurite rain gauge collector, and Netatmo rain gauge.
1000 cm² catchment area rain gauges are the largest size and have a diameter of 35.7 cm (Ø 14.06 in). Examples include EML SBS1000 and others.
REFERENCES:
Rain gauge accuracy and WMO/NWS standards
