2020
DOI: 10.1016/j.jhydrol.2020.125580
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Comparing precision lysimeter rainfall measurements against rain gauges in a coastal dune belt, Spain

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Cited by 11 publications
(13 citation statements)
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“…Thus, an increased underestimation of the precipitation intensity can be recognized with increasing reference values. Kohfahl and Saaltink (2020) also found that TBs located at the same site differed in the amount of precipitation measured during six rain events compared to a high-precision weighable lysimeter for bare soil conditions. The authors assumed that the TB, which showed significant errors with minor amounts of rainfall, was affected by an individual technical problem.…”
Section: Evaluation Of Gauge Types For the Comparison Of Precipitatio...mentioning
confidence: 81%
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“…Thus, an increased underestimation of the precipitation intensity can be recognized with increasing reference values. Kohfahl and Saaltink (2020) also found that TBs located at the same site differed in the amount of precipitation measured during six rain events compared to a high-precision weighable lysimeter for bare soil conditions. The authors assumed that the TB, which showed significant errors with minor amounts of rainfall, was affected by an individual technical problem.…”
Section: Evaluation Of Gauge Types For the Comparison Of Precipitatio...mentioning
confidence: 81%
“…The increased lysimeter data quality (i.e. precision and temporal resolution) has already led to a number of studies that 80 compared lysimeter measurements with those of other precipitation gauges (Gebler et al, 2015;Haselow et al, 2019;Hoffmann et al, 2016;Kohfahl and Saaltink, 2020;Schrader et al, 2013). Gebler et al (2015) found a 16 % underestimation https://doi.org/10.5194/hess-2022-370 Preprint.…”
Section: Introduction 40mentioning
confidence: 99%
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“…These lysimeters are able to observe non-rainfall precipitation, such as dew and water vapour adsorption (Zhang et al, 2019). A case in a dune belt in southern Spain (average annual precipitation was 550 mm) measured annual precipitation using a lysimeter, which exceeded the tipping bucket pluviometer by 13% due to water vapour adsorption (Kohfahl et al, 2019;Kohfahl & Saaltink, 2020). The structure of rain gauges easily makes summertime raindrops splash or evaporate and causes frost and snow to be lost before melting measurements in winter (Sevruk, 1996;Sevruk et al, 1989).…”
Section: Introductionmentioning
confidence: 99%
“…Several effective calibration methods have been proposed over the years: Calder and Kidd [30] suggested a method based on rain gauge parameters (bucket volume and the time between successive bucket tips); Niemczynowicz [29] proposed the equation I = aNb, where I is the measured rain gauge rate, N is the tipping rate, and a and b are fitting parameters. Marsalek [18] determined an analytical expression comparing the nominal rainfall depth increment per tip and the time required for filling the bucket; Humphrey et al [17] described an automated system performing dynamic calibration; Costello and Williams [31] proposed a method considering a laboratory-determined calibration curve; Luyckx and Berlamont [32] developed an analytical calibration taking into account the relationship between the rain gauge resolution and the slope of its regression line; Shedekar et al [33] developed a linear regression and two dynamic calibration techniques; Shimizu et al [34] developed a generalized correction equation for various TBRs; Sypka [35] developed an algorithm to implement a real-time dynamic volumetric correction based on a "tip interval" and nominal tip volume; Kohfahl and Saaltink [36] compared TBR measurements with a precision lysimeter and a weighing rain gauge. Alternatively, other authors have proposed different calibration methods [14,22,[37][38][39][40][41][42][43][44][45][46].…”
Section: Introductionmentioning
confidence: 99%