Ryan S. Padrón, J. Feyen, M. Cordova, Patricio Crespo, Rolando Célleri
{"title":"Comparación entre Pluviómetros Cuantifica Deficiencias en el Monitoreo de la Precipitación","authors":"Ryan S. Padrón, J. Feyen, M. Cordova, Patricio Crespo, Rolando Célleri","doi":"10.17163/LGR.N31.2020.0","DOIUrl":null,"url":null,"abstract":"Efforts to correct precipitation measurements have been ongoing for decades, but are scarce for tropical highlands. Four tipping-bucket (TB) rain gauges with different resolution that are commonly used in the Andean mountain region were compared-one DAVIS-RC-II, one HOBO-RG3-M, and two TE525MM TB gauges (with and without an Alter-Type wind screen). The relative performance of these rain gauges, installed side-by-side in the Zhurucay Ecohydrological Observatory, south Ecuador, at 3780 m a.s.l., was assessed using the TB with the highest resolution (0.1 mm) as reference, i.e. the TE525MM. The effect of rain intensity and wind conditions on gauge performance was estimated as well. Using 2 years of data, results reveal that (i) the precipitation amount for the reference TB is on average 5.6 to 7.2% higher than the rain gauges having a resolution of 0.2 mm and 0.254 mm respectively; (ii) relative underestimation of precipitation from the gauges with coarser resolution is higher during low-intensity rainfall mounting to a maximum deviation of 11% was observed for rain intensities ≤1 mm h−1; (iii) precipitation intensities of 2 mm h−1 or less that occur 75% of the time cannot be determined accurately for timescales shorter than 30 minutes because of the gauges’ resolution, e.g. the absolute bias is >10%; and (iv) wind has a similar effect on all sensors. This analysis contributes to increase the accuracy and homogeneity of precipitation measurements throughout the Andean highlands, by quantifying the key role of rain-gauge resolution.","PeriodicalId":41848,"journal":{"name":"Granja-Revista de Ciencias de la Vida","volume":"31 1","pages":"7-20"},"PeriodicalIF":0.6000,"publicationDate":"2020-03-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Granja-Revista de Ciencias de la Vida","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.17163/LGR.N31.2020.0","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"ENVIRONMENTAL SCIENCES","Score":null,"Total":0}
引用次数: 1
Abstract
Efforts to correct precipitation measurements have been ongoing for decades, but are scarce for tropical highlands. Four tipping-bucket (TB) rain gauges with different resolution that are commonly used in the Andean mountain region were compared-one DAVIS-RC-II, one HOBO-RG3-M, and two TE525MM TB gauges (with and without an Alter-Type wind screen). The relative performance of these rain gauges, installed side-by-side in the Zhurucay Ecohydrological Observatory, south Ecuador, at 3780 m a.s.l., was assessed using the TB with the highest resolution (0.1 mm) as reference, i.e. the TE525MM. The effect of rain intensity and wind conditions on gauge performance was estimated as well. Using 2 years of data, results reveal that (i) the precipitation amount for the reference TB is on average 5.6 to 7.2% higher than the rain gauges having a resolution of 0.2 mm and 0.254 mm respectively; (ii) relative underestimation of precipitation from the gauges with coarser resolution is higher during low-intensity rainfall mounting to a maximum deviation of 11% was observed for rain intensities ≤1 mm h−1; (iii) precipitation intensities of 2 mm h−1 or less that occur 75% of the time cannot be determined accurately for timescales shorter than 30 minutes because of the gauges’ resolution, e.g. the absolute bias is >10%; and (iv) wind has a similar effect on all sensors. This analysis contributes to increase the accuracy and homogeneity of precipitation measurements throughout the Andean highlands, by quantifying the key role of rain-gauge resolution.
几十年来,校正降水量的工作一直在进行,但对热带高地来说却很少。比较了安第斯山区常用的四种不同分辨率的翻斗式(TB)雨量计——一种是DAVIS-RC-II,一种是HOBO-RG3-M,两种是TE525MM TB雨量计(带和不带Alter型挡风屏)。这些并排安装在厄瓜多尔南部朱鲁凯生态水文观测站(海拔3780米)的雨量计的相对性能是使用最高分辨率(0.1毫米)的TB作为参考进行评估的,即TE525MM。还估算了降雨强度和风力条件对仪表性能的影响。使用2年的数据,结果表明:(i)参考TB的降水量平均比分辨率分别为0.2毫米和0.254毫米的雨量计高5.6至7.2%;(ii)在低强度降雨期间,分辨率较低的测量仪对降水量的相对低估较高,当降雨强度≤1 mm h−1时,观测到最大偏差为11%;(iii)由于测量仪的分辨率,无法在短于30分钟的时间尺度上准确确定75%时间内出现的2 mm h−1或以下的降水强度,例如绝对偏差>10%;以及(iv)风对所有传感器具有相似的影响。该分析通过量化雨量计分辨率的关键作用,有助于提高整个安第斯高地降水测量的准确性和均匀性。