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<br />...,. <br />,- .. ., <br />, ~""", l.:..... .....".,_., ,..... / " . ..,.' . ,-,' <br />~'. .,~a~'l:.b'.-i.t~!"';').fl~-..,~.,~,,.I,,,~'l <br /> <br />, :,,~",,",; ,.."._A,"_~,~ .,_",' ..,', . <br /> <br />PRECIPITATION GAUGE SITES <br /> <br />685 <br /> <br />For the assessment of a sites where direct measurements are missing or are no longer possible to obtain, <br />a classification of GSE was suggested by Sevruk and Zahlavova (1992). It consists of four classes, 1-4, and <br />three interim classes 1'5,2,5 and 3,5. The classes are characterized by (X values, as shown in Table I: normal <br />scale. In Figure 2, the four classes are presented as a series of drawings, to enable a visual appreciation of <br />how a particular GSE class should look. Consequently, (X can be used as a measure of GSE classes and <br />VIce versa. <br />The real problem is that there are no established classifications of GSE and they are not made routinely <br />by meteorological services. Therefore, assessment of the GSE has to be made solely by the interested party. <br />The present paper suggests a method of assessment of GSE classes from the station history records and <br />compares the results with direct measurements in the field in order to assess the accuracy of GSE class <br />estimates. In addition, applications of the method are presented. These applications concern the problem <br />of detection of inhomogeneities in precipitation time-series due to changes of GSE during the period of <br />observation, and the assessment and mapping of precipitation corrections for the wind-induced losses. <br /> <br />METHODS <br /> <br />The assessment of GSE classes is based on photographs, sketches, and written reports of gauge sites, as <br />found in the archives of national meteorological services. The assessment was carried out by three people, <br />separately: an inexperienced student, a partly experienced, young assistant, and an experienced, older <br />assistant, two of them geographers and one a civil engineer trained in hydrology. All three received a brief <br />introduction to the problem. The student started work immediately, without any more advice or supervision. <br />In contrast, both assistants were carefully advised and trained on examples through the first day and <br />consulted during the trial. The results for all three people have been compared with GSE classes as estimated <br />from the measured values of (X for the same gauge sites and the same time period. The number of gauge <br />sites included in the analysis was different for each person. This was partly due to the fact that the student <br />was advised to work very quickly for a period no more than 2 days. In that short time he checked a lO-year <br />period of 50 sites for GSE. In the case of the two assistants only the estimates of GSE classes were considered <br />in the analysis, which were made after 2 weeks work for the younger assistant and 2 months work for the <br />older assistant In total 40 gauge sites were analysed by the two assistants. The aim of using different <br />approaches was to see if there is some dependency of error in the estimate of GSE classes on the degree <br />of experience of a particular person. It is interesting to note that the normal scale as suggested in Table I <br />