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Update of the erosive rain factor in Slovakia using data from the period 1961a??2009

机译:使用1961A期间的数据更新斯洛伐克的腐蚀雨量?2009年

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An update of the rainfall erosivity factor (R-factor) estimated for 95 locations throughout the entire territory of Slovakia is presented in this paper. We analyzed rainfall time series with 1-minute resolution provided by the Slovak Hydrometeorological Institute. The data cover the period 1961a??2009. The rain gauges are located at altitudes ranging from 97 m a.s.l. up to 1322 m a.s.l. and cover the broadest possible range of geographic regions and climatic conditions in Slovakia with reliable rainfall measurements. First, rainfall episodes were isolated by applying the fundamental rule that two subsequent rains are separated by at least six hours of no rainfall. A total of 116,710 rainfall events were identified and analyzed. A rainfall event was classified as erosive if the two following criteria were satisfied: the maximum 15-minute intensity 6.25 mm (i.e. 25 mm hra??1, as originally used in the U.S.L.E. model, and/or rainfall depth was greater than 12.5 mm. The presented estimates of R-factor are based on 18,467 identified erosive rainfall events. Furthermore, the minimum length of rainfall record necessary for reliable estimates of R-factor has been estimated by spectral analysis. The Lomb-Scargle periodogram identified periodic behavior of the total kinetic rainfall energy and rainfall 15-minute intensities. We suggest that these periodicities are attributable mainly to the 11-year Sun spot cycle, the 18.6-year Luni-Solar cycle, and their higher harmonics. The spectral analysis also revealed that in order to capture the temporal variability the minimum length of time-series in calculating R-factors is 14a??15 years. We estimate that the long-term mean annual R-factor in Slovakia ranges from 34.8 MJ haa??1 cm hra??1 (at Gab???-kovo station) to 138 MJ haa??1 cm hra??1 (at Tatransk?? Javorina station). The median value of the mean annual R-factors for the whole country is 71.13 MJ haa??1 cm hra??1. To our best knowledge, the erosive rain factor has not been updated in Slovakia since the earlier work of Mi???-k in 1990. This paper is thus an update of the R-factors in Slovakia.
机译:本文介绍了在整个整个领土内估计95个地点的降雨腐蚀系数(R-Factor)的更新。我们分析了降雨时间序列,由斯洛伐克水文气象研究所提供的1分钟分辨率。数据涵盖了1961A期间的2009年。雨量仪位于海拔高达97米A.L.高达1322米A.L.并涵盖斯洛伐克的最广泛的地理区域和气候条件,具有可靠的降雨测量。首先,通过应用两个后续下雨的基本规则来分离降雨剧集,即至少六小时的没有降雨。共鉴定并分析了116,710个降雨事件。如果满足两种标准,将降雨事件被归类为侵蚀:最大15分钟强度6.25mm(即最初用于USLE模型的25 mm Hra-1,以及雨量深度大于12.5毫米。R-Faction的估计基于18,467个鉴定的腐蚀降雨事件。此外,通过光谱分析估计了R-Facts可靠估计所需的最小降雨记录的最小长度。LOMB曲线曲线周期图确定了周期性行为总动力学降雨量和降雨量为15分钟的强度。我们建议这些周期主要归属于11年的日光现货周期,18.6年伦 - 太阳循环及其更高的谐波。光谱分析也透露了为了捕获时间变异性,计算R因子的最小时间序列长度为14A ?? 15年。我们估计斯洛伐克的长期平均年度R因子从34.8 MJ Haa的范围?? 1 cm hra ?? 1(在gab ??? - kovo站)到138 mj haa ?? 1 cm hra ?? 1(在tatransk ??嘉豪站)。整个国家/地区的平均年度R因素的中位数为71.13 mj haa ?? 1 cm hra ?? 1。为了我们的最佳知识,自1990年早期的工作以来,斯洛伐克的腐烂雨因子尚未在斯洛伐克更新。因此,本文是斯洛伐克R因素的更新。

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