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Dating of recent avalanche events in the Eastern High Sudetes, Czech Republic

机译:捷克共和国东部高苏德特人近期雪崩事件的日期

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摘要

This article deals with recent avalanche events dated by the dendrogeomorphic method and their verification. The research was focused on two active mid-mountain avalanche sites - the Snezna kotlina Hollow and the Morava Hollow in the Eastern High Sudetes. A total of 96 trees were analysed and eight highly probable avalanches were identified since 1924 and 1935, respectively. The avalanche events were verified using historical aerial photographs, meteorological data and different historical sources (i.e. local newspapers, historic photographs, etc.). Avalanches are more frequent in the Snezna kotlina Hollow (avalanche years: 1984, 1993, 2004, 2005, 2007, 2008) than in the Morava Hollow (avalanche years: 1942, 1999). Most avalanche events correspond with heavy snowfall events or high temperature events during February and March. There are significant differences in the frequency of avalanches between the two study sites that are reflected in the morphology of the avalanche paths under study. The more active avalanche path has a more ragged surface and includes a typical avalanche gully. The results of the verification support the use of the dendrogeomorphic method because the potential avalanche events were clearly confirmed. (c) 2017 Elsevier Ltd and INQUA. All rights reserved.
机译:本文介绍了最近通过树状地貌方法发生的雪崩事件及其验证。该研究的重点是两个活跃的中山雪崩站点-东部高苏台特山脉的Snezna kotlina凹陷和Morava凹陷。自1924年和1935年以来,总共分析了96棵树,并确定了8个极有可能的雪崩。雪崩事件是使用历史航拍照片,气象数据和不同的历史资料(例如当地报纸,历史照片等)进行验证的。 Snezna kotlina Hollow(雪崩年份:1984、1993、2004、2005、2007、2008)中的雪崩发生率高于Morava Hollow(雪崩年份:1942、1999)。大多数雪崩事件与2月和3月的大雪事件或高温事件相对应。两个研究地点之间的雪崩频率存在显着差异,这反映在所研究的雪崩路径的形态上。较活跃的雪崩路径的表面更加参差不齐,并且包含典型的雪崩沟。验证结果支持使用树状地貌方法,因为已清楚地确认了潜在的雪崩事件。 (c)2017年爱思唯尔有限公司和INQUA。版权所有。

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