用树木年轮重建罗马尼亚南喀尔巴阡山脉par雪灾历史

Q4 Earth and Planetary Sciences
C. Todea, O. Pop, D. Germain
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引用次数: 7

摘要

雪崩是帕朗山脉(罗马尼亚南喀尔巴阡山脉)的一种常见现象,扰乱了旅游活动和相关基础设施,破坏了森林,并造成人员死亡。其过去的历史是评估危险区域时需要收集的重要信息。通常,在罗马尼亚,发生在森林地区的雪崩活动既没有被监测,也没有被历史档案记录下来。在这些地区,树木年轮等环境档案可能会提供有关过去雪崩活动的有用信息。本研究的目的是在Cârja峰(海拔2405米)下方的一条小路上用树木年轮重建雪崩历史,该地区过去的雪崩活动仍然被低估。从这个意义上说,57挪威云杉(Picea abies(L.)Karst.)对表现出明显受雪崩干扰迹象的树木进行了采样,并在其年轮内识别出与雪崩对树木产生的机械影响相关的生长异常,并用于重建过去的事件。重建的年表涵盖1994年至2018年,显示至少发生了11起重大事件,平均重现期为2.1年。树木年轮记录提供了研究区域内最一致的雪崩事件年表。尽管时间上的年表延伸有限,但通过树状年表重建可以更好地了解雪崩历史,这仍然是在这个雪崩多发地区实施和发展基础设施之前需要考虑的有用和相关信息。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Snow–avalanche history reconstructed with tree rings in Parâng Mountains (Southern Carpathians, Romania)
Snow avalanches are a common phenomenon in Parâng Mountains (Southern Carpathians, Romania) perturbing tourism activities and associated infrastructures, damaging forests, and causing fatalities. Its past history is an es­sential information to gather while assessing the hazard zonation areas. Usually, in Romania snow–avalanche activ­ity occurring in forested areas are neither monitored, nor recorded by historical archives. In these areas, environ­mental archives such as tree rings may provide useful information about the past avalanche activity. The purpose of the present study is to reconstruct snow–avalanche history with tree rings along a path located below Cârja Peak (2405 m a.s.l.), an area where past snow–avalanche activity still remains underestimated. In this sense, 57 Norway spruce (Picea abies (L.) Karst.) trees showing clear signs of disturbance by snow avalanches were sampled and the growth anomalies associated with the mechanical impact produced by snow avalanches on trees were identified within their rings and served to reconstruct past events. The reconstructed chronology covers the period 1994–2018 showing the occurrence of a minimum of 11 major events, with an average return period of 2.1 years. Tree–ring records provided the most consistent avalanche event chronology in the study area. Although the lim­ited extension of the chronology back in time, a better understanding of snow–avalanche history which may be gained through dendro­chronological reconstructions represent nonetheless useful and pertinent information to consider before the imple­mentation and development of infrastructure in this mountain avalanche–prone area.
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来源期刊
Revista de Geomorfologie
Revista de Geomorfologie Earth and Planetary Sciences-Computers in Earth Sciences
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1.20
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