首页> 外文期刊>Catena: An Interdisciplinary Journal of Soil Science Hydrology-Geomorphology Focusing on Geoecology and Landscape Evolution >Spatio-temporal reconstruction of snow avalanche activity using tree rings: Pierres Jean Jeanne avalanche talus, Massif de l'Oisans, France.
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Spatio-temporal reconstruction of snow avalanche activity using tree rings: Pierres Jean Jeanne avalanche talus, Massif de l'Oisans, France.

机译:使用树木年轮重建雪崩活动的时空:法国法国Massif de l'Oisans的Pierres Jean Jeanne雪崩。

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Snow avalanches are a major threat in many parts of the Alps, where they periodically damage infrastructure, disrupt transportation corridors or even cause loss of life. Nonetheless, the spatial behavior of past avalanche activity and the analysis of areas affected during particular events remain often imprecise. It was therefore the purpose of this study to reconstruct spatio-temporal patterns of past avalanche activity on a forested avalanche talus in the French Alps (Pierres Jean Jeanne talus, Massif de l'Oisans, France). A total of 232 European larches (Larix decidua Mill.) with clear signs of snow wasting events was analyzed and growth disturbances (GD) related to avalanche activity was assessed, such as tangential rows of traumatic resin ducts, the onset of compression wood or abrupt growth suppression and release. In total, 901 GD were identified in the tree-ring samples, indicating that 20 high-magnitude avalanches occurred between AD 1919 and 1994. The mean return period of snow avalanches was ~4 years with a ~26% probability that an avalanche occurs in any particular year. Interpolated maps allowed for explicit spatial estimates of return periods throughout the talus, showing a rapid increase of return frequency from 2.5 to 50 years with increasing distance from the talus apex. The distribution of avalanche years seems to be quite homogeneous in time with a gap between 1951 and 1959 and since 1994. Snowfall from a nearby meteorological station (Saint-Christophe en Oisans; 10 km from the study site) indicated that the five most recent high-magnitude events on record occurred due to above-average snowfall anomalies in December and January associated with abnormally low air temperatures. Findings suggest that a strong snow metamorphism under high temperature gradients in January could explain the occurrence of high-magnitude snow avalanches.Digital Object Identifier http://dx.doi.org/10.1016/j.catena.2010.08.004
机译:雪崩是阿尔卑斯山许多地区的主要威胁,它们会定期破坏基础设施,破坏运输走廊,甚至造成生命损失。尽管如此,过去雪崩活动的空间行为以及对特定事件期间受影响区域的分析仍然不准确。因此,本研究的目的是在法国阿尔卑斯山(皮埃尔·让·珍妮·塔卢斯,法国Massif de l'Oisans,皮埃尔·让·珍妮·塔卢斯)上重建过去雪崩活动的时空分布。总共分析了232个欧洲雪clear(Larix decidua Mill。),这些雪lar有明显的消雪事件迹象,并评估了与雪崩活动相关的生长干扰(GD),例如切开的创口树脂导管,压缩木材的发作或突然的生长抑制和释放。总共在树轮样本中鉴定出901 GD,这表明在1919年至1994年之间发生了20次高强度雪崩。雪崩的平均返还期为〜4年,在雪崩发生的可能性约为26%。任何特定的年份。内插图可以对整个距骨的返回期进行明确的空间估计,显示随着距距骨顶点距离的增加,回返频率从2.5年迅速增加到50年。雪崩年的分布在时间上似乎相当均匀,在1951年和1959年之间以及1994年以来存在间隔。从附近气象站(圣克里斯托夫·恩·奥伊桑斯;距研究地点10公里)的降雪表明,最近五个高雪期有记录的大气压事件是由于12月和1月的降雪异常高于平均水平以及异常低的气温引起的。研究结果表明,一月高温梯度下强烈的雪变质作用可以解释高雪崩的发生。数字对象标识符http://dx.doi.org/10.1016/j.catena.2010.08.004

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