小冰河期莫雷诺冰川边缘的进展,嗨罗Patagónico苏尔,南美洲

IF 1 Q4 GEOGRAPHY, PHYSICAL Bulletin of glaciological research Pub Date : 1900-01-01 DOI:10.5331/BGR.30.1
M. Aniya, P. Skvarca
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引用次数: 8

摘要

莫雷诺冰川Perito Moreno面积为258平方公里,位于南巴塔哥尼亚冰原的东侧,约50°29′s和73°04′w。目前,它止于阿根廷湖,从而将该湖分为北部的特帕诺斯运河和南部的布拉索里科。在20世纪,冰川不断地前进和后退;然而,自20世纪20年代以来,它可以被认为是相当稳定的。根据22个木材样品和1个有机样品的14C测年,我们推断莫雷诺冰川区发生了两次小冰期(LIA)进展,一次是在公元1650年左右,另一次是在公元1820- 1850年左右。这两个日期非常符合HPS的LIA的一般框架。
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Little Ice Age advances of Glaciar Perito Moreno, Hielo Patagónico Sur, South America
Glaciar Perito Moreno, with an area of 258km², is located on the eastern side of the Hielo Patagonico Sur (Southern Patagonia Icefield) at about 50°29′S and 73°04′W. Currently, it terminates in Lago Argentino, thereby dividing the lake into Canal de los Tmpanos to the north and Brazo Rico to the south. The glacier has repeatedly made small advances and retreats in the 20th century; however, it can be regarded as rather stable since the 1920. Based on 14C dating of 22 wood and one organic samples, we inferred that Glaciar Perito Moreno made two Little Ice Age (LIA) advances, one at ca. AD 1650 and the other about AD 1820-50. These two dates fit very well into the general framework of the LIA of the HPS.
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来源期刊
Bulletin of glaciological research
Bulletin of glaciological research GEOGRAPHY, PHYSICAL-
CiteScore
2.20
自引率
20.00%
发文量
1
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