Historical records of Cipreses glacier (34°S): combining documentary-inferred 'Little Ice Age' evidence from Southern and Central Chile

被引:15
作者
Araneda, Alberto [1 ,2 ]
Torrejon, Fernando [1 ,2 ]
Aguayo, Mauricio [3 ]
Alvial, Ingrid [4 ]
Mendoza, Carlos [3 ]
Urrutia, Roberto [1 ,2 ]
机构
[1] Univ Concepcion, GEP, Aquat Syst Res Unit, Environm Sci Ctr EULA Chile, Concepcion, Chile
[2] Patagonian Ecosyst Res Ctr CIEP, Concepcion, Chile
[3] Univ Concepcion, Environm Sci Ctr EULA Chile, Land & Urban Planning Res Unit, Concepcion, Chile
[4] Univ Chile, Fac Ciencias, Santiago, Chile
关键词
Historical records; glaciers; 'Little Ice Age' (LIA); Central and Southern Chile; combining information; NORTH PATAGONIAN ICEFIELD; NEW-ZEALAND; TREE-RING; CLIMATIC FLUCTUATIONS; RAINFALL VARIABILITY; LAST MILLENNIUM; WESTERLIES; MODEL; CHRONOLOGIES; LICHENOMETRY;
D O I
10.1177/0959683609345079
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The historical behaviour of Cipreses glacier from the nineteenth through the early twentieth century is described based on written records, cartography, iconography and photographs. These data allow us to infer that the last maximum advance of Cipreses glacier attributable to the 'Little Ice Age' occurred around AD 1842. The first historical retreat was recorded in 1858 and, since then, the glacier has shown a clear retreating trend with no new advances. All this information was compared with the historical data gathered for San Rafael glacier, which shows the occurrence of a cold period contemporary with the European LIA. Whereas Cipreses glacier was retreating by 1858, San Rafael glacier was advancing, reaching its last maximum between 1857 and 1875. The dates for the advances and retreats reveal a time-lag of approximately 30 years in the responses of these glaciers. The comparison of timing in glacier advances suggests that this time-lag is due to changes in precipitation and temperature associated mainly with fluctuations of the Westerlies.
引用
收藏
页码:1173 / 1183
页数:11
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