Abstract
Distinct annual dust layers are preserved both in the tropical Quelccaya ice cap located in the Southern Andes of Peru as well as in the Guliya ice cap in the far Western Kunlun mountains of Tibet. The Tibetan Plateau and Bolivian-Peruvian altiplano have similar mean elevations (∼ 4000 metres) and their regional weather patterns are driven primarily by the sensible heat flux over these plateaus and latent heat release during precipitation. On average 70 to 80% of their annual snowfall arrives during their wet seasons, November to April on Quelccaya and April to August on Guliya.
This paper compares the 1500 year net accumulation (An) record from Quelccaya with the 2000 year net accumulation history from Guliya. This similarity between theses An histories is striking given that the sites are 20,000 km apart, lying on opposite sides of the Pacific Basin. During the overlapping 1500 years the major periods of drought and wetness appear contemporaneous, suggesting a teleconnection for higher-frequency climatic events such as the El Niño-Southern Oscillation (ENSO). Now, for the first time, a longer temporal perspective is available from ice core records and it suggests that lower-frequency teleconnections may exist as well.
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© 1996 Springer-Verlag Berlin Heidelberg
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Thompson, L.G. (1996). Climatic Changes for the last 2000 Years Inferred from Ice-Core Evidence in Tropical Ice Cores. In: Jones, P.D., Bradley, R.S., Jouzel, J. (eds) Climatic Variations and Forcing Mechanisms of the Last 2000 Years. NATO ASI Series, vol 41. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-61113-1_14
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DOI: https://doi.org/10.1007/978-3-642-61113-1_14
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