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J. F. Bolzan

Researcher at Ohio State University

Publications -  30
Citations -  4751

J. F. Bolzan is an academic researcher from Ohio State University. The author has contributed to research in topics: Ice core & Ice sheet. The author has an hindex of 16, co-authored 30 publications receiving 4514 citations. Previous affiliations of J. F. Bolzan include Energy Research and Development Administration.

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Tropical Climate Instability: The Last Glacial Cycle from a Qinghai-Tibetan Ice Core

TL;DR: An ice core record from the Guliya ice cap on the Qinghai-Tibetan Plateau provides evidence of regional climatic conditions over the last glacial cycle as discussed by the authors.
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Late glacial stage and holocene tropical ice core records from huascaran, peru.

TL;DR: Two ice cores from the col of Huascar�n in the north-central Andes of Peru contain a paleoclimatic history extending well into the Wisconsinan (W�rm) Glacial Stage and include evidence of the Younger Dryas cool phase, implying that a strong warming has dominated the last two centuries.
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A 25,000-Year Tropical Climate History from Bolivian Ice Cores

TL;DR: The abrupt onset and termination of a Younger Dryas-type event suggest atmospheric processes as the probable drivers of regional accumulation during the LGS, during deglaciation, and over the past 3000 years, which is concurrent with higher water levels in regional paleolakes.
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The Greenland Ice Sheet Project 2 depth-age scale : Methods and results

TL;DR: The Greenland Ice Sheet Project 2 (GISP2) depth-age scale is presented based on a multiparameter continuous count approach to a depth of 2800 m, using a systematic combination of parameters that have never been used to this extent before as mentioned in this paper.
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Holocene--late pleistocene climatic ice core records from qinghai-tibetan plateau.

TL;DR: Three ice cores to bedrock from the Dunde ice cap on the north-central Qinghai-Tibetan Plateau of China provide a detailed record of Holocene and Wisconsin-W�rm late glacial stage (LGS) climate changes in the subtropics.