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Mark S. Twickler

Researcher at University of New Hampshire

Publications -  47
Citations -  6063

Mark S. Twickler is an academic researcher from University of New Hampshire. The author has contributed to research in topics: Ice core & Ice sheet. The author has an hindex of 29, co-authored 47 publications receiving 5804 citations.

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A 110,000-Yr Record of Explosive Volcanism from the GISP2 (Greenland) Ice Core

TL;DR: This article used the GISP2 ice core to develop a continuous record of explosive volcanism over the past 110,000 yr. They identified ∼850 volcanic signals with sulfate concentrations greater than that associated with historical eruptions from either equatorial or mid-latitude regions that are known to have perturbed global or Northern Hemisphere climate, respectively.
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Sulfate and nitrate concentrations from a south Greenland ice core

TL;DR: An ice core in south Greenland covering the period 1869 to 1984 was analyzed for oxygen isotopes and chloride, nitrate, and sulfate concentrations and shows that the "excess" sulfate concentration has tripled and the nitrate concentration has doubled.
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The Holocene-Younger Dryas Transition Recorded at Summit, Greenland

TL;DR: In this paper, the transition between the Younger Dryas and Holocene climate periods occurred over a 40-year period and most of the transition occurred in a series of steps with durations of about 5 years.
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Greenland ice core “signal” characteristics: An expanded view of climate change

TL;DR: In this paper, the major ions contained in the Greenland Ice Sheet Project 2 (GISP 2) ice core from the present to ∼674 A.D. were analyzed to yield an environmental reconstruction for this period that includes a description of nitrogen and sulfur cycling, volcanic emissions, sea salt and terrestrial influences.
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Climate Change During the Last Deglaciation in Antarctica

TL;DR: High-resolution glaciochemical series from a central Greenland ice core and a new site in east Antarctica display similar variability, suggesting that rapid climate change events occur more frequently in Antarctica than previously demonstrated.