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Tyler R. Jones

Researcher at Institute of Arctic and Alpine Research

Publications -  34
Citations -  1874

Tyler R. Jones is an academic researcher from Institute of Arctic and Alpine Research. The author has contributed to research in topics: Ice core & Ice sheet. The author has an hindex of 11, co-authored 32 publications receiving 1544 citations. Previous affiliations of Tyler R. Jones include University of Colorado Boulder.

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Eemian interglacial reconstructed from a Greenland folded ice core

Dorthe Dahl-Jensen, +132 more
- 24 Jan 2013 - 
TL;DR: In this paper, the North Greenland Eemian Ice Drilling (NEEM) ice core was extracted from folded Greenland ice using globally homogeneous parameters known from dated Greenland and Antarctic ice-core records.

Eemian interglacial reconstructed from a Greenland folded ice core (SCI)

Dorthe Dahl-Jensen, +133 more
TL;DR: The new North Greenland Eemian Ice Drilling (‘NEEM’) ice core is presented and shows only a modest ice-sheet response to the strong warming in the early Eemians, which was probably driven by the decreasing summer insolation.
Journal ArticleDOI

Precise interpolar phasing of abrupt climate change during the last ice age

Christo Buizert, +82 more
- 30 Apr 2015 - 
TL;DR: A north-to-south directionality of the abrupt climatic signal is demonstrated, which is propagated to the Southern Hemisphere high latitudes by oceanic rather than atmospheric processes, which confirms a central role for ocean circulation in the bipolar seesaw.
Journal ArticleDOI

Global atmospheric teleconnections during Dansgaard–Oeschger events

TL;DR: In this paper, the authors used a high-resolution deuterium-excess record from West Antarctica to show that the latitude of the mean moisture source for Antarctic precipitation changed in phase with abrupt shifts in Northern Hemisphere climate, and significantly before Antarctic temperature change.
Journal ArticleDOI

Southern Hemisphere climate variability forced by Northern Hemisphere ice-sheet topography

TL;DR: The authors used a water isotope record from West Antarctica to demonstrate that interannual to decadal climate variability at high southern latitudes was almost twice as large at the Last Glacial Maximum as during the ensuing Holocene epoch (the past 11,700 years).