GISP2 Oxygen Isotope Ratios

By M. Stuiver, P. Grootes. Quaternary Research, 2000

615 citations recorded by the source corpus.

Subfields: Atmospheric Science, Ecology, Oceanography

View Paper: https://www.semanticscholar.org/paper/121191096b1a6ffbbe6fac7749c3be00294a5670

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. Eli Tziperman
2. H. Gildor
3. A. Voelker
4. M. Sarnthein
5. M. Nadeau
6. J. R. Allen
7. R. Muscheler
8. M. Salter-Townshend

In Ecology

1. M. Nadeau
2. A. Voelker
3. M. Sarnthein
4. A. Timmermann
5. Andrew C. Parnell
6. John Haslett
7. P. Grootes
8. M. Blaauw

In Oceanography

1. A. Voelker
2. M. Sarnthein
3. M. Nadeau
4. J. R. Allen
5. Brian Huntley
6. A. Timmermann
7. P. Grootes

Citations in the corpus

• Coherent Resonant Millennial-Scale Climate Oscillations Triggered by Massive Meltwater Pulses (2003, background): “Recently, Timmermann and Lohmann (2000) and Monahan et al. (2002) proposed a new mechanism for the destabilization of the THC.”
• Bayesian inference for palaeoclimate with time uncertainty and stochastic volatility (2015, methodology): “We obtain informative prior distributions for the IG parameters φ1 and φ2 by fitting the NIG process to the last 14k years of a similarly irregularly-spaced ice core data set from Greenland (Stuiver, 2000).”
• Radiocarbon Levels in the Iceland Sea from 25–53 kyr and their Link to the Earth's Magnetic Field Intensity (2000, methodology): “Here we use the bidecadal data set which is based on the 20-cm resolution record (equal to an average time resolution of 12 yr during interstadials and 30 yr during stadials; Stuiver and Grootes [2000] ; data available from http://depts.washington.edu/qil/datasets/gisp2_main.html).”
• Dust cycle: An emerging core theme in Earth system science (2011, background): “The Greenland ice cores are of special significance with respect to the recognition of millennial-scale changes (Fuhrer et al., 1999; Stuiver and Grootes, 2000).”
• Tree rings and ice cores reveal C-14 calibration uncertainties during the Younger Dryas (2008, positive): “Our synchronization reveals that the two-step increase in temperature at the end of the YD is a synchronous feature in both ice-core δ O and tree-ring width”