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Barlow, L K (1999): GISP2 Stable Isotopes (Deuterium, annual averages). PANGAEA, https://doi.org/10.1594/PANGAEA.56088, In supplement to: Barlow, L K; White, James W C; Barry, Roger G; Rogers, John; Grootes, Pieter Meiert (1993): The North Atlantic Oscillation signature in deuterium and deuterium excess signals in the Greenland Ice Sheet Project 2 ice core, 1840-1970. Geophysical Research Letters, 20(24), 2901-2904, https://doi.org/10.1029/93GL03305

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Related to:
Barlow, L K (1994): Evaluation of seasonal to decadal scale deuterium and deuterium excess signals, GISP2 ice core, Summit, Greenland, A.D. 1270-1985. PhD Thesis, University of Colorado, Boulder, Colorado, USA
Barlow, L K; Rogers, John; Serreze, Mark C; Barry, Roger G (1997): Aspects of climate variability in the North Atlantic sector: Discussion and relation to the Greenland Ice Sheet Project 2 high-resolution isotopic signal. Journal of Geophysical Research: Oceans, 102(C12), 26333-26344, https://doi.org/10.1029/96JC02401
White, D E; White, James W C; Steig, Eric J; Barlow, L K (1997): Reconstructing annual and seasonal climatic responses from volcanic events since A.D. 1270 as recorded in the deuterium signal from the Greenland Ice Sheet Project 2 ice core. Journal of Geophysical Research: Atmospheres, 102(D16), 19683-19694, https://doi.org/10.1029/97JD00774
White, James W C; Barlow, L K; Fisher, D; Grootes, Pieter Meiert; Jouzel, Jean; Johnsen, Sigfús Jóhann; Stuiver, Minze; Clausen, Henrik Brink (1997): The climate signal in the stable isotopes of snow from Summit, Greenland: Results of comparisons with modern climate observations. Journal of Geophysical Research: Oceans, 102(C12), 26425-26440, https://doi.org/10.1029/97JC00162
Project(s):
Greenland Ice Core Projects (GRIP/GISP/NGRIP)
Coverage:
Latitude: 72.970000 * Longitude: -38.800000
Date/Time Start: 1990-01-01T00:39:00 * Date/Time End: 1990-01-01T00:39:00
Minimum DEPTH, ice/snow: 2.55 m * Maximum DEPTH, ice/snow: 187.97 m
Event(s):
GISP2 * Latitude: 72.970000 * Longitude: -38.800000 * Date/Time: 1990-01-01T00:39:00 * Elevation: 3208.0 m * Recovery: 3053 m * Campaign: GISP * Basis: Sampling/drilling ice * Method/Device: Drilling/drill rig (DRILL) * Comment: GISP2 is a combination of the shallow B and the deeper D core; about 200 ka
Comment:
Year is calendar year associated with the sample, determined as described in Barlow (1994). This is effectively a winter-to-winter year, as defined by troughs in the delta deuterium data, as opposed to the summer-to-summer year defined by the official layer-counted timescale of Meese et al. (1997).
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, ice/snowDepth ice/snowmGeocode
2AGEAgeka BPGeocode
3δ DeuteriumδD‰ SMOWBarlow, L KANNUAL AVERAGES ! These data were produced in the stable isotope laboratory of at the University of Colorado. The variable Year is the calendar year associated with the sample, determined as described in Barlow (1994). This is effectively a winter-to-winter year, as defined by troughs in the delta deuterium data, as opposed to the summer-to-summer year defined by the official layer-counted timescale of Meese et al. (1997).
4AgeAgea ADBarlow, L KThese data were produced in the stable isotope laboratory of at the University of Colorado. The variable Year is the calendar year associated with the sample, determined as described in Barlow (1994). This is effectively a winter-to-winter year, as defined by troughs in the delta deuterium data, as opposed to the summer-to-summer year defined by the official layer-counted timescale of Meese et al. (1997).
Size:
1372 data points

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