MEDIAN LATITUDE: 36.295000 * MEDIAN LONGITUDE: -19.230000 * SOUTH-BOUND LATITUDE: 0.000000 * WEST-BOUND LONGITUDE: -38.460000 * NORTH-BOUND LATITUDE: 72.590000 * EAST-BOUND LONGITUDE: 0.000000 * DATE/TIME START: 1990-01-01T00:39:00 * DATE/TIME END: 1990-01-01T00:39:00 * MINIMUM DEPTH, ice/snow: 0.99 m * MAXIMUM DEPTH, ice/snow: 1867.00 m

27/07/1999

text/tab-separated-values, 34960 data points

https://doi.pangaea.de/10.1594/PANGAEA.55534

doi:10.1594/PANGAEA.55534

en

PANGAEA

Alley, Richard B; Anandakrishnan, Sridhar (1995): Variations in melt-layer frequency in the GISP2 ice core: implications for Holocene summer temperatures in central Greenland. Annals of Glaciology, 21, 64-70

Alley, Richard B; Shuman, C A; Meese, D A; Gow, AJ; Taylor, K C; Cuffey, K M; Fitzpatrick, JJ; Grootes, Pieter Meiert; Zielinski, G A; Ram, M; Spinelli, Glenn; Elder, Bruce C (1997): Visual-stratigraphic dating of the GISP2 ice core: Basis, reproducibility, and application. Journal of Geophysical Research-Oceans, 102(C12), 26367-26382, doi:10.1029/96JC03837

GRIP/GISP (1997): The Greenland Summit Ice Cores CD-ROM GISP2/GRIP. National Snow and Ice Data Center, University of Colorado at Boulder, and World Data Center for Paleoclimatology, National Geophysical Data Center, Boulder Colorado, CD-ROM, http://store.pangaea.de/Projects/GRIP-GISP/grip-gisp.iso

Spinelli, Glenn (1996): A statistical analysis of ice-accumulation level and variability in the GISP2 ice core and a reexamination of the age of the termination of the Younger Dryas cooling episode. Earth System Science Center Technical Report University of New, 96-001

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