Deuterium analysis of ice core GISP2 ...

The Greenland Ice Sheet Project 2 (GISP2) core can enhance our understanding of the relationship between parameters measured in the ice in central Greenland and variability in the ocean, atmosphere, and cryosphere of the North Atlantic Ocean and adjacent land masses. Seasonal (summer, winter) to ann...

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Bibliographic Details
Main Authors: Barlow, L K, White, James W C, Barry, Roger G, Rogers, John, Grootes, Pieter Meiert
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 1993
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.716876
https://doi.pangaea.de/10.1594/PANGAEA.716876
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Summary:The Greenland Ice Sheet Project 2 (GISP2) core can enhance our understanding of the relationship between parameters measured in the ice in central Greenland and variability in the ocean, atmosphere, and cryosphere of the North Atlantic Ocean and adjacent land masses. Seasonal (summer, winter) to annual responses of dD and deuterium excess isotopic signals in the GISP2 core to the seesaw in winter temperatures between West Greenland and northern Europe from A.D. 1840 to 1970 are investigated. This seesaw represents extreme modes of the North Atlantic Oscillation, which also influences sea surface temperatures (SSTs), atmospheric pressures, geostrophic wind strength, and sea ice extents beyond the winter season. Temperature excursions inferred from the dD record during seesaw/extreme NAO mode years move in the same direction as the West Greenland side of the seesaw. Symmetry with the West Greenland side of the seesaw suggests a possible mechanism for damping in the ice core record of the lowest decadal ... : 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 ...