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Ice cores record millennia of ancient snowfalls, which gradually turned to crystalline glacier ice.
Schneider, D. P. & Steig, E. J. Ice cores record significant 1940s Antarctic warmth related to tropical climate variability.
Pollen stratigraphies and chronologies of two cores record the vegetational development of the area from the Late Glacial treeless landscape to the forest and steppe of today.
Nanocrystalline CoFe2O4 with such properties have potential applications in high frequency devices, memory cores, recording media, and in biomedical field [6].
Greenland ice cores record a pulse of starkly reduced levels of organic carbon sequestration.
The ice cores record large amounts of atmospheric dust during this seven-year period, not all of it originating on Earth.
This was the highest monthly average in recorded history, and in fact according to ice core records it is the highest value in at least 800,000 years.
Sowers, T., Alley, R. B. & Jubenville, J. Ice core records of atmospheric N2O covering the last 106,000 years.
One approach is to obtain spatial reconstructions of climate using deep ice core records.
Thompson, L. G. et al. Tropical ice core records: Evidence for asynchronous glaciation on Milankovitch timescales.
Thompson, L. G. et al. Late Glacial stage and Holocene tropical ice core records from Huascaran, Peru.
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