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H. Oerter

Researcher at Alfred Wegener Institute for Polar and Marine Research

Publications -  5
Citations -  1441

H. Oerter is an academic researcher from Alfred Wegener Institute for Polar and Marine Research. The author has contributed to research in topics: Ice sheet & European Project for Ice Coring in Antarctica. The author has an hindex of 4, co-authored 5 publications receiving 1341 citations.

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One-to-one coupling of glacial climate variability in Greenland and Antarctica.

Carlo Barbante, +88 more
- 09 Nov 2006 - 
TL;DR: In this paper, a glacial climate record derived from an ice core from Dronning Maud Land, Antarctica, which represents South Atlantic climate at a resolution comparable with the Greenland ice core records was presented.
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A Review of Antarctic Surface Snow Isotopic Composition : Observations, Atmospheric Circulation, and Isotopic Modeling

TL;DR: In this article, a database of surface Antarctic snow isotopic composition is constructed using available measurements, with an estimate of data quality and local variability, and the capacity of theoretical isotopic, regional, and general circulation atmospheric models to reproduce the observed features and assess the role of moisture advection in spatial deuterium excess fluctuations.
Journal ArticleDOI

Progress in 14C dating of ice at Utrecht

TL;DR: In this article, a special milling device has been constructed to chip the ice at -20 o C. The background of 7.0 + 2.0 percent modem carbon (pmC) for a sample of 50 pg C, including extraction and conversion, limits the 14C dating of ice with accelerator mass spectrometry (AMS) to about 20000 years.
Posted ContentDOI

Spatiotemporal variability of oxygen isotope compositions in three contrasting glacier river catchments in Greenland

TL;DR: In this paper, the authors examined three glacierized catchments in Greenland with different areas, glacier hydrology and thermal regimes, and found that during peak flow season the δ18O composition is controlled by the proportion between snowmelt and ice melt with episodic inputs of rainwater and occasional storage and release of a specific water component due to changes in the subglacial drainage system.