Henrik B Clausen

Biographic Data

ID5601361
NAMEHenrik B Clausen
GIVEN NAMESHenrik B
FAMILY NAMEClausen
SIGNATURECLAUSEN H B
AFFILIATIONSUniversity of Copenhagen
VERIFIEDNo
TOTAL WORKS7
TOTAL CITATIONS5
AUTHOR COUNT7
EDITOR COUNT0
FIRST PUBLICATION YEAR1986
LATEST PUBLICATION YEAR2014
H-INDEX1

  • A stratigraphic framework for abrupt climatic changes during the Last Glacial period based on three synchronized Greenland ice-core records

    Open AccessSune O Rasmussen, Matthias Bigler et al.ARTICLEQuaternary Science Reviews2014

    Due to their outstanding resolution and well-constrained chronologies, Greenland ice-core records provide a master record of past climatic changes throughout the Last Interglacial–Glacial cycle in the North Atlantic region. As part of the INTIMATE (INTegration of Ice-core, MArine and TErrestrial records) project, protocols have been proposed to ensure consistent and robust correlation between different records of past climate. A key element of th…

  • High-Resolution Greenland Ice Core Data Show Abrupt Climate Change Happens in Few Years

    Open AccessJørgen Peder Steffensen, K K Andersen et al.ARTICLEScience2008

    The last two abrupt warmings at the onset of our present warm interglacial period, interrupted by the Younger Dryas cooling event, were investigated at high temporal resolution from the North Greenland Ice Core Project ice core. The deuterium excess, a proxy of Greenland precipitation moisture source, switched mode within 1 to 3 years over these transitions and initiated a more gradual change (over 50 years) of the Greenland air temperature, as r…

  • The Greenland Ice Core Chronology 2005, 15–42ka. Part 2

    Open AccessAndreas Svensson, Anders Svensson et al.ARTICLEQuaternary Science Reviews2006

  • Oxygen isotope and palaeotemperature records from six Greenland ice‐core stations

    Open AccessSigfús J Johnsen, Dorthe Dahl‐Jensen et al.ARTICLEJournal of Quaternary Science2001

    Oxygen isotope variations spanning the last glacial cycle and the Holocene derived from ice‐core records for six sites in Greenland (Camp Century, Dye‐3, GRIP, GISP2, Renland and NorthGRIP) show strong similarities. This suggests that the dominant influence on oxygen isotope variations reflected in the ice‐sheet records was regional climatic change. Differences in detail between the records probably reflect the effects of basal deformation in the…

  • The Eem Stable Isotope Record along the GRIP Ice Core and Its Interpretation

    Open AccessSigfús J Johnsen, Henrik B Clausen et al.ARTICLEQuaternary Research1995

    A 3029-m-long deep ice core extending nearly to bedrock has been drilled at the very top of the Greenland ice sheet (Summit) by the Greenland Ice-core Project (GRIP), an international European joint effort organized by the European Science Foundation. The ice core reaches back to 250,000 yr B.P. according to dating based partly on stratigraphic methods and partly on ice-flow modeling. A continuous and detailed stable isotope (δ 18 O) profile alon…

  • Ash layers from Iceland in the Greenland GRIP ice core correlated with oceanic and land sediments

    Open AccessKarl Grönvold, Níels Óskarsson et al.ARTICLEEarth and Planetary Science Letters1995

    Four previously known ash layers (Ash Zones I and II, Saksunarvatn and the Settlement layer) all originating in Iceland, have been identified in the Central Greenland ice core GRIP. This correlation of the ash between the different environments is achieved by comparison of the chemical composition of glass shards from the ash. This establishes and confirms detailed correlations between the different types of depositional records and the absolute …

  • Ice-Core Dating of the Pleistocene/Holocene Boundary Applied to a Calibration of the 14 C Time Scale

    Open AccessClaus U Hammer, Henrik B Clausen et al.ARTICLERadiocarbon1986Cited by: 5References: 10

    Seasonal variations in 18 O content, in acidity, and in dust content have been used to count annual layers in the Dye 3 deep ice core back to the Late Glacial. In this way the Pleistocene/Holocene boundary has been absolutely dated to 8770 BC with an estimated error limit of ± 150 years. If compared to the conventional 14 C age of the same boundary a value of Δ 14 C = 53 ± 13‰ is obtained. This Δ 14 C value suggests that 14 C levels during the La…