W Dansgaard

Datos Biográficos

ID5592585
NOMBREW Dansgaard
NOMBRESW
APELLIDODansgaard
FIRMADANSGAARD W
AFILIACIONESUniversity of Copenhagen
VERIFICADONo
TOTAL DE OBRAS7
TOTAL DE CITAS0
TOTAL COMO AUTOR7
TOTAL COMO EDITOR0
PRIMER AÑO DE PUBLICACIÓN1964
AÑO MÁS RECIENTE DE PUBLICACIÓN2012
ÍNDICE H0

  • Stable isotopes in precipitation

    Open AccessW DansgaardARTICLETellus A Dynamic Meteorology and…2012

    In chapter 2 the isotopic fractionation of water in some simple condensation-evaporation processes are considered quantitatively on the basis of the fractionation factors given in section 1|2. The condensation temperature is an important parameter, which has got some glaciological applications. The temperature effect (the δ's decreasing with temperature) together with varying evaporation and exchange appear in the “amount effect” as high δ's in s…

  • Evidence for general instability of past climate from a 250-kyr ice-core record

    Open AccessW Dansgaard, Sara Johnsen et al.ARTICLENature1993

  • Irregular glacial interstadials recorded in a new Greenland ice core

    Open AccessSara Johnsen, S J Johnsen et al.ARTICLENature1992

  • In Brief

    Open AccessG Hattersley-Smith, Heather Myers et al.ARTICLEPolar Record1990

    An abstract is not available for this content so a preview has been provided. Please use the Get access link above for information on how to access this content

  • Greenland ice sheet evidence of post-glacial volcanism and its climatic impact

    Open AccessC U Hammer, H B Clausen et al.ARTICLENature1980

  • Speculations about the Next Glaciation

    Open AccessW Dansgaard, S J Johnsen et al.ARTICLEQuaternary Research1972

    A spectacular 10‰ drop in the 18 O 16 O ratio (δ) in precipitation indicative of rapid cooling occurred at Camp Century, Greenland, 89,500 y.a. The timing is based upon an assumption of δ periodicity being constant in time. Onset of the Wisconsin pleniglacial is reflected by 6‰ δ drop at 73,000 BP. Similar event might have occurred 109,000 y.a., but the core at corresponding depth is missing. Could it also happen today?

  • Stable isotopes in precipitation

    Open AccessW DansgaardARTICLETellus B: Chemical and Physical…1964

    In chapter 2 the isotopic fractionation of water in some simple condensation-evaporation processes are considered quantitatively on the basis of the fractionation factors given in section 1.2. The condensation temperature is an important parameter, which has got some glaciological applications. The temperature effect (the δ's decreasing with temperature) together with varying evaporation and exchange appear in the “amount effect” as high δ's in s…