Water isotope diffusion rates from the NorthGRIP ice core for the last 16,000 years - Glaciological and paleoclimatic implications

V. Gkinis; S. B. Simonsen; S. L. Buchardt; J. W. C. White; B. M. Vinther

doi:10.1016/j.epsl.2014.08.022

Water isotope diffusion rates from the NorthGRIP ice core for the last 16,000 years - Glaciological and paleoclimatic implications

V. Gkinis, S. B. Simonsen, S. L. Buchardt, J. W. C. White, B. M. Vinther

Is-, Klima- og Geofysik

50 Citationer (Scopus)

Originalsprog	Engelsk
Tidsskrift	Earth and Planetary Science Letters
Vol/bind	405
Sider (fra-til)	132-141
ISSN	0012-821X
DOI	https://doi.org/10.1016/j.epsl.2014.08.022
Status	Udgivet - 1 nov. 2014

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10.1016/j.epsl.2014.08.022

Citationsformater

@article{2bb32e338edf4b60b42ae41046dc3b46,

title = "Water isotope diffusion rates from the NorthGRIP ice core for the last 16,000 years - Glaciological and paleoclimatic implications",

keywords = "ice cores, water isotopes, paleotemperatures, firn diffusion, Greenland, Holocene",

author = "V. Gkinis and Simonsen, {S. B.} and Buchardt, {S. L.} and White, {J. W. C.} and Vinther, {B. M.}",

year = "2014",

month = nov,

day = "1",

doi = "10.1016/j.epsl.2014.08.022",

language = "English",

volume = "405",

pages = "132--141",

journal = "Earth and Planetary Science Letters",

issn = "0012-821X",

publisher = "Elsevier",

}

TY - JOUR

T1 - Water isotope diffusion rates from the NorthGRIP ice core for the last 16,000 years - Glaciological and paleoclimatic implications

AU - Gkinis, V.

AU - Simonsen, S. B.

AU - Buchardt, S. L.

AU - White, J. W. C.

AU - Vinther, B. M.

PY - 2014/11/1

Y1 - 2014/11/1

KW - ice cores

KW - water isotopes

KW - paleotemperatures

KW - firn diffusion

KW - Greenland

KW - Holocene

U2 - 10.1016/j.epsl.2014.08.022

DO - 10.1016/j.epsl.2014.08.022

M3 - Journal article

SN - 0012-821X

VL - 405

SP - 132

EP - 141

JO - Earth and Planetary Science Letters

JF - Earth and Planetary Science Letters

ER -

Water isotope diffusion rates from the NorthGRIP ice core for the last 16,000 years - Glaciological and paleoclimatic implications

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