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An Oxygen-Isotope Paleothermometer from Ice in Siberian Permafrost

Datos Bibliográficos

ID24085658
AutoresVladimir I Nikolayev, Dmitry V Mikhalev
Año1995
Volumen43
Número1
Páginas14-21
Fecha de publicación1995-01-01
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaQuaternary Research (JOURNAL)
Identificadores de la revistaISSN: 0033-5894 • E-ISSN: 1096-0287
EditorialCambridge University Press (CUP) (PUBLISHER)
DOI10.1006/qres.1995.1002
OpenAlexW2072617905
IdiomaEN
Citas recibidas4
Referencias citadas10

There is a clear linear relationship between mean annual (or seasonal) air temperature at the Earth's surface and the mean oxygen isotopic composition of precipitation in polar regions. Whereas this relationship is well preserved in polar ice caps, it may not be in permafrost because freshly deposited snow in permafrost areas is subjected to great deflation and drifting by wind. Moreover, melting and freezing within the snow cover and the active layer can lead to isotopic fractionation. The δ 18 O of recent ground ice also depends on its geomorphic context and on the lithology (content of organic matter) of ice-containing sediments. Nevertheless, mean cold-season air temperature near the ground surface and δ 18 O in recent ground ice are highly correlated. Therefore, the δ 18 O of ground ice (ice cement and segregated ice) in permafrost areas can be used for paleoclimatic reconstructions.

Atmospheric sciences · Climatology · Cryosphere · Geochemistry · Geomorphology · Isotopes of oxygen · Permafrost · Polar · Sea ice · Snow · Climate change and permafrost · Geology · Groundwater and Isotope Geochemistry · Methane Hydrates and Related Phenomena · Oceanography

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    Open Access•W Dansgaard•Tellus A Dynamic Meteorology and…•2012

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Obras citantes distintas4
Citas por año0,15
Intervalo de citas2000 - 2016 (17)
Velocidad de citaciónhistorical
Altamente citadoNo
Tipos de citaNeutras: 3
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