Isotope composition of snow from individual snowfall in the northeast of Europe, December 2003

Isotope composition of snow samples from individual snowfall was measured on the transect of approximately 1400 km through the northeast of Europe from Konosha station through Inta Town and Seida Town up to Polar Ural. Stable isotope contents of Oxygen-18 and Deuterium as well as Deuterium excess ar...

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Bibliographic Details
Main Authors: Vasil'chuk, Yurij K, Chizhova, Julia N, Papesch, W
Format: Dataset
Language:English
Published: PANGAEA 2022
Subjects:
Arkhangelsk Oblast
Russia
Date/Time of event
deuterium excess
Eletskaya
European North
Event label
HAND
Inta
Komi
Konosha
Latitude of event
Location
Longitude of event
Mikun
oxygen and hydrogen stable isotopes
Pechora
Polar_Ural-2
Sample ID
Sampling by hand
Seida-2
snowfall
snowfall measurements
Stable isotope analysis
Temperature
air
Ukhta
Weather station/meteorological observation
WST
Yadriha
Yamal-Nenets
δ18O
δ Deuterium
Arkhangelsk
nenets
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.939386
https://doi.org/10.1594/PANGAEA.939386
Description
Summary:Isotope composition of snow samples from individual snowfall was measured on the transect of approximately 1400 km through the northeast of Europe from Konosha station through Inta Town and Seida Town up to Polar Ural. Stable isotope contents of Oxygen-18 and Deuterium as well as Deuterium excess are not constant in uniform air mass, but strongly vary depending on condensation temperature. It is demonstrated that the values of Oxygen-18 and deuterium decrease by 1.4 and 10.8 ‰ per 1 degree of latitude. With decreasing Oxygen-18 content by 8.17 ‰ and Deuterium by 60.3 ‰, Deuterium excess increases by 8.1 ‰. Data was collected inthe northeast of Europe between December 23rd and 24th 2003.

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