Stable oxygen (δ18O) and hydrogen (δD) isotopes in precipitation from Inuvik in the western Canadian Arctic (2015-2018)

Precipitation was collected in the city of Inuvik (68.3°N, 133.5°W) in the western Canadian Arctic over 37 months between August 2015 and August 2018. The regular sampling of meteoric water for subsequent stable isotope analysis was conducted at the Aurora Research Institute (Western Arctic Research...

Full description

Bibliographic Details
Main Authors: Fritz, Michael, Wetterich, Sebastian, McAlister, Joel, Meyer, Hanno
Format: Dataset
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 2021
Subjects:
Canada
deuterium excess
global meteoric water line
GMWL
Inuvik
LMWL
local meteoric water line
stable water isotopes
western Arctic
δ18O
δD
DATE/TIME
Precipitation description
δ18O, water
δ Deuterium, water
Deuterium excess
Water sample, precipitation
Mass spectrometer Finnigan Delta-S
Calculated
NUNATARYUK, Permafrost thaw and the changing Arctic coast, science for socioeconomic adaptation NUNATARYUK
Arctic
Aurora Research Institute
permafrost
Online Access:https://dx.doi.org/10.1594/pangaea.935027
https://doi.pangaea.de/10.1594/PANGAEA.935027
Description
Summary:Precipitation was collected in the city of Inuvik (68.3°N, 133.5°W) in the western Canadian Arctic over 37 months between August 2015 and August 2018. The regular sampling of meteoric water for subsequent stable isotope analysis was conducted at the Aurora Research Institute (Western Arctic Research Centre, 191 Mackenzie Road, Inuvik, NT X0E 0T0, Canada). The samples obtained resulted in 134 valid measurements of the isotopic composition of both snow and rain. The oxygen (δ18O) and hydrogen (δD) stable isotope compositions of precipitation were measured in the Stable Isotope Facility of the Alfred Wegener Institute in Potsdam (Germany), using a Finnigan MAT Delta-S mass spectrometer. Values are given as per mil (‰) difference from the Vienna Standard Mean Ocean Water (VSMOW) standard. Deuterium excess (d) was calculated as: d = δD – 8*δ18O.The goal of this data collection is to present a new local meteoric water line (LMWL) from Inuvik in the western Canadian Arctic. This data set fills a gap in the western Arctic, where isotopic data of precipitation are scarce and stem mostly from before the year 2000. Regional studies of meteorology, hydrology, environmental geochemistry and paleoclimate may benefit from this dataset and the new Inuvik LMWL.

Similar Items