Water stable isotopes in snow along a traverse of the West Antarctic Ice Sheet: insights into moisture origins, air-masses distillation history, and climatic value

Abstract This study investigated the water isotopic content (δ18O, δD, d-excess) of the surface snow along a 995 km traverse over the West Antarctic Ice Sheet from the Möller Ice Stream – Institute Ice Stream to the upper reaches of the Pine Island Glacier drainage basin. The purpose of this study w...

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Bibliographic Details
Published in:Anais da Academia Brasileira de Ciências
Main Authors: ANDRESSA MARCHER, RONALDO T. BERNARDO, JEFFERSON C. SIMÕES, JEFFREY AUGER
Format: Article in Journal/Newspaper
Language:English
Published: Academia Brasileira de Ciências 2022
Subjects:
water stable isotopes
surface snow
isotopic fractionation
air masses
moisture origin
WAIS
Science
Q
Antarctic
Weddell Sea
Austral
West Antarctic Ice Sheet
Bellingshausen Sea
Pacific
Weddell
Pine Island Glacier
Institute Ice Stream
Möller Ice Stream
Antarc*
Ice Sheet
Online Access:https://doi.org/10.1590/0001-3765202220210353
https://doaj.org/article/5aeedf7bd5a945b2b59bdf50d9dc68b1
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Summary:Abstract This study investigated the water isotopic content (δ18O, δD, d-excess) of the surface snow along a 995 km traverse over the West Antarctic Ice Sheet from the Möller Ice Stream – Institute Ice Stream to the upper reaches of the Pine Island Glacier drainage basin. The purpose of this study was to evaluate the climatic record preserved in the snow. We analyzed 92 surface samples (~0.15–0.20 m deep), retrieved during 2014/2015 austral summer from every ~10 km along the traverse route, using the laser spectroscopy technique. We computed the isotopic-geographical characteristics and spatial co-isotopic empirical relationships and compared the isotopic results with the tropospheric mean annual temperature and air mass trajectories. Our isotopic results were sensitive to capturing the well-known climatic asymmetry between the Amundsen-Bellingshausen Sea (ABS; which receives more influence from warmer (oceanic) air masses) and Weddell Sea (WS; more influenced by colder (continental) air masses) sectors. Further, the spatial distribution of δs and d-excess and the co-isotopic relationships reflect two preferential fractionation paths: one from the coast of the ABS sector to the WS sector, and another from the coast of the WS sector to the inland. The Pacific Ocean is confirmed as the primary source of moisture.

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