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Snowfall and water stable isotope variability in East Antarctica controlled by warm synoptic events

Citation

Servettaz, APM and Orsi, AJ and Curran, MAJ and Moy, AD and Landais, A and Agosta, C and Winton, VHL and Touzeau, A and McConnell, JR and Werner, M and Baroni, M, Snowfall and water stable isotope variability in East Antarctica controlled by warm synoptic events, Journal of Geophysical Research: Atmospheres, 125, (17) Article e2020JD032863. ISSN 2169-897X (2020) [Refereed Article]


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Copyright 2020 American Geophysical Union

DOI: doi:10.1029/2020JD032863

Abstract

Understanding climate proxy records that preserve physical characteristics of past climate is a prerequisite to reconstruct long‐term climatic conditions. Water stable isotope ratios (δ18O) constitute a widely used proxy in ice cores to reconstruct temperature and climate. However, the original climate signal is altered between the formation of precipitation and the ice, especially in low‐accumulation areas such as the East Antarctic Plateau. Atmospheric conditions under which the isotopic signal is acquired at Aurora Basin North (ABN), East Antarctica, are characterized with the regional atmospheric model Modèle Atmosphérique Régional (MAR). The model shows that 50% of the snow is accumulated in less than 24 days year−1. Snowfall occurs throughout the year and intensifies during winter, with 64% of total accumulation between April and September, leading to a cold bias of −0.86°C in temperatures above inversion compared to the annual mean of −29.7°C. Large snowfall events are associated with high‐pressure systems forcing warm oceanic air masses toward the Antarctic interior, which causes a warm bias of +2.83°C. The temperature‐δ18O relationship, assessed with the global atmospheric model ECHAM5‐wiso, is primarily constrained by the winter variability, but the observed slope is valid year‐round. Three snow δ18O records covering 2004–2014 indicate that the anomalies recorded in the ice core are attributable to the occurrence of warm winter storms bringing precipitation to ABN and support the interpretation of δ18O in this region as a marker of temperature changes related to large‐scale atmospheric conditions, particularly blocking events and variations in the Southern Annular Mode.

Item Details

Item Type:Refereed Article
Keywords:snow fall, water stable isotopes, East Antarctic, Aurora Basin North, precipitation
Research Division:Earth Sciences
Research Group:Physical geography and environmental geoscience
Research Field:Palaeoclimatology
Objective Division:Environmental Policy, Climate Change and Natural Hazards
Objective Group:Understanding climate change
Objective Field:Effects of climate change on Antarctic and sub-Antarctic environments (excl. social impacts)
UTAS Author:Curran, MAJ (Dr Mark Curran)
UTAS Author:Moy, AD (Dr Andrew Moy)
ID Code:140706
Year Published:2020
Web of Science® Times Cited:4
Deposited By:Oceans and Cryosphere
Deposited On:2020-09-02
Last Modified:2021-04-28
Downloads:2 View Download Statistics

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