[HTML][HTML] A review of air–ice chemical and physical interactions (AICI): liquids, quasi-liquids, and solids in snow

T Bartels-Rausch, HW Jacobi, TF Kahan… - Atmospheric …, 2014 - acp.copernicus.org
Snow in the environment acts as a host to rich chemistry and provides a matrix for physical
exchange of contaminants within the ecosystem. The goal of this review is to summarise the …

An overview of snow photochemistry: evidence, mechanisms and impacts

AM Grannas, AE Jones, J Dibb… - Atmospheric …, 2007 - acp.copernicus.org
It has been shown that sunlit snow and ice plays an important role in processing
atmospheric species. Photochemical production of a variety of chemicals has recently been …

Glacial ecosystems

A Hodson, AM Anesio, M Tranter… - Ecological …, 2008 - Wiley Online Library
There is now compelling evidence that microbially mediated reactions impart a significant
effect upon the dynamics, composition, and abundance of nutrients in glacial melt water …

Changes in environment over the last 800,000 years from chemical analysis of the EPICA Dome C ice core

EW Wolff, C Barbante, S Becagli, M Bigler… - Quaternary Science …, 2010 - Elsevier
The EPICA ice core from Dome C extends 3259m in depth, and encompasses 800ka of
datable and sequential ice. Numerous chemical species have been measured along the …

Nitrogen and oxygen isotopic constraints on the origin of atmospheric nitrate in coastal Antarctica

J Savarino, J Kaiser, S Morin… - Atmospheric …, 2007 - acp.copernicus.org
Throughout the year 2001, aerosol samples were collected continuously for 10 to 15 days at
the French Antarctic Station Dumont d'Urville (DDU)(66° 40'S, l40° 0'E, 40 m above mean …

Photolysis imprint in the nitrate stable isotope signal in snow and atmosphere of East Antarctica and implications for reactive nitrogen cycling

MM Frey, J Savarino, S Morin, J Erbland… - Atmospheric …, 2009 - acp.copernicus.org
The nitrogen (δ 15 N) and triple oxygen (δ 17 O and δ 18 O) isotopic composition of nitrate
(NO 3−) was measured year-round in the atmosphere and snow pits at Dome C, Antarctica …

Factors controlling variability in the oxidative capacity of the troposphere since the Last Glacial Maximum

LT Murray, LJ Mickley, JO Kaplan… - Atmospheric …, 2014 - acp.copernicus.org
The oxidative capacity of past atmospheres is highly uncertain. We present here a new
climate–biosphere–chemistry modeling framework to determine oxidant levels in the present …

Seasonal variations in N and O isotopes of nitrate in snow at Summit, Greenland: Implications for the study of nitrate in snow and ice cores

MG Hastings, EJ Steig… - Journal of Geophysical …, 2004 - Wiley Online Library
Nitrogen and oxygen isotopes of NO3− have been measured in snow and firn from Summit,
Greenland. The 15N/14N and 18O/16O ratios of NO3− in recently fallen snow are similar to …

[HTML][HTML] The SP19 chronology for the South Pole Ice Core–Part 1: volcanic matching and annual layer counting

DA Winski, TJ Fudge, DG Ferris, EC Osterberg… - Climate of the …, 2019 - cp.copernicus.org
Abstract The South Pole Ice Core (SPICEcore) was drilled in 2014–2016 to provide a
detailed multi-proxy archive of paleoclimate conditions in East Antarctica during the …

Air–snow transfer of nitrate on the East Antarctic Plateau–Part 1: Isotopic evidence for a photolytically driven dynamic equilibrium in summer

J Erbland, WC Vicars, J Savarino… - Atmospheric …, 2013 - acp.copernicus.org
Here we report the measurement of the comprehensive isotopic composition (δ 15 N, Δ 17 O
and δ 18 O) of nitrate at the air–snow interface at Dome C, Antarctica (DC, 75° 06'S, 123° …