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[HTML][HTML] A review of air–ice chemical and physical interactions (AICI): liquids, quasi-liquids, and solids in snow
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 …
exchange of contaminants within the ecosystem. The goal of this review is to summarise the …
An overview of snow photochemistry: evidence, mechanisms and impacts
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 …
atmospheric species. Photochemical production of a variety of chemicals has recently been …
Glacial ecosystems
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 …
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
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 …
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
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 …
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
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 …
(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
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 …
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
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 …
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
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 …
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
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° …
and δ 18 O) of nitrate at the air–snow interface at Dome C, Antarctica (DC, 75° 06'S, 123° …