This study examined the spatial and temporal variability of chemistry in the seasonal snowpack of the Glacier Lakes catchments in southeastern Wyoming. Snow board data revealed high pH snows (mean pH> 5.0) had higher mean SO4^2- concentrations than low pH snows (11.8 μeq L-1 versus 8.5 μeg L- 1) but lower mean NO3- concentrations (8.2 μeq L-1 versus 10.0 μeg L-1). The high pH snows were also deeper and had higher mean values for Ca^2+, Na^+, and Mg^2+, but lower mean conductivity and density. Different source areas may explain the differences between these two types of snow.hydrology collectio
This article reviews several aspects of snow hydrochemistry: the chemistry of snowfall including che...
This paper describes the physical and chemical properties of the snowpack on John Evans Glacier, Ell...
Abstract The chemical composition of seasonal snow covers was studied in the taiga-tundra transition...
The spatial variability of ionic concentrations in snowpack at the Glacier Lakes Ecosystem Experimen...
During 1993–97, samples of the full depth of the Rocky Mountain snowpack were collected at 52 sites ...
Seasonal snowpack chemistry data from the Rocky Mountain region of the US was examined to identify l...
This study quantifies spatial and temporal patterns in snow water equivalent (SWE), chemistry, and w...
Snow melt is a predominant source of water in the mountains of Colorado. Water quality of this snow ...
This paper describes the temporal variations in acidity and main dissolved ion concentrations of pre...
Temperate glaciers are highly sensitive to climatic and environmental changes. Studying the chemical...
Samples collected from four snow pits at Eclipse Icefield, Yukon, Canada, were analyzed for stable i...
Surface snow observations were carried out on many glaciers in the Arctic. The observational sites w...
Measurements of various inorganic species in snow collected in central and southern California durin...
In order to elucidate the spatial variation of chemicals deposited with snowfall in central Japan an...
Chemical records from alpine ice cores provide an invaluable source of paleoclimatic and environment...
This article reviews several aspects of snow hydrochemistry: the chemistry of snowfall including che...
This paper describes the physical and chemical properties of the snowpack on John Evans Glacier, Ell...
Abstract The chemical composition of seasonal snow covers was studied in the taiga-tundra transition...
The spatial variability of ionic concentrations in snowpack at the Glacier Lakes Ecosystem Experimen...
During 1993–97, samples of the full depth of the Rocky Mountain snowpack were collected at 52 sites ...
Seasonal snowpack chemistry data from the Rocky Mountain region of the US was examined to identify l...
This study quantifies spatial and temporal patterns in snow water equivalent (SWE), chemistry, and w...
Snow melt is a predominant source of water in the mountains of Colorado. Water quality of this snow ...
This paper describes the temporal variations in acidity and main dissolved ion concentrations of pre...
Temperate glaciers are highly sensitive to climatic and environmental changes. Studying the chemical...
Samples collected from four snow pits at Eclipse Icefield, Yukon, Canada, were analyzed for stable i...
Surface snow observations were carried out on many glaciers in the Arctic. The observational sites w...
Measurements of various inorganic species in snow collected in central and southern California durin...
In order to elucidate the spatial variation of chemicals deposited with snowfall in central Japan an...
Chemical records from alpine ice cores provide an invaluable source of paleoclimatic and environment...
This article reviews several aspects of snow hydrochemistry: the chemistry of snowfall including che...
This paper describes the physical and chemical properties of the snowpack on John Evans Glacier, Ell...
Abstract The chemical composition of seasonal snow covers was studied in the taiga-tundra transition...