snow depth

Physical and chemical characteristics of stream-associated snow patches in Fryxell Basin, McMurdo Dry Valleys, Antarctica during the 2021-2022 austral summer

Abstract: 

Snow patches within and adjacent to stream channels in the Fryxell Basin of Taylor Valley, Antarctica were sampled during the 2021-2022 austral summer as part of the McMurdo Dry Valleys Long Term Ecological Research program. This data package includes snow pit measurements (snow temperature, depth, density, and water equivalent) as well as chemical characteristics of snow samples that were analyzed for nutrient, cation, and anion concentrations.

LTER Core Areas: 

Dataset ID: 

9040

Associated Personnel: 

1199
1200
1201

Short name: 

strm_snowpatch

Data sources: 

snowpatch

Methods: 

Measurements for snow pits dug across Taylor Valley were obtained for this dataset during November and December of the 2021-2022 field season. Snow patches were specifically sampled early in the year before the streams had started to flow. Snow pits were dug both within stream channels and adjacent to stream channels for 10 streams across Lake Fryxell Basin and Commonwealth Stream in Taylor Valley. Snow depth of each pit was recorded and snow density was measured using a snow cutter of known volume and a spring scale. Snow density and snow depth was then used to calculate snow water equivalent (SWE) of each snow patch sampled.

Snow samples for each pit were also collected using a snow core device. The snow samples were put in a whirlpack bag and transported back to the field laboratory at F6 camp. At F6, samples were melted and filtered for nutrient, cation, and anion analysis. Because not all samples had enough water for all analysis, nutrient analysis was prioritized and anions/cations were not able to be run for every sample. For anions and cations, 50 mls (for each) of the melted snow water was filtered through a Nucleopore (0.4 µm) filter. The filtrate was saved and stored at +4 °C for future analysis. For nutrients, 100 ml of raw melted snow sample was filtered through an ashed GF/C filter. The filtrate was saved and frozen at -20 °C for future analysis.

All analysis was run by the MCM LTER at the Crary Laboratory at McMurdo Station or at the University of Colorado Boulder, in the same way that stream water samples are rum as part of the long-term sample collection for the MCM LTER. Anions and cations were run in the Crary Laboratory at McMurdo Station between 2021-12-03 and 2022-01-14 with a dilution factor of 1. Nutrients (N & SRP) were run at the University of Colorado Boulder on 2022-06-07.

Maintenance: 

This work was supported by the US National Science Foundation grants #OPP-1637708 and #OPP-2224760 for Long Term Ecological Research.

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