Environmental Data: IceCube_microCT_Snow_grainsize
Description
The specific surface area (SSA) of different snow types were measured with the IceCube instrument and the Scanco Medical microCT 40. In addition, the snow ...
Citation
Martin, J., Schneebeli, M. (2022). IceCube_microCT_Snow_grainsize. EnviDat. https://www.doi.org/10.16904/envidat.333.
Resources
IceCube and MicroCT data
The file contains all micro-CT and IC measurements for snow types A, B, C, D and E used in our study. All samples were processed (and stored) in a cold laboratory at -15°C.
IceCube and MicroCT dataGrain survey of snow particles
The file contains all measurements of the artificial particles for snow types A, B, C, D and E, including the artificial particle mass in the Petri dish.
Grain survey of snow particlesTARTES simulations
Jupyter notebook with TARTES simulations.
TARTES simulationsStatistics of samples
Statistics of samplesgreenland_summit_density_ssa_data
The file contains all data for the plot in figure 1 of the co-located density and SSA measurement at Summit, Greenland in May 2015, conducted by Schneebeli, Proksch, Schmid.
greenland_summit_density_ssa_dataartificial_snow_data set
The file contains all micro-CT and IC measurements of the artificial snow data set. The data set was originally produced to investigate the influence of black carbon on SSA measurements.
artificial_snow_data setSMP_measurements
SMP measurement files for snow types A, B, C and D.
SMP_measurementsInfluence of black carbon on the measurement of the specific surface of snow with the near infrared method - Philipp Baumann
These experiments investigate different possible errors by measuring the specific surface area (SSA) of snow with the near infrared method. The influence of black carbon on this measurement was disproved, the theory was therefore validated. It shows that sunlight has no influence on the measurement with the IceCube. Wind drift snow as thin layer on the sample can increase the measured value of the specific surface by a few percent. This could be part of the error, observed in former measurements at SLF. As reference for the measured SSA values with the near infrared method, computer tomography was used to verify the SSA values.
Influence of black carbon on the measurement of the specific surface of snow with the near infrared method - Philipp Baumann