These files include data of volumetric liquid water content and wet-snow fraction measured in layered snow during infiltration experiments in a cold laboratory. Twelve experiments were performed using snow with different grain size and under different water input rates. Profiles are reported in terms of depth from the top surface of each sample (first column). Additional information may be found in the mentioned paper
Evaluating and improving snow models and outflow predictions for hydrological applications is hinder...
ABSTRACT. Under melt–freeze conditions crusts may evolve within a snowpack, which may favour avalanc...
Measurements from a spatial array of thermistors set in a natural snowpack are used to track the pro...
Data of liquid water flow around a capillary barrier in snow are still limited. To gain insight into...
The heterogeneous movement of liquid water through the snowpack during precipitation and snowmelt l...
The effect of capillary barriers in layered snowcovers has been examined through use of a numerical...
From 2-4 April 2014 about 50 researchers attended the workshop „Liquid water in snow – measurements ...
The capillary pressure and flux were measured in an old wet snowpack on Mt. Seymour, British Columbi...
Scientists with expertise in avalanche formation, remote sensing issues, and other cryospheric matte...
The liquid water content (lwc) of wet snow is a fundamental parameter in determining snow properties...
Recent mathematical models treat a natural snow-pack as a mixture body consisting of solid ice grain...
The quantity of liquid water in the snowpack defines its wetness. The temporal evolution of snow wet...
ABSTRACT: Starting 1968, basic investigations have been performed of snow electromagnetic parameters...
Field trials of the dilution technique for measuring snow liquid water content show that the refined...
A field method of determining the free water content of snow by measuring the density to which wet s...
Evaluating and improving snow models and outflow predictions for hydrological applications is hinder...
ABSTRACT. Under melt–freeze conditions crusts may evolve within a snowpack, which may favour avalanc...
Measurements from a spatial array of thermistors set in a natural snowpack are used to track the pro...
Data of liquid water flow around a capillary barrier in snow are still limited. To gain insight into...
The heterogeneous movement of liquid water through the snowpack during precipitation and snowmelt l...
The effect of capillary barriers in layered snowcovers has been examined through use of a numerical...
From 2-4 April 2014 about 50 researchers attended the workshop „Liquid water in snow – measurements ...
The capillary pressure and flux were measured in an old wet snowpack on Mt. Seymour, British Columbi...
Scientists with expertise in avalanche formation, remote sensing issues, and other cryospheric matte...
The liquid water content (lwc) of wet snow is a fundamental parameter in determining snow properties...
Recent mathematical models treat a natural snow-pack as a mixture body consisting of solid ice grain...
The quantity of liquid water in the snowpack defines its wetness. The temporal evolution of snow wet...
ABSTRACT: Starting 1968, basic investigations have been performed of snow electromagnetic parameters...
Field trials of the dilution technique for measuring snow liquid water content show that the refined...
A field method of determining the free water content of snow by measuring the density to which wet s...
Evaluating and improving snow models and outflow predictions for hydrological applications is hinder...
ABSTRACT. Under melt–freeze conditions crusts may evolve within a snowpack, which may favour avalanc...
Measurements from a spatial array of thermistors set in a natural snowpack are used to track the pro...