Skip to main content
. 2016 Mar 17;45(5):516–537. doi: 10.1007/s13280-016-0770-0

Table 2.

Overview of observation methods in quantifying various snow parameters

Target parameter(s) Method(s) Reference(s)
Destructive ground-based snow observations
Snow depth  Simple (avalanche) or semi-automated probes (e.g. MagnaProbe) e.g. Sturm et al. (2006)
Specific surface area (SSA) (i.e. the surface area of ice per unit mass)  Near-infrared photography and infrared reflectance methods e.g. Matzl and Schneebeli (2006), Gallet et al. (2009) Arnaud et al. (2011), and Montpetit et al. (2012)
Penetration resistance and deviation of snow density, grain parameters, and SSA.  SnowMicroPen (Highly resolved measurements (250 measurements/mm) Schneebeli and Johnson (1998) and Proksch et al. (2015)
Snowfall/new snow  Snow board (i.e. new-snow observations are being conducted by placing a board (snow board) on the snow surface and revisiting it every 24 h to read the additional snow height e.g. Fierz et al. (2009)
Liquid water content in snow  ‘Denoth capacity probe’ or ‘Finnish Snow Fork’ (e.g. used to deriving dielectric/conduction properties of the snow) Denoth (1994) and Sihvola and Tiuri (1986)
Non-destructive ground-based snow observations
Snow depth  Acoustic snow-depth sensors, ultrasonic methods, lasers, manual readings at stakes, and automatic readings utilizing time-lapse cameras
Snow density and snow bulk liquid water content  Upward-looking ground penetrating radar (upGPR)
 Combination of upGPR with buried GPS sensors (allows for direct conversion for density, SWE and liquid water content)
Time domain reflectometer (TDR)
e.g. Mitterer et al. (2011), Avanzi et al. (2014), Heilig et al. (2015), Schmid et al. (2014, 2015), and Stacheder (2005)
Snow water equivalent (SWE)  Snow pillows or snow scales weigh the mass of the snowpack above the sensors and convert this to SWE
Snow albedo  Net radiometer e.g. Michel et al. (2008)
Snow-cover fraction Derived from hourly-daily digital photos acquired from automatic time-lapse digital cameras installed in terrestrial areas, e.g. near glaciers and ice fields e.g. Bernard et al. (2013)
Avalanche hazard and activity  Seismic sensor Reiweger et al. (2015)
 Infrasound arrays e.g. Van Herwijnen and Schweizer (2011), Havens et al. (2014)