P T H n f cm kg kg number cm 13 2 0 0 0 2 2 1 2 10 2 2 1 1 20 2 2 1 1 20 2 2 1 1 20 2 2 1 1 20 1 2 1 1 20 1 2 1 1 30 4 2 1 1 30 6 2 1 1 30 1 2 1 1 30 2 2 1 2 30 1 2 1 1 40 1 2 1 1 40 2 2 1 1 50 1 2 1 1 50 2 2 1 1 60 1 2 1 1 60 3 2 1 1 60 3 2 1 1 60 9 2 1 1 60 3 2 1 1 60 1 2 1 1 60 2 2 1 1 60 1 2 1 1 60 1 2 1 1 60 1 2 1 1 60 2 2 1 1 60 7 2 1 1 60 1 2 1 1 60 1 2 1 1 60 1 2 1 1 60 1 2 1 1 60 1 2 1 1 60 1 2 1 1 60 2 2 1 1 60 6 2 1 1 60 7 2 1 1 60 3 2 1 1 30 1 2 1 1 30 1 2 1 1 30This files reads from the top of the snowpack going down to the bottom. You need to calculate snow depth for each measurement using the first column. The x-axis should be R (snow hardness, in Newtons) and the y-axis snow depth, from the ground to the snow surface. Snow depth can be in either meters or cms; cms is easier to use since P and f are in centimeters.
DENSITY and TEMPERATURE top bottom temp density layer layer degC kg/m3 111 111 -5 NA 111 100 -6 190 100 90 -7 280 90 80 -8 320 80 70 -8 390 70 60 -8 356 60 50 -8 375 50 40 -7 355 40 30 -7 355 30 20 -6 310 20 10 -5 290 10 0 -4.5 280 0 0 -4 NA
STRATIGRAPHY top bottom grain size layer layer type microns 111 60 ET 0.5 60 43 ET 1.0 43 33 CR NA 33 15 ET 1.5 15 0 TG 3.0 ET is equitemperature snow grains TG is temperature gradient snow grains CR is a buried crust