For many of the experiments being carried out as part of the SIPEX voyage, knowing the density of the snow cover is an important part of the data being collected. This is particularly true for the EM measurements and the radar altimetry teams as their results differ depending on the density of the snow. The way the scientists find snow density is very straight forward and can easily be replicated in the classroom. The simply plunge a cylinder of known diameter and length into the snow and remove a ‘snow core’. Then they weigh the snow that they removed and calculate the density.
Density is defined as mass per unit volume, in other words it’s the mass of a given amount of substance divided by the volume occupied by that amount.
This activity can be used to illustrate the concept of density, it allows students to revisit volume and the area of a circle.
This activity involves students sampling two different types of ‘snow’ and calculating and comparing their densities.
If students are finding it hard to visualise what is meant by kg/m3, you can get 12 metre sticks and ask students to arrange them to form a cube. This will show them what 1m3 looks like. You can then pass around a 1kg mass (1kg bag of flour would do) and point out to students that X amount of that mass is in a volume of 1m3 for a particular substance (see table below). For example if you take the density of air, just over that 1 lot of that mass is found in every 1m3 of air, whereas for sea water 1030 lots of that mass are found in a m3.
| Material | Density (kg/m-3) |
| Sea Water | 1030 |
| Fresh Water | 1000 |
| Ice | 920 |
| Snow | 100-500 |
| Air | 1.29 |
| Steam(100oC) | 0.6 |
| (values quoted at standard room temp. and pressure) | |
Note: Snow is basically many small ice crystals separated by air. So dry powdery 'light' snow has a low density(~100kg/m3), whereas wet 'heavy' snow has a higher density (~500kg/m3).
This activity would be a good introduction to 'Sea Ice and Salinity', also found in the Teachers Toolbox.