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Resources for extending the learning
Featured Process: The World Under the Snow
The recent cold affecting much of the country puts limits on outside activities for lots of people, but there are a lot of active creatures out there who don't mind, as long as the snow is deep enough. They are the denizens of the subnivean, which is not the layer in the drawer below the hand cream, but rather the active world beneath the snow. Subnivean happenings unfold in the space between the ground and the snow that is created as snow gets draped over plants, trees, bushes and other things. We discussed the molecular magic of ice and snow in early December – not only does snow’s molecular structure make it less dense than water, but it also makes snow a great insulator, particularly light, fluffy snow. Just 25 cm of snow can result in constant temperatures a bit above or below 0oC at ground level when surface temperatures plunge to -20-40oC. But don’t trust me. Find your own snow bank, dig a pit, and record the results (click here for lessons). Solidifying warm gelatin in clear canisters might actually be more fun. Keep in mind that snow thrown by plows or shovels will be denser and provide less insulation.
With lots of snow, small rodent populations can explode in winter, since snow increases the habitat where they can move around relatively safe from predators. But not entirely – owls, particularly the Great Gray, are adapted to hear and plunge through 30 cm of snow to capture prey, sometimes leaving perfect marks to tell the tale (of course, they aren’t always so elegant about it and may occasionally underestimate snow depth). However, freeze/thaw cycles will result in a hard enough crust that the owls cannot penetrate, jeopardizing their survival. “Chalk one up for the rodents,” you might think, but that crust can also limit gas exchange to the point where all oxygen below the crust is used up and the rodents die. Crusty conditions can put other wildlife at risk, too. Global warming may lead to more of these cycles, in some areas. And what would happen if there was more winter precipitation, but also warmer weather to melt it quicker? Which species would be the winners and losers? We don’t know the answers, or how exactly numerous factors will interplay, but certainly it will lead to cascading impacts and significant ecosystem changes. Everything is connected.
Towards spring, plants in cavities beneath the snow may have their own greenhouse, getting enough sun and humidity to get a leg up on plants either exposed to the elements or buried under deeper snow, even to the point of blooming. Soil microbes, particularly fungi, may actually reach their peak biomass under the snow.
Here’s more on the ecology of snow, life beneath the snow, and simple activities for producing subnivean dioramas and studying winter temperatures.
Where’s My Cache teaches students about how certain animals, like the Gray jay, are adapted to cold Canadian winters with the use of caches. |
Other Happenings:
Pukak (poo-cack) the layer of bonded, granular snow that covers the ground. Animals travel through the pukak layer, where the heat from the earth keeps them warm.
Siqoq (see-kok) drifting snow, the kind that makes “snow snakes” drift across the snow or road.
Qali (kal-ee) snow that collects on tree branches and fence posts.
Api (ah-pee) snow on the ground.
Anniu(an-nee-you) falling snow.
Get outside for a Snow Tour! Make a trail and write a nature guide for other students to follow. Choose 10 unique points of interest along your trail and write a short description for each one. |