Monday, February 20, 2006

North Slope of Alaska


RedOrbit.com puts out all sorts of pictures of pace and Earth images. I found this one interesting of the North Slope of Alaska. I have been to Barrow twice now so I feel closer to the area. I think the following article helps to explain the differences between ice floes and what actually happens in a frozen ocean.


Along the northern Arctic shores of Alaska, ice, snow, and cold dominate the landscape, even on a sunny day in June. This false-color satellite image shows electric blue ice and snow, the green vegetation of the hardy plants and mosses of the tundra, the deep blue of flowing rivers and open ocean, and pink-hued outcrops of bare, rocky ground.
The tundra runs the length of northern Alaska and is known as the North Slope. Only a surface "active layer" of the tundra thaws each season; most of the soil is permanently frozen year-round. On top of this permafrost, water flows to sea via shallow, braided streams or settles into pools and ponds. Along the bottom of the image the rugged terrain of the Brooks Range Mountains is snow-covered in places (blue areas) and exposed (pink areas) in others.
The sea hadn't surrendered to approaching summer. Along the coast, fast ice still clings to the shore in a solid, frozen sheet. At the top of the scene is the drifting sea ice. A dark blue strip of open water, known as a flaw lead, separates the fast ice from the drifting sea ice. Because the drift ice wanders freely with the wind and sea currents, it shatters into pieces that become rounded from the constant jostling.

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