I.
How did we get frozen poles? A.Many of thousands of years ago, when the
continents were centered differently. ocean currents used to circulate
to poles, warming them B. Towards the N. Pole, land masses encircled
the pole, enclosing the Arctic Ocean and cutting off its circulation (
see map below). The waters could no longer be warmed by more southern
ocean currents, and thus they froze. As the sun's rays are too weak at
the poles, major seasonal melting in the region can not occur. C. At S. Pole, Antarctic ice masses drifted
toward the pole and eventually settled directly over it. Because of this
large consolidated land mass, ocean currents could no longer circulate
within and the land froze. Now it's all frozen year round.
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II. What defines the tundra? A. The tundra begins where the taiga, the cold northern forest, ends. There are almost no trees in the tundra. B. Physically it includes a thin band in Europe and wider portions of Siberia and North America. C. The transition between tundra and taiga is more of an ecotone than a borderline. Flying north over the transition zone, you would see the trees become smaller and more spread apart until there was only a sparse spotting of dwarf spruces. |
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III. Tell me about the climate.
A. The tundra eceives very little precipitation
- less than 25 cm or 9.8 inches/yr, half as rain and half as snow B. Most of snow falls in Oct.
and Nov., when the air is warm enough to hold some
moisture. C. If you only considered precipitation it
could be considered a desert, but permafrost keeps moisture imprisoned
there. D. The tundra has a very short growing season
- about 2 months, because the snow reflects the sun's weak rays until
they become strong enough to melt it. The ecosystem compensates by its
high growth and turnover rate during this period. Average temperature
of the warmest month lies between 50F (10C) and 32F (0C). E. Springtime brings a rude awakening- together
with the late snow and sleet, ice breaks off surface of rivers and crashes
into banks, tearing apart everything in its path. This is quickly replaced
with a moderating transition to summer and its green revival. F. Daylight lasts almost 24
hrs a day during summer. IV. What is the tundra like? A. With almost no trees, land formations stand
out i bleak contrast to the exposed landscape. B. Lakes, ponds, and marshes are surprsingly
common. C. Although very cold most of year, on the
warmest days of summer, it's possible to swim in the lakes. The average
temp is only 10 degrees C in summer, but some days get quite warm and
even hot.


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Vegetation on the tundra consists of grasses, sedges, lichens, dwarf heath,willow shrubs together with associated mosses and lichens.. As one moves south, the vegetation changes into birch-lichen woodland, and then into needleleaf forest. |
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Plants are adapted to gusting winds, heavy
snows, and widely ranging temperatures. They carry on photosynthesis under
brilliant light during short periods of daylight Large root systems, often several times the size of above-ground biomass. Plants send stored energy, in the form of carbohydrates, into large root systems so energy can be stored for spring when the growing season is short and plants must grow quickly. Growth is spread out over several growing seasons because each season is so short - some plants take several growing seasons for their seeds to develop fully - bud lies beneath snow all winter and continue developing in the following summer Instead of seeds, many plants reproduce by sending out runners, much like the ramet trees which appear as individuals but are genetically identical... Berry bearing bushes and the artic willow spread horizontally instead of vertically to avoid transpirational loss of water by the dry wind and to form a dense mat which stays warmer than above Most vegetation has compact shoot/leaf structures with leathery coatings to conserve moisture Go to this page for more on the vegetation of the Tundra.... |
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Animals Smaller herbivores:
Arctic hare, or snowshoe rabbit, and lemming, pika,
marmot feed on grasses, sedge and other vegetation. The
ptarmigan, a grouselike bird which we mentioned earlier can
change it feather color to match the
seasons.Go
to this page for more info on this group Larger herbivores: Musk-ox,
caribou, and reindeer are the dominant large grazers,
feeding on grass, sedge, lichen, and willow.However also
common are the mountain goats, and big-horned sheep.
Go
to this page for more info on this group Carnivores: include the wolf,
artic fox, and snowy owl. Polar bears, and sometimes brown
bears are seen.Go
to this page for more info on this group Insects such as black flies
and mosquitoes are abundant as well as butterflies, beetles,
and grasshoppers. Many birds nest in the tundra
shrubbery in summer, migrating to milder climates before the
winter season sets in.
Artic
wildlife is circumpolar (surrounding or near either pole of
the earth), the same or closely related species are found
around the world.
Continue on for more information on:
soils/nutrient flow and the
incredible geomorphic
features ( polygons, pingos)
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E. Iglich and ecology students from previous courses, with much indebtednesss to the many excellent web sites which are cited...