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.

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.

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.


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.

Plants are adapted to gusting winds, heavy snows, and widely ranging temperatures. They carry on photosynthesis under brilliant light during short periods of daylight
Height wise they must stay within a few inches of ground because of the strong cold wind and because it is warmest near the ground
.....Collect energy efficiently by holding lots of chlorophyll

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....

Animals

Artic wildlife is circumpolar (surrounding or near either pole of the earth), the same or closely related species are found around the world.

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.


Continue on for more information on:
soils/nutrient flow and the incredible geomorphic features ( polygons, pingos) 

 

Introduction (1)

geomorphic features(3)

small herbivores (5)

carnivores (7)

vegetation plus (2)

soils & nutrient flow (4)

large herbivores (6)

 

E. Iglich and ecology students from previous courses, with much indebtednesss to the many excellent web sites which are cited...