To the Greeks, arktos (bear) was the land lying in the direction of the Great Bear or Big Dipper, a prominent constellation of the northern sky. Even today a precise definition of the word Arctic eludes us (Fig. 1). Cartographers, astronomers, and, to some extent, dynamic meteorologists view the Arctic as the area enclosed by the Arctic Circle (66°33′N), north of which the sun does not rise on the winter solstice or set on the summer solstice. Oceanographers define Arctic waters as having a temperature near 0°C and a salinity of approximately 30 parts per thousand. Geologists use the presence of permafrost (perenially frozen ground) to define the Arctic. Climatologists, for the most part, use vegetation cover as an integrator of climate and surface conditions, thus defining Arctic as the area north of the tree line. Köppen (see reference in Wilson, 1967) approximated the tree line by the 10°C isotherm (line of constant temperature) of the warmest month, while others define as tundra...
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© 1987 Van Nostrand Reinhold
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Alt, B.T. (1987). Arctic climates . In: Climatology. Encyclopedia of Earth Science. Springer, Boston, MA. https://doi.org/10.1007/0-387-30749-4_13
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DOI: https://doi.org/10.1007/0-387-30749-4_13
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