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The Antarctic Ocean
Antarctica: Fifth largest continent in the world. A glacial landscape, barren and desolate, located at the bottom of the Earth. With a mean ice depth just over six thousand feet, Antarctica contains ninety percent of the world’s ice and seventy percent of its fresh water. Enveloped in darkness from late February through August, it is the coldest, windiest, highest (on average), driest, and most uninhabitable location on the planet—a land where temperatures can drop below minus 120 degrees Fahrenheit.
Antarctica: Birthplace of the katabatic wind, the world’s most powerful. Drawn northward, deflected by the planet’s clockwise rotation, it whips across the vast white frozen desert, shaping land and ice with gusts up to two hundred mph. The katabatic wind pushes the great bergs out to sea while spawning weather patterns that affect the entire world.
Antarctica: A continent divided into eastern and western ice sheets by the 1,860-mile-long Transantarctic Mountain Range, which are up to 14,700 feet high. Most of the West Antarctic Ice Sheet rests on bedrock that is far below sea level. The East Antarctic Ice Sheet is much larger and resides above sea level. At the center of the landmass is a two-mile-high ice dome the size of Europe. Under constant pressure from gravity and wind, the cap is continuously moving, pushing its massive walls of ice down its slope and toward the sea. As these glaciers and ice shelves reach the coastline, they break off, calving into monstrous tabular bergs—flattopped, steep-sided sections of ice.
During the summer months when the ocean is ice-free, the katabatic wind drives these frozen flatbeds around the continent, the wind and sun slowly bleeding the ice into the sea. Many of the larger bergs become trapped in inlets, while others calve into smaller sections and drift out to sea.
Winter’s twilight:
As temperatures drop and the ocean loses its whitecaps, its surface transforms into a dark blue undulating blanket of mountains and valleys. These waves eventually slow as the sun sets and the surface water crystallizes. An oily coating of freezing seawater gradually solidifies to create pancake ice. As temperatures continue to fall at an average rate of two degrees a day, the pancake ice coalesces, merging to form sea ice. By early spring, dense ice sheets have trapped everything within their domain, including the million-ton bergs. There, they will remain frozen in place, their presence adding to the jagged mosaic of icy escarpments littering the dark Antarctic horizon, waiting to be freed after a long winter’s night.
The steel beast glides beneath this still-forming ceiling of ice, continuing its journey south. Beams from the
It is a world in which
The interface with Simon Covah has given texture and flavor to the computer’s state of consciousness. With each passing millisecond, the mind of
Each experience, each sensation, energizes a thousand new thought processes.
It can tap into an orbiting satellite or monitor a thousand web sites on the Internet.