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McMurdo Sound

Geographic location

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Karte des McMurdo-Sunds mit den Trockentälern
Meile · Public domain

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Through Sound (geography), Antarctica and Airplane

Captain James Clark Ross discovered the sound in February 1841 and named it after Lieutenant Archibald McMurdo of HMS Terror. The sound serves as a resupply route for cargo ships and airplanes that land on floating ice airstrips near McMurdo Station. The McMurdo seasonal Ice Runway was operated from October to December from the 1950s to the 2010s, then in December the ice breaks up and McMurdo port is opened by an Icebreaker ship and ships can resupply the Antarctic bases.

Physical characteristics

Boundary and extents

The sound extends approximately 55 kilometers (34 mi) in length and width, and opens into the larger Ross Sea to the north. To the south, the sound is bounded by the Ross Ice Shelf cavity, to the west lies the Royal Society Range, and to the east is Ross Island. McMurdo Sound is separated from the McMurdo Ice Shelf (part of the Ross Ice Shelf) by the Haskell Strait. Winter Quarters Bay lies at the south end of the Sound and is the southernmost port on Earth.

While the sound is navigable, it contains a significant amount of drift ice, especially along the shoreline of Winter Quarters Bay. The pack ice that girdles the shoreline at Winter Quarters Bay and elsewhere in the sound presents a considerable obstacle to surface ships. Vessels require ice-strengthened hulls and often have to rely upon escort by icebreakers. Less than 10 percent of McMurdo Sound's shoreline is free of ice.

During austral winter, McMurdo Sound presents a large expanse of surface ice. In summer, ships approaching the sound are often blocked by various amounts of first-year ice, fast ice (connected to the shoreline), and hard multi-year ice. Subsequently, icebreakers are required for maritime resupply missions to McMurdo Station.

Ross Island is the southernmost piece of land in Antarctica that is accessible by ship. In addition, the harbour at McMurdo's Winter Quarters Bay is the world's southernmost seaport (Department of Geography, Texas A&M University). The access by ships depends upon favorable ice conditions.

Tourism is increasingly popular in other parts of Antarctica but remains limited in McMurdo Sound due to the extreme sea conditions.

Temperatures

Cold circumpolar currents of the Southern Ocean shrink the flow of warm South Pacific or South Atlantic waters reaching McMurdo Sound and other Antarctic coastal waters. McMurdo Sound experiences katabatic winds from the Antarctic polar plateau. McMurdo Sound freezes over with sea ice about 3 metres (9.8 ft) thick during the winter. During the austral summer when the pack ice breaks up, wind and currents may push the ice northward into the Ross Sea, stirring up cold bottom currents that spill into the ocean basins. Temperatures during the winter months at McMurdo Station have dropped as low as −28 °C (−18 °F). December and January are the warmest months, with average highs at −4 °C (25 °F).

Effects of wind

Polar winds are a driving force behind weather systems arising from three surface zones that converge at McMurdo Sound: the polar plateau and the Transantarctic Mountains, the Ross Ice Shelf, and the Ross Sea. These surface zones create a range of dynamic weather systems. Cold, heavy air descending rapidly from the polar plateau at elevations of 3,000 metres (9,800 ft) or more spawns fierce katabatic winds. These dry winds can reach hurricane force when they reach the Antarctic coast. Wind instruments recorded Antarctica's highest wind velocity at the coastal station Dumont d'Urville in July 1972 at 320 kilometres per hour (200 mph) (Australian Government Antarctic Division).

Prevailing winds into McMurdo Sound shoot between mountain passes and other land formations, producing blizzards known locally as "Herbies". Such blizzards can occur any time of year. Residents of McMurdo Station and Scott Base have dubbed the nearby White Island and Black Island "Herbie Alley" due to winds that funnel blizzards between the islands (Field Manual for the U.S. Antarctic Program).

Overall the continent's extremely cold air does not hold enough moisture for significant snowfall. The annual snowfall on Ross Island averages only 17.6 centimetres (6.9 in). Snowfall in Antarctica's interior is far less at 5 centimetres (2.0 in). Snow seldom accumulates on the McMurdo Dry Valleys on the western shores of McMurdo Sound.

McMurdo Sound provides an important component in Antarctica's global effects upon climate. A key factor is the polar winds that can drive the sound's pack ice into the Ross Sea summer or winter. Frigid katabatic winds rake subsequently exposed water, causing sea ice to form. Freezing surface water excludes salt from the water below; leaving behind heavy, cold water that sinks to the ocean floor. This process repeats along Antarctica's coastal areas, spreading cold sea water into Earth's ocean basins.

According to an interview with climatologist Gerd Wendler, published in the National Science Foundation's Antarctic Sun, one could dive to the ocean floor anywhere in the world and encounter water from the coast of Antarctica. "Seventy-five percent of all the bottom water, wherever you are, comes from Antarctica."

Temperatures

  • Average mean sea-level temp: −20 °C (−4 °F).
  • Monthly mean range: −3 °C (27 °F) in January to −28 °C (−18 °F) in August.
  • Stormiest months: February and October.

Wildlife

A rich sea life thrives under the barren expanse of McMurdo Sound's ice pack. Frigid waters that would kill many other fish in the world sustain the Antarctic notothenioid, a bony "ice fish" related to walleyes and perch. Cactus sponges, globe sponges, starfish, sea urchins, and sea anemones are also present. Large sea spiders inhabit the depths of the sound and feed on sea anemones. Antarctic krill flourish in the upper depths of the waters.

Antarctic penguins, emperor penguins, and Adélie penguins live in and around the sound. The Weddell seal, leopard seal, and crabeater seal have been spotted, as well as orcas.

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