Iceberg

For other uses, see Iceberg (disambiguation).

Icebergs at Cape York, Greenland.

An iceberg is a large piece of ice from freshwater that has broken off from a snow-formed glacier or ice shelf and is floating in open water. It may subsequently become frozen into pack ice. Alternatively, it may come to rest on the seabed in shallower water, causing ice scour (also known as ice gouging) or becoming an ice island.

Etymology

The word "iceberg" is a partial loan translation from Dutch ijsberg, literally meaning ice mountain, cognate to Danish Isbjerg, German Eisberg, Low Saxon Iesbarg and Swedish/Norwegian Isberg.

Overview

Iceberg calved from the Ross Ice Shelf.

Because the density of pure ice is about 920 kg/m³, and that of sea water about 1025 kg/m³, typically only one-tenth of the volume of an iceberg is above water. The shape of the underwater portion can be difficult to judge by looking at the portion above the surface. This has led to the expression "tip of the iceberg", for a problem or difficulty that is only a small manifestation of a larger problem.

Icebergs generally range from 1 to 75 metres (3–250 ft) above sea level and weigh 100,000 to 200 000 tons. The tallest known iceberg in the North Atlantic was 168 metres (550 ft) above sea level, making it the height of a 55-storey building. Despite their size, the icebergs of Newfoundland move an average of 17 kilometres a day (10 mi). These icebergs originate from the glaciers of western Greenland, and may have an interior temperature of -15 to -20°C (5 to -4 °F).

Though usually confined by winds and currents to move close to the coast, the largest icebergs recorded have been calved, or broken off, from the Ross Ice Shelf of Antarctica. Iceberg B-15, photographed by satellite in 2000, measured 295 km long and 37 km wide (183-23 mi), with a surface area of 11,000 km² (4,250 mi²). The mass was estimated around three billion tonnes.

When an iceberg melts, it makes a fizzing sound called "Bergie Seltzer"". This sound is made when compressed air bubbles trapped in the iceberg pop. The bubbles come from air trapped in snow layers that later became glacial ice.

Ice campers who camp on top of flat or hollowed icebergs are known as icebergers.

Classification

Size

A photomontage visualising what the whole of an iceberg might look like

Names for various sizes of iceberg are not universal, but usually follow a similar pattern. The size classification in the table below is used by the International Ice Patrol:

Size Category	Height	Length
Growler	Less than 1 metre (3.3 ft)	Less than 5 metres (16 ft)
Bergy Bit	1–5 metres (3.3–16.4 ft)	5–15 metres (16–49 ft)
Small	5–15 metres (16–49 ft)	15–60 metres (49–197 ft)
Medium	15–45 metres (49–148 ft)	60–120 metres (200–390 ft)
Large	45–75 metres (148–246 ft)	120–200 metres (390–660 ft)
Very Large	Over 75 metres (246 ft)	Over 200 metres (660 ft)

Recent large icebergs

• Iceberg B-15 11,000 square kilometres, 2000,
• Iceberg B-15A, 3,100 square kilometres (1,200 sq mi), broke off 2003
• Iceberg C-19, 5,500 sq km, 2002
• Iceberg B-9, 5,390 sq km, 1987
• Iceberg D-16, 120 sq mi, 2006
• Iceberg B-17B 140 square kilometres (54 sq mi), 1999, shipping alert issued December 2009

Shape

In addition to the above size classification, there is also a type of classification based on shape. The two basic types of iceberg forms are tabular and non-tabular.

Tabular icebergs have steep sides and a flat top, much like a plateau, with a length-to-height ratio of more than 5:1. This type of iceberg can be quite large, as in the case of Pobeda Ice Island.

Non-tabular icebergs have different shapes, and include:

Twilight iceberg in midnight sun from Ilulissat

• Dome: An iceberg with a rounded top.
• Pinnacle: An iceberg with one or more spires.
• Wedge: An iceberg with a steep edge on one side and a slope on the opposite side.
• Dry-Dock: An iceberg that has eroded to form a slot or channel.
• Blocky: An iceberg with steep, vertical sides and a flat top. It differs from tabular icebergs in that its shape is more like a block than a flat sheet.

Monitoring

An iceberg in Greenland.

Iceberg A22A in the South Atlantic Ocean.

Icebergs are monitored worldwide by the U.S. National Ice Center (NIC), established in 1995, which produces analyses and forecasts of Arctic, Antarctic, Great Lakes and Chesapeake Bay ice conditions. More than 95% of the data used in its sea ice analyses are derived from the remote sensors on polar-orbiting satellites that survey these remote regions of the Earth.

The NIC is the only organization that names and tracks all Antarctic Icebergs. It assigns each iceberg larger than 10 nautical miles (18 km) along at least one axis a name composed of a letter indicating its point of origin and a running number. The letters used are as follows:

• A – longitude 0° to 90° W (Bellingshausen Sea, Weddell Sea)
• B – longitude 90° W to 180° (Amundsen Sea, Eastern Ross Sea)
• C – longitude 90° E to 180° (Western Ross Sea, Wilkes Land)
• D – longitude 0° to 90° E (Amery Ice Shelf, Eastern Weddell Sea)

Iceberg B15, which calved from the Ross Ice Shelf in 2000 and initially had an area of 11,000 km², was the largest iceberg ever recorded. It broke apart in November 2002. The largest remaining piece of it, Iceberg B-15A, with an area of 3,000 km², was still the largest iceberg on Earth until it ran aground and split into several pieces October 27, 2005. It has been determined that the cause of the breakup was an ocean swell generated by an Alaskan storm 6 days earlier and 13,500 km (8,370 miles) away.

History

In the 20th century, several scientific bodies were established to study and monitor the icebergs. The International Ice Patrol, formed in 1914 in response to the Titanic disaster, monitors iceberg dangers near the Grand Banks of Newfoundland and provide the "limits of all known ice" in that vicinity to the maritime community.

In March 2008, a chunk of Antarctic ice, about seven times the size of Manhattan, suddenly collapsed, putting an even greater portion of glacial ice at risk, and an ice shelf about the size of Connecticut was "hanging by a thread" as of March 25, 2008.

Technology history

Damn iceberg, you look so smug just because you thought that you sunk theRMS Titanic; there's even a smudge of red paint much like the Titanic's on your base!

There was no system in place before April 1912 to track icebergs, to guard against ship collisions. The sinking of the RMS Titanic, which caused the deaths of 1,523 of its 2,228 passengers, created the demand for a system to observe icebergs. For the remainder of the ice season of that year, the United States Navy patrolled the waters and monitored ice flow. In November 1913, the International Conference on the Safety of Life at Sea met in London to devise a more permanent system of observing icebergs. Within three months, the participating maritime nations had formed the International Ice Patrol (IIP). The goal of the IIP was to collect data on meteorology and oceanography in order to measure currents, iceflow, ocean temperature, and salinity levels. They published their first records in 1921, which allowed for a year-by-year comparison of iceberg movement.

New technologies monitor icebergs. Aerial surveillance of the seas in the early 1930s allowed for the development of charter systems that could accurately detail the ocean currents and iceberg locations. In 1945, experiments tested the effectiveness of radar in detecting icebergs. A decade later, oceanographic monitoring outposts were established for the purpose of collecting data; these outposts continue to serve in environmental study. A computer was first installed on a ship for the purpose of oceanographic monitoring in 1964, which allowed for a faster evaluation of data. By the 1970s, icebreaking ships were equipped with automatic transmissions of satellite photographs of ice in Antarctica. Systems for optical satellites had been developed, but were still limited by weather conditions. In the 1980s, drifting buoys were used in Antarctic waters for oceanographic and climate research. They are equipped with sensors that measure ocean temperature and currents. Side-Looking Airborne Radar (SLAR) made it possible to acquire images regardless of weather conditions. On November 4, 1995, Canada launched RADARSAT-1. Developed by the Canadian Space Agency, it provides images of Earth for both scientific and commercial purposes. This system was the first to use Synthetic Aperture Radar (SAR), which sends microwave energy to the ocean surface and records the reflections to track icebergs. The European Space Agency launched ENVISAT on March 1, 2002, an environmental satellite which uses Advanced Synthetic Aperture Radar (ASAR). This can detect changes in surface height accurately. The Canadian Space Agency launched RADARSAT-2 in December 2007, which uses SAR and multipolarization modes and follows the same orbit path as RADARSAT-1.

External links

• Iceberg Finder Service for east coast of Canada
• Icebergs of The Arctic and Antarctic
• Iceberg Google maps - South Georgia