An Arctic iceberg breaks off from a glacier and can be found floating in the water or aground. Icebergs themselves don't exist for many years, but the glaciers that calve them are thousands of years old.
Iceberg timeline:
1,000 B.C.: Snow falls on arctic ice caps and, during the next several months, turns into firn – a granular form of snow.
950 B.C.: The firn is compressed into dense ice because of the added firn and snow that have accumulated on top of what fell 50 years earlier.
Between 950 B.C. and 2002 A.D.: The weight of the ice cap forces the ice to slowly flow seaward.
1993 A.D.: Icebergs are calved – break off of the glacier – because they are weakened by the rising and falling tides on the coast.
1996 A.D.: The icebergs calved three years previous melt. An estimated one percent of icebergs make it as far as the Atlantic Ocean. If an iceberg travels that far, it will melt within months from the warm waters. If an iceberg stops drifting in Baffin Bay, however, it can take more than four years for the iceberg to melt.
Range
Western Greenland's glaciers calve 90 percent of all icebergs found in Newfoundland's waters. This means that between 30,000 and 40,000 icebergs are calved annually.
After calving usually on the west coast of Greenland, icebergs drift to the coast of Newfoundland, which is about 1,800 nautical miles. The average iceberg drift speed is about 0.7 kilometres per hour, but this is influenced by factors including iceberg size, shape, currents, waves and wind. They travel in the Baffin Current, then the Labrador Current and finally reach the Grand Banks of Newfoundland. Once they reach the Grand Banks, icebergs drift either eastward – north of the Flemish Cap – or southward between the Flemish Cap and the Grand Banks – also known as Iceberg Alley.
Link: http://www.canadiangeographic.ca/magazine/ma06/indepth/nathistory.asp
Icebergs
Icebergs are pieces of floating ice that calve (break off) from ice shelves and glaciers. They can be of any size and are very common in the Southern Ocean. Believe it or not, scientists call small icebergs growlers (these are about the size of a small car) while the next biggest size of iceberg are called bergy bits (these are about the size of a house and no, we aren't making the name up!).
Icebergs that calve from ice shelves are tabular (flat topped) but icebergs may also be described as dome-shaped, sloping, pinnacled, weathered or glacier bergs.
The rule that 90% of an iceberg lie underwater is true and this is one of the reasons why they are so dangerous to Ships, as you can't see their shape under water. Another dangerous thing about icebergs is that because they move with the ocean currents, they cannot be marked on navigation charts.
When HMS Endurance is in Antarctica, the Ship's Meteorologists use radar and satellites to help them locate the position of drifting icebergs and this information is also passed on to all the ships in the area. Although HMS Endurance is of a special design so that it can withstand the shocks of constantly breaking through ice, every possible measure is taken to avoid a collision with an iceberg. The most famous Ship to hit an iceberg was the Titanic in 1912.
Scientists use a particular coding system for naming icebergs. When an iceberg is first sighted, it is given a letter of the alphabet (A,B,C or D) and a sequential number.
Satellite pic by NASA of icebergs
The letter of the alphabet relates to the particular sector of Antarctica in which the iceberg was first sighted:A = Bellinshausen/Weddell Sea
B = Amundsen/Eastern Ross Sea
C = Western Ross Sea/ Wilkesland
D = Amery/ Eastern Weddell Sea
Eventually, storms, waves and warmer surface water all help to melt drifting icebergs, but they have been known to last over 6 years.
Link: http://www.visitandlearn.co.uk/factfiles06/ice6.asp
Melting Ice and Sea Levels
Each year about 8 mm (0.3 inch) of water from the entire surface of the oceans goes into the Antarctica and Greenland ice sheets as snowfall. If no ice returned to the oceans, sea level would drop 8 mm every year as much of the deposited snow is water originally from the ocean. Although approximately the same amount of water returns to the ocean in icebergs and from ice melting at the edges, scientists do not know which is greater, the ice going in or the ice coming out. The difference between the ice input and output is called the mass balance and is important because it causes changes in global sea level.
The Archimedes' Principle helps us understand why and how sea levels rise:
Archimedes' Principle - When an object is completely or partially immersed in a fluid, the fluid exerts an upward force on the object equal to the weight of the fluid displaced by the object.
Firstly, when considering melting ice and sea levels, we need to appreciate that ice is either already floating in the ocean or it is grounded on a landmass.
Because of Archimedes' Principle, if the ice is already floating in the ocean, the total mass of the ocean and ice remains unchanged even when the ice melts. Dr. Peter Noerdlinger, a professor at St. Mary’s University in Nova Scotia, Canada, has recently demonstrated that the difference in density between the fresh water ice and salt water of the oceans will add a small amount to sea levels when this ice melts.
However, the real rise in sea levels comes from ice that is grounded on a landmass. As the melted ice flows as water, or falls as ice chunks into the ocean it increases the total volume of the ocean. That is, ice discharged from a grounded ice sheet directly into the ocean has an immediate impact on sea level. Because the Greenland and Antarctic ice sheets are sitting on land and not floating, they have the potential to raise sea levels significantly.
Ice Sheets, Ice Shelves, Icebergs and Sea Ice
To understand the connection between melting ice and sea levels, we also need to appreciate the difference between Ice Sheets, Ice Shelves, Icebergs and Sea Ice.
The Antarctic ice sheet is the largest single mass of ice on Earth. It covers an area of almost 14 million km² and contains 30 million km³ of ice. Around 90% of the fresh water on the Earth's surface is held in the ice sheet, and, according to Richard S. Williams, Jr., United States Geological Survey geologist, if melted, could cause sea levels to rise by 65 meters (213 feet, although the 4th IPCC report suggests a rise of 57 metres or 187 feet). The Greenland ice sheet occupies about 82% of the surface of Greenland, and if melted would cause sea levels to rise by 7 metres (23 feet).
An ice shelf is a thick, floating platform of ice that forms where a glacier or ice sheet flows down to a coastline and onto the ocean surface. Ice shelves are found in Antarctica, Greenland and Canada only. Ice shelves can actually float up and down with the tides, grating against the rocks and eventually breaking apart. Because they are already floating on the water, ice shelves do not raise sea level when they melt (except by a small amount due to the salt-freshwater differential as noted by Noerdlinger).
Ice shelves flow by gravity-driven horizontal spreading on the ocean surface. That flow continually moves ice from the grounding line to the seaward front of the shelf. The primary mechanism of mass loss from ice shelves is iceberg calving. With regards to melting ice and sea levels, and because icebergs are already floating they have little impact on sea levels.
In contrast to the above, sea ice or pack ice is formed on water, is much thinner, and forms throughout the Arctic Ocean and Southern Ocean around the continent of Antarctica. Again, and in terms of melting ice and sea levels, sea ice has little impact on overall sea level rise.
Link: http://www.global-greenhouse-warming.com/melting-ice-and-sea-levels.html
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