Typical sea ice types are shown here near the end of the winter season. Also shown is how often sea ice has been present at any location on the 26th February over the last 30 years. Based on the observations of sea ice extents and ice types over the last 30 years, this map shows how frequently sea ice has been present and what is the most likely predominant ice type and where. Sea ice is any form of ice that is found at sea and has originated from the freezing of seawater. The ice type gives an indication of the thickness of sea ice such as new ice, grey ice, grey-white ice, first year ice, and old ice. Ice represents a danger for navigation. Information on sea ice is essential in estimating transportation costs, and what type of vessel is appropriate.
Late Winter Sea Ice Conditions shows the typical sea ice types near the end of the winter season (February 26) and as well as frequency of sea ice on that date. The frequency of sea ice indicates how often sea ice has been present on February 26 over the last 30 years.
The ice type gives an indication of the thickness of sea ice. When sea ice first forms it is referred to as new ice. As winter progresses it grows in extent and thickness. As sea ice thickens it is referred to successively as grey ice, grey–white ice and first year ice. During the summer sea ice melts and any first year ice remaining at the end of the summer melt is then renamed "old ice" on October 1.
Various ice types can be present in a given area, but one of them will be predominant. The predominant ice type is the one in greatest concentration in a particular area. However, because of the danger that old ice represents for navigation, and if 40% or more of the area contains old ice then the predominant ice type will be old ice even if thinner ice in greater concentration is present.
This map shows the frequency of sea ice and what is the most likely predominant ice type encountered near the end of the winter season (February 26). In the winter, sea ice is usually present in all coastal waters of Canada except for those of British Columbia where warm ocean currents from the south prevent the formation of sea ice. There is old ice in the Arctic and first year ice in most of the remaining waters except for thinner grey and grey-white ice in portions of the Gulf of St. Lawrence and East Newfoundland waters. This situation is normal in the winter as shown by the very high frequencies of sea ice present during the winter. In some years, with colder temperatures and strong north-westerly winds sea ice will extend further eastward and southward along the east coast as shown by lower frequencies of sea ice in those areas. The extent of sea ice in those areas is limited by the heat exchange from warmer and deeper waters offshore that melts the sea ice moving in those areas.
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Navigating in ice and smoke in the Gulf of St.Lawrence during winter time.
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Landsat 7 image, taken on February 14th, 2002, in the St.Lawrence River at Baie Comeau (Quebec)
Also shown are areas of permanent ice and the estimated maximum extent of ice observed outside Canadian waters. Areas designated permanent ice indicate where ice has been observed all year round throughout the period 1969 to 1998. The estimated maximum extent of ice outside Canadian waters displays where ice has been observed on February 26 at least once over the 30 year period.
Two animations are created for sea ice. Each animation was presented in two different formats: flash and html. The Atlas of Canada relies on Macromedia’s technology for the delivery of multimedia content. The Atlas of Canada media player will attempt to detect whether you have the necessary software installed, and will give you notice if you do not. In order to play the animations in flash, you must install the Macromedia Flash Player. Installation instructions on Macromedia Flash Player are available at Macromedia Web site.