DRIFT ICE
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(Redirected from Pack ice)
'Drift ice' consists of sea ice that floats on the surface of the water in cold regions, as opposed to fast ice, which is attached ("fastened") to a shore. Usually drift ice is carried along by winds and sea currents, hence its name, "drift ice".
When the drift ice is driven together into a large single mass, it is called 'pack ice'. Typically areas of pack ice are identified by high percentage of surface coverage by ice: e.g., 80-100%.
An 'ice floe' is a large piece of drift ice that might range from tens-of-yards to several miles in diameter. Wider chunks of ice are called 'ice fields'.
The two major ice packs are the Arctic ice pack and the Antarctic ice pack.
In many areas such as the Baltic, drift ice is traditionally a seasonal event, appearing in winter and vanishing in warmer seasons.
Seasonal ice drift in the Sea of Okhotsk by the northern coast of HokkaidÅ, Japan has become a tourist attraction of this area with harsh climate.[1] Sea of Okhotsk is the southernmost area in the Northern hemisphere where drift ice may be observed.
The major aspects of the drift ice are:
★ Security of navigation
★ Climatic impact, see "Polar ice packs" for details
★ Geological impact
★ Biosphere influence, see Ecology of sea ice
The most important areas of pack ice are the Polar ice packs formed from seawater in the Earth's polar regions: the Arctic ice pack of the Arctic Ocean and the Antarctic ice pack of the Southern Ocean. Polar packs significantly change their size during seasonal changes of the year. Because of vast amounts of water added to or removed from the oceans and atmosphere, the behavior of polar ice packs has a significant impact of the global changes in climate.
★ Ice drift
★ Drift ice station
★ Sea ice
★ Polynya
★ Shelf ice
★ Iceberg
1. A Port's Ice Is Thinning, and So Is Its Tourist Trade, ''New York Times'', March 14, 2006
★ Drift Ice as a Geologic Agent, google video by US Geologic Survey
★ Ice in the Sea Chapter from Nathaniel Bowditch's ''American Practical Navigator''
★ Cryosphere Today : Current Arctic sea ice conditions
★ Data source for sea ice picture
★ Marine Modeling and Analysis Branch
★ Everything you ever wanted to know about sea ice but were afraid to ask
★ Animation of the movement of sea ice, September 2003 through May of 2004.
★ NSIDC Sea Ice Index
Drift ice, Greenland
'Drift ice' consists of sea ice that floats on the surface of the water in cold regions, as opposed to fast ice, which is attached ("fastened") to a shore. Usually drift ice is carried along by winds and sea currents, hence its name, "drift ice".
When the drift ice is driven together into a large single mass, it is called 'pack ice'. Typically areas of pack ice are identified by high percentage of surface coverage by ice: e.g., 80-100%.
Ice floes / Pack ice
An 'ice floe' is a large piece of drift ice that might range from tens-of-yards to several miles in diameter. Wider chunks of ice are called 'ice fields'.
The two major ice packs are the Arctic ice pack and the Antarctic ice pack.
In many areas such as the Baltic, drift ice is traditionally a seasonal event, appearing in winter and vanishing in warmer seasons.
Seasonal ice drift in the Sea of Okhotsk by the northern coast of HokkaidÅ, Japan has become a tourist attraction of this area with harsh climate.[1] Sea of Okhotsk is the southernmost area in the Northern hemisphere where drift ice may be observed.
The major aspects of the drift ice are:
★ Security of navigation
★ Climatic impact, see "Polar ice packs" for details
★ Geological impact
★ Biosphere influence, see Ecology of sea ice
| Contents |
| Polar ice packs |
| See also |
| References |
Polar ice packs
The most important areas of pack ice are the Polar ice packs formed from seawater in the Earth's polar regions: the Arctic ice pack of the Arctic Ocean and the Antarctic ice pack of the Southern Ocean. Polar packs significantly change their size during seasonal changes of the year. Because of vast amounts of water added to or removed from the oceans and atmosphere, the behavior of polar ice packs has a significant impact of the global changes in climate.
See also
★ Ice drift
★ Drift ice station
★ Sea ice
★ Polynya
★ Shelf ice
★ Iceberg
References
1. A Port's Ice Is Thinning, and So Is Its Tourist Trade, ''New York Times'', March 14, 2006
★ Drift Ice as a Geologic Agent, google video by US Geologic Survey
★ Ice in the Sea Chapter from Nathaniel Bowditch's ''American Practical Navigator''
★ Cryosphere Today : Current Arctic sea ice conditions
★ Data source for sea ice picture
★ Marine Modeling and Analysis Branch
★ Everything you ever wanted to know about sea ice but were afraid to ask
★ Animation of the movement of sea ice, September 2003 through May of 2004.
★ NSIDC Sea Ice Index
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psst.. try this: add to faves
