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- Drift_ice abstract "Drift ice is any sea ice other than fast ice, the latter being attached ("fastened") to the shoreline or other fixed objects (shoals, grounded icebergs, etc.). Drift ice is carried along by winds and sea currents, hence its name. When drift ice is driven together into a large single mass (>70% coverage), it is called pack ice. Wind and currents can pile up that ice to form ridges up to several metres in height. These represent a challenge for icebreakers and offshore structures operating in cold oceans and seas. Drift ice consists of floes, individual pieces of sea ice 20 metres (66 ft) or more across. There are names for various floe sizes: small – 20 metres (66 ft) to 100 metres (330 ft); medium – 100 metres (330 ft) to 500 metres (1,600 ft); big – 500 metres (1,600 ft) to 2,000 metres (6,600 ft); vast – 2 kilometres (1.2 mi) to 10 kilometres (6.2 mi); and giant – more than 10 kilometres (6.2 mi).Seasonal ice drift in the Sea of Okhotsk by the northern coast of Hokkaidō, Japan has become a tourist attraction of this area with harsh climate, and is one of the 100 Soundscapes of Japan. The Sea of Okhotsk is the southernmost area in the Northern hemisphere where drift ice may be observed.Drift ice affects: Security of navigation Climatic impact (see Polar ice packs) Geological impact Biosphere influence (see Ecology of sea ice)The two major ice packs are the Arctic ice pack and the Antarctic ice pack. 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 on global changes in climate.".
- Drift_ice thumbnail Greenland_East_Coast_7.jpg?width=300.
- Drift_ice wikiPageExternalLink cryosphere.
- Drift_ice wikiPageExternalLink ~eisatlas.
- Drift_ice wikiPageExternalLink seaice_index.
- Drift_ice wikiPageExternalLink seaice.
- Drift_ice wikiPageExternalLink iceinfo.html.
- Drift_ice wikiPageExternalLink videoplay?docid=-780082861495345281.
- Drift_ice wikiPageExternalLink seaice.
- Drift_ice wikiPageExternalLink halfsize_20030928-20040510.avi.
- Drift_ice wikiPageExternalLink chapt34.pdf.
- Drift_ice wikiPageID "665139".
- Drift_ice wikiPageRevisionID "585205817".
- Drift_ice hasPhotoCollection Drift_ice.
- Drift_ice subject Category:Earth_phenomena.
- Drift_ice subject Category:Glaciology.
- Drift_ice subject Category:Sea_ice.
- Drift_ice comment "Drift ice is any sea ice other than fast ice, the latter being attached ("fastened") to the shoreline or other fixed objects (shoals, grounded icebergs, etc.). Drift ice is carried along by winds and sea currents, hence its name. When drift ice is driven together into a large single mass (>70% coverage), it is called pack ice. Wind and currents can pile up that ice to form ridges up to several metres in height.".
- Drift_ice label "Drift ice".
- Drift_ice label "Drijfijs".
- Drift_ice label "Hielo a la deriva".
- Drift_ice label "Pack".
- Drift_ice label "Treibeis".
- Drift_ice label "流氷".
- Drift_ice sameAs Treibeis.
- Drift_ice sameAs Hielo_a_la_deriva.
- Drift_ice sameAs Pack.
- Drift_ice sameAs 流氷.
- Drift_ice sameAs 유빙.
- Drift_ice sameAs Drijfijs.
- Drift_ice sameAs m.025tyg0.
- Drift_ice sameAs Q1378564.
- Drift_ice sameAs Q1378564.
- Drift_ice wasDerivedFrom Drift_ice?oldid=585205817.
- Drift_ice depiction Greenland_East_Coast_7.jpg.
- Drift_ice isPrimaryTopicOf Drift_ice.