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Exploring Arctic Transpolar Drift During Dramatic Sea Ice Retreat
Author(s) -
Gascard JeanClaude,
Festy Jean,
le Goff Hervé,
Weber Matthieu,
Bruemmer Burghard,
Offermann Michael,
Doble Martin,
Wadhams Peter,
Forsberg René,
Hanson Susan,
Skourup Henriette,
Gerland Sebastian,
Nicolaus Marcel,
Metaxian JeanPhilippe,
Grangeon Jacques,
Haapala Jari,
Rinne Eero,
Haas Christian,
Wegener Alfred,
Heygster Georg,
Jakobson Erko,
Palo Timo,
Wilkinson Jeremy,
Kaleschke Lars,
Claffey Kerry,
Elder Bruce,
Bottenheim Jan
Publication year - 2008
Publication title -
eos, transactions american geophysical union
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.316
H-Index - 86
eISSN - 2324-9250
pISSN - 0096-3941
DOI - 10.1029/2008eo030001
Subject(s) - arctic sea ice decline , climatology , arctic ice pack , arctic , sea ice , arctic geoengineering , environmental science , global warming , ice albedo feedback , climate change , the arctic , cryosphere , arctic dipole anomaly , oceanography , drift ice , geology
The Arctic is undergoing significant environmental changes due to climate warming. The most evident signal of this warming is the shrinking and thinning of the ice cover of the Arctic Ocean. If the warming continues, as global climate models predict, the Arctic Ocean will change from a perennially ice‐covered to a seasonally ice‐free ocean. Estimates as to when this will occur vary from the 2030s to the end of this century. One reason for this huge uncertainty is the lack of systematic observations describing the state, variability, and changes in the Arctic Ocean.

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