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dc.contributor.advisorGraversen, Rune
dc.contributor.authorBalafkan, Nozhan
dc.date.accessioned2018-08-23T07:13:37Z
dc.date.available2018-08-23T07:13:37Z
dc.date.issued2018-05-15
dc.description.abstractThe behavior of the autumn and winter weather pattern over Europe and Eurasia was investigated during two periods of high and low ice concentration in September over the Kara-Siberian sea. A statistically significant anomalous energy flux from the east Siberian sea to the atmosphere was detected during October of low ice years. Furthermore, an anomalous behavior in the atmospheric circulation was detected during the October of the LIYs. Additionally, statistically significant positive anomaly was observed over northern Europe and central Eurasia during January and February of the years with high ice concentration at the Kara-Siberian sea.en_US
dc.identifier.urihttps://hdl.handle.net/10037/13564
dc.language.isoengen_US
dc.publisherUiT Norges arktiske universiteten_US
dc.publisherUiT The Arctic University of Norwayen_US
dc.rights.accessRightsopenAccessen_US
dc.rights.holderCopyright 2018 The Author(s)
dc.rights.urihttps://creativecommons.org/licenses/by-nc-sa/3.0en_US
dc.rightsAttribution-NonCommercial-ShareAlike 3.0 Unported (CC BY-NC-SA 3.0)en_US
dc.subject.courseIDFYS-3900
dc.subjectKara-Siberian seaen_US
dc.subjectAtmospheric circulationen_US
dc.subjectmidlatitude weather patternen_US
dc.subjectVDP::Matematikk og Naturvitenskap: 400::Fysikk: 430en_US
dc.subjectVDP::Mathematics and natural science: 400::Physics: 430en_US
dc.subjectVDP::Matematikk og Naturvitenskap: 400::Geofag: 450::Meteorologi: 453en_US
dc.subjectVDP::Mathematics and natural science: 400::Geosciences: 450::Meteorology: 453en_US
dc.titleKara-Siberian sea ice anomaly and its impact on the atmosphereen_US
dc.typeMaster thesisen_US
dc.typeMastergradsoppgaveen_US


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Attribution-NonCommercial-ShareAlike 3.0 Unported (CC BY-NC-SA 3.0)
Except where otherwise noted, this item's license is described as Attribution-NonCommercial-ShareAlike 3.0 Unported (CC BY-NC-SA 3.0)