Vis enkel innførsel

dc.contributor.authorYang, Qinghua
dc.contributor.authorXiu, Yongwu
dc.contributor.authorLuo, Hao
dc.contributor.authorWang, Jinfei
dc.contributor.authorLandy, Jack Christopher
dc.contributor.authorBushuk, Mitchell
dc.contributor.authorWang, Yiguo
dc.contributor.authorLiu, Jiping
dc.contributor.authorChen, Dake
dc.date.accessioned2023-09-06T12:26:32Z
dc.date.available2023-09-06T12:26:32Z
dc.date.issued2023-06-20
dc.description.abstractIn the context of global warming, Arctic sea ice has declined substantially during the satellite era (Kwok 2018). The retreating and thinning of Arctic sea ice provide opportunities for human activities in the Arctic, such as tourism, fisheries, shipping, natural resource exploitation, and wildlife management; however, new risks emerge. To ensure the safety and emergency management of human activities in the Arctic, reliable Arctic sea ice prediction is essential.en_US
dc.identifier.citationYang, Xiu, Luo, Wang, Landy, Bushuk, Wang, Liu, Chen. Better synoptic and subseasonal sea ice thickness predictions are urgently required: a lesson learned from the YOPP data validation. Environmental Research Letters. 2023;18(7)
dc.identifier.cristinIDFRIDAID 2169266
dc.identifier.doi10.1088/1748-9326/acdcaa
dc.identifier.issn1748-9326
dc.identifier.urihttps://hdl.handle.net/10037/30758
dc.language.isoengen_US
dc.publisherIOP Publishingen_US
dc.relation.journalEnvironmental Research Letters
dc.rights.holderCopyright 2023 The Author(s)en_US
dc.rights.urihttps://creativecommons.org/licenses/by/4.0en_US
dc.rightsAttribution 4.0 International (CC BY 4.0)en_US
dc.titleBetter synoptic and subseasonal sea ice thickness predictions are urgently required: a lesson learned from the YOPP data validationen_US
dc.type.versionpublishedVersionen_US
dc.typeJournal articleen_US
dc.typeTidsskriftartikkelen_US
dc.typePeer revieweden_US


Tilhørende fil(er)

Thumbnail

Denne innførselen finnes i følgende samling(er)

Vis enkel innførsel

Attribution 4.0 International (CC BY 4.0)
Med mindre det står noe annet, er denne innførselens lisens beskrevet som Attribution 4.0 International (CC BY 4.0)