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A modeling study of coastal circulation and landfast ice in the nearshore Beaufort and Chukchi seas using CIOM
dc.contributor.authorWang, Jiaen_US
dc.contributor.authorMizobata, Koheien_US
dc.contributor.authorBai, Xuezhien_US
dc.contributor.authorHu, Haoguoen_US
dc.contributor.authorJin, Meibingen_US
dc.contributor.authorYu, Yanlingen_US
dc.contributor.authorIkeda, Motoen_US
dc.contributor.authorJohnson, Walteren_US
dc.contributor.authorPerie, Williamen_US
dc.contributor.authorFujisaki, Ayumien_US
dc.date.accessioned2014-08-06T16:50:02Z
dc.date.availableWITHHELD_11_MONTHSen_US
dc.date.available2014-08-06T16:50:02Z
dc.date.issued2014-06en_US
dc.identifier.citationWang, Jia; Mizobata, Kohei; Bai, Xuezhi; Hu, Haoguo; Jin, Meibing; Yu, Yanling; Ikeda, Moto; Johnson, Walter; Perie, William; Fujisaki, Ayumi (2014). "A modeling study of coastal circulation and landfast ice in the nearshore Beaufort and Chukchi seas using CIOM." Journal of Geophysical Research: Oceans 119(6): 3285-3312.en_US
dc.identifier.issn2169-9275en_US
dc.identifier.issn2169-9291en_US
dc.identifier.urihttps://hdl.handle.net/2027.42/108088
dc.description.abstractThis study investigates sea ice and ocean circulation using a 3‐D, 3.8 km CIOM (Coupled Ice‐Ocean Model) under daily atmospheric forcing for the period 1990–2008. The CIOM was validated using both in situ observations and satellite measurements. The CIOM successfully reproduces some observed dynamical processes in the region, including the Bering‐inflow‐originated coastal current that splits into three branches: Alaska Coastal Water (ACW), Central Channel branch, and Herald Valley branch. In addition, the Beaufort Slope Current (BSC), the Beaufort Gyre, the East Siberian Current (ESC), mesoscale eddies, and seasonal landfast ice are well simulated. The CIOM also reproduces reasonable interannual variability in sea ice, such as landfast ice, and anomalous open water (less sea ice) during the positive Dipole Anomaly (DA) years, vice versa during the negative DA years. Sensitivity experiments were conducted with regard to the impacts of the Bering Strait inflow (heat transport), onshore wind stress, and sea ice advection on sea ice change, in particular on the landfast ice. It is found that coastal landfast ice is controlled by the following processes: wind forcing, Bering Strait inflow, and sea ice dynamics. Key Points Modeling landfast ice and nearshore processes Reveal mesoscale eddies using a model and theory Nearshore sea ice responds to both +DA and −DAen_US
dc.publisherAGUen_US
dc.publisherWiley Periodicals, Inc.en_US
dc.subject.otherDipole Anomalyen_US
dc.subject.otherCoupled Ice‐Ocean Modelingen_US
dc.subject.otherLandfast Iceen_US
dc.subject.otherArctic Oceanen_US
dc.subject.otherBeaufort Seaen_US
dc.subject.otherChukchi Seaen_US
dc.titleA modeling study of coastal circulation and landfast ice in the nearshore Beaufort and Chukchi seas using CIOMen_US
dc.typeArticleen_US
dc.rights.robotsIndexNoFollowen_US
dc.subject.hlbsecondlevelAtmospheric and Oceanic Sciencesen_US
dc.subject.hlbsecondlevelGeological Sciencesen_US
dc.subject.hlbtoplevelScienceen_US
dc.description.peerreviewedPeer Revieweden_US
dc.description.bitstreamurlhttp://deepblue.lib.umich.edu/bitstream/2027.42/108088/1/jgrc20680.pdf
dc.identifier.doi10.1002/2013JC009258en_US
dc.identifier.sourceJournal of Geophysical Research: Oceansen_US
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dc.owningcollnameInterdisciplinary and Peer-Reviewed


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