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dc.contributor.authorHuiding Wu
dc.contributor.authorShan Bai
dc.contributor.authorHai Li
dc.contributor.authorZhanhai Zhang
dc.contributor.authorZhilian Wang
dc.contributor.authorKeguang Wang
dc.contributor.authorQinzheng Liu
dc.date.accessioned2017-05-08T21:14:02Z
dc.date.available2017-05-08T21:14:02Z
dc.date.copyrightJune 2000
dc.date.issued2000
dc.identifier.other%28asce%290887-381x%282000%2914%3A2%2868%29.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl/handle/yetl/43690
dc.description.abstractThe sea ice model for simulating ice growth, decay, and drift in the Bohai Sea was developed based on the ice conditions in the Sea and on existing sea ice models. Both dynamic and thermodynamic processes of sea ice are incorporated into the model. The viscous-plastic constitutive law is applied to estimate the internal ice stress. The thermodynamic growth rates are determined from the effect of thermodynamic forcing from atmosphere and ocean, which are parameterized according to the heat exchanges at the air/ice, air/water, and ice/water interfaces. This model is coupled with an oceanic model and is linked to a numerical weather prediction model for forecasting ice conditions in the Bohai Sea and the northern Yellow Sea. Statistical verification was used to make an objective assessment of the model. This paper summarizes the development of the sea ice model and its application in Bohai Sea ice forecast.
dc.publisherAmerican Society of Civil Engineers
dc.titleModeling and Forecasting of Bohai Sea Ice
dc.typeJournal Paper
dc.journal.volume14
dc.journal.issue2
dc.journal.titleJournal of Cold Regions Engineering
dc.identifier.doi10.1061/(ASCE)0887-381X(2000)14:2(68)
dc.treeJournal of Cold Regions Engineering:;2000:;Volume ( 014 ):;issue: 002
dc.contenttypeFulltext


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