One-Dimensional Sea Ice-Ocean Model Applied to SHEBA Experiment in 1997-1998 Winter

A one-dimensional sea ice-ocean model with its application in the Arctic Ocean is presented. The model includes a mixed-layer ocean model, a multi-layer snow/ice model, and the interfaces among atmosphere, snow/sea ice, and sea water. The observational data from the measurements at the ice station o...

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Main Author: Wen-Yih Sun Jiun-Dar Chern
Format: Article
Language:English
Published: Springer 2010-01-01
Series:Terrestrial, Atmospheric and Oceanic Sciences
Subjects:
Online Access: http://tao.cgu.org.tw/images/attachments/v211p000.pdf
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author Wen-Yih Sun Jiun-Dar Chern
author_facet Wen-Yih Sun Jiun-Dar Chern
author_sort Wen-Yih Sun Jiun-Dar Chern
collection DOAJ
description A one-dimensional sea ice-ocean model with its application in the Arctic Ocean is presented. The model includes a mixed-layer ocean model, a multi-layer snow/ice model, and the interfaces among atmosphere, snow/sea ice, and sea water. The observational data from the measurements at the ice station of the Surface Heat Budget of the Arctic Ocean (SHEBA) field experiment between November 1997 and January 1998 were used to drive and validate the model. The energy budget of the stand-alone simulations shows that the longwave radiative cooling is mainly balanced by the heat released of freezing at the bottom of the sea-ice. The results also show that the effect of ventilation and blowing snow are required to reproduce the detailed observed surface temperature, thickness of the sea ice, sensible heat flux and upward longwave radiation.
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spelling doaj.art-fb42cbf6938c45b88f297e3a93dd3c3f2022-12-22T01:57:20ZengSpringerTerrestrial, Atmospheric and Oceanic Sciences1017-08392311-76802010-01-0121100010.3319/TAO.2009.03.20.01(IWNOP)885One-Dimensional Sea Ice-Ocean Model Applied to SHEBA Experiment in 1997-1998 WinterWen-Yih Sun Jiun-Dar ChernA one-dimensional sea ice-ocean model with its application in the Arctic Ocean is presented. The model includes a mixed-layer ocean model, a multi-layer snow/ice model, and the interfaces among atmosphere, snow/sea ice, and sea water. The observational data from the measurements at the ice station of the Surface Heat Budget of the Arctic Ocean (SHEBA) field experiment between November 1997 and January 1998 were used to drive and validate the model. The energy budget of the stand-alone simulations shows that the longwave radiative cooling is mainly balanced by the heat released of freezing at the bottom of the sea-ice. The results also show that the effect of ventilation and blowing snow are required to reproduce the detailed observed surface temperature, thickness of the sea ice, sensible heat flux and upward longwave radiation. http://tao.cgu.org.tw/images/attachments/v211p000.pdf SHEBAModelEnergy budget
spellingShingle Wen-Yih Sun Jiun-Dar Chern
One-Dimensional Sea Ice-Ocean Model Applied to SHEBA Experiment in 1997-1998 Winter
Terrestrial, Atmospheric and Oceanic Sciences
SHEBA
Model
Energy budget
title One-Dimensional Sea Ice-Ocean Model Applied to SHEBA Experiment in 1997-1998 Winter
title_full One-Dimensional Sea Ice-Ocean Model Applied to SHEBA Experiment in 1997-1998 Winter
title_fullStr One-Dimensional Sea Ice-Ocean Model Applied to SHEBA Experiment in 1997-1998 Winter
title_full_unstemmed One-Dimensional Sea Ice-Ocean Model Applied to SHEBA Experiment in 1997-1998 Winter
title_short One-Dimensional Sea Ice-Ocean Model Applied to SHEBA Experiment in 1997-1998 Winter
title_sort one dimensional sea ice ocean model applied to sheba experiment in 1997 1998 winter
topic SHEBA
Model
Energy budget
url http://tao.cgu.org.tw/images/attachments/v211p000.pdf
work_keys_str_mv AT wenyihsunjiundarchern onedimensionalseaiceoceanmodelappliedtoshebaexperimentin19971998winter