Abstract
The prevailing types of the atmospheric stratification over the snow-ice cover at the top of Taganrog Bay for eleven winter seasons of 2007/2008–2017/2018 have been determined using the numerical experiments on reproducing the seasonal variations in the sea ice thickness. Series of calculations both with the constant transfer coefficients and with the coefficients obtained taking into account the surface stratification of the atmosphere have been carried out. The model results of both series have been compared with each other and with in situ measurements.
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Translated from Meteorologiya i Gidrologiya, 2024, No. 3, pp. 31-41. https://doi.org/10.52002/0130-2906-2024-3-31-41.
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Zav’yalov, D.D., Solomakha, T.A. Parameterizing Heat and Moisture Exchange in a Regional Thermodynamic Model of Sea Ice. Russ. Meteorol. Hydrol. 49, 203–211 (2024). https://doi.org/10.3103/S1068373924030038
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DOI: https://doi.org/10.3103/S1068373924030038