An operational model for Lithuania's coastal zone

Pub Date : 2013-06-20 DOI:10.5200/BALTICA.2013.26.12
P. Zemlys, I. Dailidienė, Jevgenijus Zaboras
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引用次数: 3

Abstract

The results of testing (hindcast) an operational hydrodynamic model HIROMB_LT for Lithuania's coastal zone are presented and analysed in this paper. A model is developed using the program code of an opera- tional hydrodynamic model of the Baltic Sea HIROMB (Swedish Meteorological and Hydrological Institute). The model grid (horizontal resolution 300m, vertical resolution 25 layers) covers the Baltic Sea coastal area until the Gdansk Bay in the West and Latvian border in the North and the Curonian Lagoon. The model simu- lated water levels, surface water temperature surface water salinity and ice cover variables were tested against measurements for the year 2009. The model shows satisfactory performance on water level and temperature and rather weak performance on salinity at stations where good reproduction of the mixing of fresh and saline water is critical (Juodkrantė and Klaipėda seaside stations). The model performance on ice thickness is still problematic because of too coarse spatial resolution of westerly winds. Despite of these shortcomings, the model can be used for operational forecasts already; however, data assimilation may be necessary for salinity and ice thickness.
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立陶宛沿海地区的运作模式
本文介绍了立陶宛海岸带运行水动力模型HIROMB_LT的测试(后播)结果,并进行了分析。利用瑞典气象水文研究所(HIROMB)波罗的海运行水动力模型的程序代码,建立了一个模型。模型网格(水平分辨率300米,垂直分辨率25层)覆盖了波罗的海沿岸地区,直到西部的格但斯克湾和北部的拉脱维亚边界以及库尔尼泻湖。该模型模拟了水位、地表水温度、地表水盐度和冰盖变量,并根据2009年的测量结果进行了测试。该模型在水位和温度方面的表现令人满意,而在淡水和咸水混合的良好再现至关重要的站点(juodkrantnik和Klaipėda海滨站点),其盐度方面的表现相当弱。由于西风的空间分辨率过于粗糙,模型在冰厚上的表现仍然存在问题。尽管存在这些缺点,该模型已经可以用于业务预测;然而,对于盐度和冰厚,可能需要同化数据。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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