Leads as natural fairways in the Gulf of Finland

O. Parn, J. Haapala, L. Sipelgas
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引用次数: 1

Abstract

The monitoring and prediction of sea ice conditions are vital for safe and economical winter navigation in the Gulf of Finland (GoF), where ice conditions are very variable and dynamic. Flaw leads and ice ridges are common features in the GoF. In this study the occurrence frequency of the leads and ridges during 1971–2009 is analyzed. For the historical period, the ice charts of the Estonian Meteorological and Hydrological Institute (EMHI) were used for determining their occurrence and location in the Gulf of Finland. A case study was performed for a severe winter in 2002/2003. MODIS satellite imagery was used in addition to ice charts for determining the location of the leads in the Gulf of Finland. Also, the HELMI ice model was used to examine ice characteristics during the winter of 2002/2003 and the relationship between deformed ice growth rates and the speed and direction of wind. The results of the analysis of historical data show that on the average the leads are most common in the Estonian coastal region where their occurrence is typically 10–30%. During severe winters, leads occur quite often also in the Finnish coastal region, but the ridges are more common in the Estonian coast.
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芬兰湾的天然航道
在芬兰湾,海冰状况的监测和预测对于安全和经济的冬季航行至关重要,因为芬兰湾的海冰状况非常多变和动态。缺陷导线和冰脊是GoF的常见特征。本研究分析了1971-2009年间引线和脊的发生频率。在历史时期,爱沙尼亚气象和水文研究所(EMHI)的冰图被用来确定它们在芬兰湾的发生和位置。对2002/2003年的一个严冬进行了个案研究。除了冰图之外,还使用了MODIS卫星图像来确定芬兰湾铅的位置。此外,利用HELMI冰模型研究了2002/2003年冬季的冰特征以及变形冰生长速率与风速和风向之间的关系。对历史数据的分析结果表明,平均而言,这些线索在爱沙尼亚沿海地区最为常见,其发生率通常为10-30%。在严冬,芬兰沿海地区也经常出现铅,但山脊在爱沙尼亚海岸更常见。
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