Raduńskie Górne湖和Ostrzyckie湖冰况的统计关系/一致性

Q3 Environmental Science Limnological Review Pub Date : 2018-09-01 DOI:10.2478/limre-2018-0011
J. Barańczuk
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引用次数: 4

摘要

摘要本文试图通过对位于卡舒边湖区中部的两个基准湖的相关分析,对有关冰现象的几个选定参数进行分析和比较。这些湖泊是:Raduńskie Górne,一个较大的湖泊(387.2 hm2)和Ostrzyckie,一个较小的湖泊,面积为308.0 hm2。分析涵盖1971-2010年期间的测量序列。用于分析Raduńskie Górne湖冰现象数据的材料来自Borucino的Gdańsk大学湖沼站,而Ostrzyckie湖的数据来自气象和水管理研究所。分析了冰况的下列参数之间的关系:冰现象的持续时间、冰覆盖的持续时间、冰覆盖的平均厚度和最大厚度。分析和数据比较表明,所分析的参数之间存在很强和非常强的关系,这使得开发适当的统计模型成为可能。因此,如果缺乏其中一个湖泊的冰覆盖模式的数据,则可以使用详细的经验模型和另一个湖泊的数据来重建它们。
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The statistical relation/coherence between ice-regimes of Lake Raduńskie Górne and Lake Ostrzyckie
Abstract This article is an attempt to analyse and compare several selected parameters regarding ice phenomena using the correlation analysis of two lakes, which are benchmark lakes located in the central part of the Kashubian Lakeland. These lakes are: Raduńskie Górne, a larger one (387.2 hm2) and Ostrzyckie, a smaller one covering an area of 308.0 hm2. The analysis covered measurement sequences for the period 1971–2010. The material for analysis regarding data on ice phenomena on Lake Raduńskie Górne was obtained from the University of Gdańsk Limnological Station in Borucino while the data for Lake Ostrzyckie was obtained from the Institute of Meteorology and Water Management (IMGW). Relations between the following parameters of the ice regime were analysed: duration of the ice phenomena, duration of the ice cover, average and maximum thickness of the ice cover. The analysis and data comparisons have revealed that there are strong and very strong relations between the analysed parameters, which made it possible to develop proper statistical models. Hence, should there be a lack of data on the ice-cover pattern for one of these lakes it is possible to recreate them using the elaborated empirical models and data for the other.
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来源期刊
Limnological Review
Limnological Review Environmental Science-Ecology
CiteScore
1.60
自引率
0.00%
发文量
0
审稿时长
16 weeks
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