{"title":"jagodne湖(波兰东北部)冰况变化","authors":"M. Ptak, M. Sojka, B. Nowak","doi":"10.15576/asp.fc/2019.18.1.89","DOIUrl":null,"url":null,"abstract":"Aim of the study Indication of directions and pace of changes in ice regime of Jagodne Lake in 1975–2015. An analysis of predictability of ice phenomena in relation to stability and seasonality and an understanding mutual interactions between parameters describing ice regime of the lake. Material and methods Data from the Jagodne Małe water gauge station on Jagodne Lake, concerning: the dates of the beginning and the end of ice phenomena, the beginning and the end of ice cover, and the thickness of ice cover from 1975–2015. Average monthly air temperature from the IMGW-PIB synoptic station in Mikołajki. Statistical analysis based on trend analysis using the non-parametric Mann-Kendall test and the Colwell method. Results and conclusions The research has proven that Jagodne Lake shows some tendencies to change in ice regime over the last four decades. These trends should be identified with a successive shortening of ice season and a decrease of the thickness of ice cover. However, these changes in the case of the beginning and the end of ice phenomena (including ice cover) and the thickness of ice cover are not statistically significant. Only shortening of ice phenomena duration was observed and confirmed by the Mann-Kendall statistical test. The analyzed object reacts similarly to most of lakes, for which research on changes in icing was conducted. The observed increase of average temperatures in April had an influence on shortening of ice phenomena.","PeriodicalId":51904,"journal":{"name":"Acta Scientiarum Polonorum-Formatio Circumiectus","volume":"3 1","pages":""},"PeriodicalIF":0.4000,"publicationDate":"2019-03-30","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"5","resultStr":"{\"title\":\"CHANGES IN ICE REGIME OF JAGODNE LAKE (NORTH-EASTERN POLAND)\",\"authors\":\"M. Ptak, M. Sojka, B. Nowak\",\"doi\":\"10.15576/asp.fc/2019.18.1.89\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Aim of the study Indication of directions and pace of changes in ice regime of Jagodne Lake in 1975–2015. An analysis of predictability of ice phenomena in relation to stability and seasonality and an understanding mutual interactions between parameters describing ice regime of the lake. Material and methods Data from the Jagodne Małe water gauge station on Jagodne Lake, concerning: the dates of the beginning and the end of ice phenomena, the beginning and the end of ice cover, and the thickness of ice cover from 1975–2015. Average monthly air temperature from the IMGW-PIB synoptic station in Mikołajki. Statistical analysis based on trend analysis using the non-parametric Mann-Kendall test and the Colwell method. Results and conclusions The research has proven that Jagodne Lake shows some tendencies to change in ice regime over the last four decades. These trends should be identified with a successive shortening of ice season and a decrease of the thickness of ice cover. However, these changes in the case of the beginning and the end of ice phenomena (including ice cover) and the thickness of ice cover are not statistically significant. Only shortening of ice phenomena duration was observed and confirmed by the Mann-Kendall statistical test. The analyzed object reacts similarly to most of lakes, for which research on changes in icing was conducted. The observed increase of average temperatures in April had an influence on shortening of ice phenomena.\",\"PeriodicalId\":51904,\"journal\":{\"name\":\"Acta Scientiarum Polonorum-Formatio Circumiectus\",\"volume\":\"3 1\",\"pages\":\"\"},\"PeriodicalIF\":0.4000,\"publicationDate\":\"2019-03-30\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"5\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Acta Scientiarum Polonorum-Formatio Circumiectus\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.15576/asp.fc/2019.18.1.89\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"AGRONOMY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Acta Scientiarum Polonorum-Formatio Circumiectus","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.15576/asp.fc/2019.18.1.89","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"AGRONOMY","Score":null,"Total":0}
引用次数: 5
摘要
目的研究1975-2015年Jagodne湖冰况变化的方向和速度。分析与稳定性和季节性有关的冰现象的可预测性,并了解描述湖泊冰况的参数之间的相互作用。资料与方法取自Jagodne Małe Jagodne湖水位测量站,资料涉及:1975-2015年冰现象开始和结束的日期、冰盖开始和结束的日期、冰盖厚度。IMGW-PIB天气观测站在Mikołajki的月平均气温。统计分析基于趋势分析,采用非参数Mann-Kendall检验和Colwell方法。结果与结论研究表明,在过去40年里,Jagodne湖的冰态呈现出一定的变化趋势。这些趋势应与冰季的连续缩短和冰盖厚度的减少相一致。然而,这些变化在开始和结束冰现象(包括冰盖)和冰盖厚度的情况下没有统计学意义。仅观察到冰现象持续时间缩短,并经Mann-Kendall统计检验证实。分析对象的反应与大多数湖泊相似,为此进行了结冰变化的研究。观测到的4月平均气温的升高对冰现象的缩短有影响。
CHANGES IN ICE REGIME OF JAGODNE LAKE (NORTH-EASTERN POLAND)
Aim of the study Indication of directions and pace of changes in ice regime of Jagodne Lake in 1975–2015. An analysis of predictability of ice phenomena in relation to stability and seasonality and an understanding mutual interactions between parameters describing ice regime of the lake. Material and methods Data from the Jagodne Małe water gauge station on Jagodne Lake, concerning: the dates of the beginning and the end of ice phenomena, the beginning and the end of ice cover, and the thickness of ice cover from 1975–2015. Average monthly air temperature from the IMGW-PIB synoptic station in Mikołajki. Statistical analysis based on trend analysis using the non-parametric Mann-Kendall test and the Colwell method. Results and conclusions The research has proven that Jagodne Lake shows some tendencies to change in ice regime over the last four decades. These trends should be identified with a successive shortening of ice season and a decrease of the thickness of ice cover. However, these changes in the case of the beginning and the end of ice phenomena (including ice cover) and the thickness of ice cover are not statistically significant. Only shortening of ice phenomena duration was observed and confirmed by the Mann-Kendall statistical test. The analyzed object reacts similarly to most of lakes, for which research on changes in icing was conducted. The observed increase of average temperatures in April had an influence on shortening of ice phenomena.