Landscape‐hydrological phenomenon of the formation of floating islands on Lake Chebarkul (Davletovo) in the Ural River basin, Russia

V. M. Pavleichik, Z. Sivohip
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Abstract

Aim. To record factually the development of floating islands on Lake Chebarkul (Davletovo) as a landscape‐hydrological phenomenon in the Ural River basin and in the Southern Trans‐Urals, to determine the mechanisms of formation and to identify the specific features of their morphostructure, intra‐annual movements and long‐term dynamics.Materials and Methods. Based on images of high (2003–2020) and medium (1972–2020) spatial resolution, an analysis was made of qualitative and quantitative indicators reflecting the long‐term and intra‐ annual dynamics of the state of floating islands (mats) and coastal thickets of macrophytes («splavina» or «labza» in Russian).Results. It was established that the main source of material for the islands were the coastal thickets of macrophytes at the site of the confluence of watercourses into the lake (Yangelka River and Mogak Crrek), which periodically (during periods of extreme spring floods) lose contact with coastal shallow waters and are carried into the lake. The high variability of the states and the dynamism of the displacement of the islands, as well as the tendency to reduce the number and area of the islands and coastal thickets of macrophytes, caused, among other factors, by the consequences of the anomalous summer flood of 2013, were revealed. Being in an unfixed state, floating islands drift along the water area of the lake for considerable distances, reaching 10–15 km or more during the ice‐ free period of the year. The main driving force is the wind, which causes prevailing alongshore displacements of the islands: as a result of collisions, they are reduced in size and acquire a rounded shape in plan.Conclusion. Throughout the historical period, floating islands around the world have been perceived as a landscape phenomenon that deserves protection and rational use. Lake Chebarkul with floating islands is of undoubted interest as an object of geographical, hydrological, ecological and biological research.
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俄罗斯乌拉尔河流域切巴库尔湖(达夫列托沃)浮岛形成的景观水文现象
的目标。真实记录切巴库尔湖(达夫列托沃)上漂浮岛屿的发展,作为乌拉尔河流域和南跨乌拉尔地区的一种景观水文现象,确定其形成机制,并确定其形态结构、年内运动和长期动态的具体特征。材料与方法。基于高(2003-2020年)和中(1972-2020年)空间分辨率影像,对反映浮岛(垫)和沿海大型植物灌丛(俄语为“splavina”或“labza”)长期和年内动态的定性和定量指标进行了分析。已经确定,岛屿的主要材料来源是水道入湖(Yangelka河和Mogak creek)汇合处的沿海大型植物灌丛,这些灌丛周期性地(在春季极端洪水期间)与沿海浅水失去联系,并被带到湖中。揭示了2013年夏季异常洪水造成的岛屿状态的高变异性和位移的动态性,以及岛屿和沿海大型植物灌丛数量和面积减少的趋势。由于处于不固定状态,浮岛沿着湖面漂移相当远的距离,在一年的无冰期可达10-15公里或更远。主要的驱动力是风,它引起了岛屿沿海岸的普遍位移:由于碰撞,它们的尺寸减小,并在平面上获得圆形。纵观历史,世界各地的浮岛一直被视为一种值得保护和合理利用的景观现象。作为地理、水文、生态和生物研究的对象,切巴库尔湖和浮动岛屿无疑是一个令人感兴趣的对象。
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来源期刊
CiteScore
0.80
自引率
50.00%
发文量
73
审稿时长
8 weeks
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