Dynamics of Reed Vegetation Area in the Sivash Gulf (Sea of Azov) according to Satellite Data

E. Eremina, E. Sovga, S. Stanichny, V. Mikhailov
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Abstract

The paper analyzes peculiarities of formation of the Sivash Gulf coastal area, which manifest at the moment as a combination of abrasive and accumulation processes. The paper gives more details about vegetation coasts (a special coast type related to a specific sedimentation type) defined by reed vegetation development, which is prevalent near clough entries in apexes of ingressive gulfs and “secondary” lagoons. Using data of digital multizonal satellites Landsat 5 and 7 as well as Sentinel-2 L1C, the paper considers dynamics (2014–2020) of reed coast areas in the East and South Sivash after damming the North Crimean Canal in 2014 as a consequence thereof and related increase of salinity in the gulf water area. For comparison, the paper analyzes dynamics of vegetation coast spread as a result of the canal functioning, also reed vegetation area growth up to the 1990s is considered. The ecological role of reed vegetation as a distinctive biotope is shown. It is emphasized that damming of the North Crimean Canal not only led to changes of the gulf salinity regime but also affected its entire ecosystem, including the reed coast, formation of which was promoted by increase of fresh water volume in the gulf water balance. Impact of the North Crimean Canal and its damming in 2014 on change of the reed vegetation area in the East and South Sivash was estimated using satellite data. At the studied zone of Prisivashie, flood plain areas shrank most of all in the Knyazevsky and Balaganovsky Gulfs as well as near the Alekseevskaya extinct lake in the South Sivash. In the Rogachinsky Gulf, despite discontinued drainage, influence of waste waters remains significant. Therefore, reed communities have preserved here best. It is shown that for some water areas shrinkage of areas populated by reed vegetation can considerably slow down provided there are local p ermanent or periodic fresh water sources, e. g. waste waters coming from settlements.
基于卫星数据的亚速海西瓦什湾芦苇植被面积动态
本文分析了西瓦什湾沿岸地区形成的特殊性,目前表现为磨蚀作用和堆积作用的结合。本文详细介绍了芦苇植被发育所定义的植被海岸(一种与特定沉积类型相关的特殊海岸类型),这种海岸普遍存在于入侵海湾和“次生”泻湖顶端的峡谷入口附近。利用数字多向卫星Landsat 5和7以及Sentinel-2 L1C的数据,本文考虑了2014年北克里米亚运河筑坝后东、南西瓦什芦苇海岸地区的动态(2014 - 2020年),以及海湾水域盐度的相关增加。为了进行比较,本文分析了运河作用下植被海岸扩展的动态,并考虑了20世纪90年代以来芦苇植被面积的增长情况。阐述了芦苇植被作为一种独特的生物群落的生态作用。强调北克里米亚运河的筑坝不仅导致了海湾盐度状况的变化,而且影响了包括芦苇海岸在内的整个生态系统,芦苇海岸的形成是由于海湾水平衡中淡水量的增加而促进的。利用卫星数据估算了2014年北克里米亚运河及其筑坝对西瓦什东部和南部芦苇植被面积变化的影响。在priivashie的研究区,洪水平原面积缩小的最主要是在Knyazevsky和Balaganovsky海湾,以及南西瓦什的Alekseevskaya灭绝湖附近。在罗金斯基湾,尽管已停止排水,但废水的影响仍然很大。因此,芦苇群落在这里保存得最好。研究表明,在某些水域,只要当地有永久或周期性的淡水来源,例如来自住区的废水,芦苇植被居住区的萎缩速度就会大大减缓。
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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