巴尔喀什湖乌日纳尔海峡水流特征

S. Alimkulov, A. Myrzakhmetov, A.A. Tursunova, A. Tairov, K. Bolatov
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引用次数: 0

摘要

巴尔喀什湖的生态系统是一个独特的自然综合体,在一个相对较小的领土上有5个气候带,从Tanirtau的冰川开始,到巴尔喀什地区的炎热沙漠结束。本研究考察了水位的动态变化问题以及与之相关的湖泊面积和水量。巴尔喀什湖的水位是反映整个流域生态系统状况的主要指标之一。在流量调节之前,湖泊水位周期性变化,主要在341和342 m BS之间,最近由于来水高含水期,湖泊水位在这些标志之间。这个湖的独特之处在于,它被一条狭窄的海峡分成两部分,两部分的水成分不同——西部几乎是新鲜的,东部是微咸的。2022年秋天在乌兹纳尔海峡进行了实地研究,文章介绍了这次考察的结果。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Characteristics of the water flow in the Uzynaral strait of lake Balkash
The ecological ecosystem of Lake Balkash is a unique natural complex, where 5 climatic zones are located on a relatively small territory, starting from the glaciers of Tanirtau and ending with the hot deserts of the Balkash region. This study examines the issues of dynamic changes in the water level and the associated area and volume of water in the lake. The level of Lake Balkash is one of the main indicators of the state of the entire ecosystem of the basin. Prior to the regulation of the flow, the lake level cyclically changed, mainly between the marks 341 and 342 m BS, recently due to the period of high-water content of the incoming river flow, the lake level is between these marks. The uniqueness of the lake is that it is divided by a narrow strait into two parts with different water compositions – in the western part it is almost fresh, and in the eastern part it is brackish. Field studies were conducted in the Uzynaral Strait in the autumn of 2022, the article presents the results of this expedition.
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