Assessment of Minimum Water Level in Lakes and Reservoirs Based on Their Morphological and Hydrological Features

被引:4
|
作者
Doulgeris, Charalampos [1 ]
Koukouli, Panagiota [2 ]
Georgiou, Pantazis [2 ]
Dalampakis, Paschalis [1 ]
Karpouzos, Dimitrios [2 ]
机构
[1] Hellen Agr Org DEMETER, Soil & Water Resources Inst, Sindos 57400, Central Macedon, Greece
[2] Aristotle Univ Thessaloniki, Sch Agr, Dept Hydraul Soil Sci & Agr Engn, Thessaloniki 54124, Central Macedon, Greece
关键词
minimum lake level; hydromorphological analysis; Lake Vegoritida catchment; Greek lakes; AQUATIC MACROPHYTES; REQUIREMENTS;
D O I
10.3390/hydrology7040083
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
The sustainable management of lakes and reservoirs requires the determination of their minimum environmental water level. Even though the assessment of minimum water level depends on a number of biotic and abiotic factors of the lake ecosystem, in many cases these factors are not entirely known and, furthermore, their evaluation is usually a challenging and laborious task. On the other hand, the lakes/reservoirs may comprise an important water resource to meet the requirements arising from economic activities. In this paper, the morphological and hydrological features of four lakes of northern Greece were analysed in order to assess their minimum environmental water level. The hydromorphological analysis was based on the relationship of the lake surface area and volume with water level as well as the water inflow from the lake's hydrological catchment area, considering as the lake's critical volume storage, the annual water volume flowing into a lake from its hydrological catchment area with a probability of exceedance 50% of a long time series of hydrological years. By combining morphological and hydrological features, the proposed methodology aimed to extend the analysis based solely on morphological features, and assess more comprehensively the minimum environmental water level in the four lakes, ensuring also the rising from the minimum level to the maximum (overflow) level for most of the hydrological years.
引用
收藏
页码:1 / 14
页数:13
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