Lake Level Fluctuation Impact on River Morphology Change

2022 ◽  
pp. 99-111
Author(s):  
Sisay Mengistie Eshetie ◽  
Mengistie Abate Meshesha
Keyword(s):  
Lake Level ◽  
River Morphology ◽  
Level Fluctuation ◽  
Morphology Change ◽  
Lake Level Fluctuation

scholarly journals Lake level fluctuation in Qehan Salt Lake during 29-8 ka, Inner Mongolia

2016 ◽  
Vol 28 (4) ◽  
pp. 909-916
Author(s):  
SIQIN Bilige ◽  
◽  
CHUN Xi ◽  
SONG Jie ◽  
BAI Xuemei
Keyword(s):  
Inner Mongolia ◽  
Lake Level ◽  
Salt Lake ◽  
Level Fluctuation ◽  
Lake Level Fluctuation

Photoautotrophic community changes in Lagunillo del Tejo (Spain) in response to lake level fluctuation: Two centuries of sedimentary pigment records

2009 ◽  
Vol 40 (3) ◽  
pp. 376-386 ◽  
Author(s):  
Lidia Romero-Viana ◽  
Brendan J. Keely ◽  
Antonio Camacho ◽  
Eduardo Vicente ◽  
M. Rosa Miracle
Keyword(s):  
Lake Level ◽  
Level Fluctuation ◽  
Lake Level Fluctuation ◽  
Community Changes

scholarly journals Hydrological regime of Adygine lake, Tien Shan, Kyrgyzstan

Geografie ◽  
2014 ◽  
Vol 119 (4) ◽  
pp. 320-341 ◽  
Author(s):  
Kristýna Falátková ◽  
Miroslav Šobr ◽  
Jan Kocum ◽  
Bohumír Janský
Keyword(s):  
Water Level ◽  
Lake Level ◽  
Hydrological Regime ◽  
Climatic Conditions ◽  
Tien Shan ◽  
Diurnal Fluctuation ◽  
Substantial Part ◽  
Level Fluctuation ◽  
Lake Level Fluctuation ◽  
Specific Factors

This article provides a detailed analysis of the hydrological regime of the Adygine glacial lake in Tien Shan, Kyrgyzstan, and of the specific factors which affect it. Glaciers of central Tien Shan are considered to be very sensitive indicators of climate change. The studied lake belongs to a system of relatively recently formed lakes situated near the front of the retreating glacier and is numbered amongst the potentially dangerous. The lake’s water level and its dependence on the development of climatic conditions in the area were monitored in detail in 2007–2012. A substantial part of this paper is the evaluation of the inflow and outflow balance of the lake’s basin. The results confirmed that the hydrological regime is glacial and exhibits its typical characteristics, such as a seasonal evolution of runoff delay or significant diurnal fluctuation of the lake’s water level. During the monitored period, no major changes in annual lake level fluctuation were recorded.

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