THE INFLUENCE OF CLIMATIC CHANGES ON THE HYDROLOGICAL REGIME OF NORTHERN RIVERS OF KRASNOYARSK KRAI

2021 ◽  
Vol 42 (3) ◽  
pp. 113-121
Author(s):  
T.A. Burenina ◽  
D.A. Prysov ◽  
A.V. Musokhranova
Author(s):  
Agnieszka Rutkowska ◽  
Silvia Kohnová ◽  
Kazimierz Banasik ◽  
Jan Szolgay

Abstract Flow characteristics of intermittent rivers in Slovakia. Intermittent rivers are rivers that cease to fl ow, i.e. temporary, ephemeral, seasonal, and episodic rivers. Analysis of hydrological regime of such rivers is pivotal in assessment of water resources because changes in fl ow characteristics of such rivers may affect neighboring catchments or the entire region through changes in water supply reservoirs such as lakes, wetlands and mosses. Recently, an increasing number of intermittent rivers and ephemeral streams (IRES) and an elongation of the zero- -fl ow events has been observed in Europe due to climatic changes and anthropogenic influence. Intermittent rives in Slovakia were studied in the paper using statistical methods. The characteristics of the zero-fl ow period, of duration of the longest annual zero-fl ow event and of timing of such events were derived. The circular statistics were helpful in recognition of the dates of occurrence of such events. The comparative analysis between catchments was performed. The variability in precipitation and evapotranspiration and the increasing temperature were identified as the possible drivers of the fl ow intermittence in these catchments. The research was performed within the COST Action SMIRES (Science and Management of Intermittent Rivers & Ephemeral Streams).


Author(s):  
Cristinel Costandache ◽  
Lucian Dinca ◽  
Laurentiu Popovici ◽  
Ciprian Tudor

"Climatic changes displayed through extremes (thermic or hydric) correlated with uncontrolled anthropic interventions exercised over time on land usages are the main factors that emphasize ecological and hydric disequilibrium from the South, East part of Romania. Specific of our country, the torrential precipitation regime generates rapid floods in mountain and hill areas. Torrential and land degrading processes occur on slopes and on the main hydrographic network as a result of torrential runoffs. Their consequences extend on a larger area than the one on which they occur. This happens especially as a consequence of perturbing the hydrological regime of water courses, generating floods in downstream areas or the cogging of accumulation lakes in periods with rain redundancies. Forest protection cultures (forest vegetation) installed on degraded or overexploited agricultural lands from the hill and mountain areas represent the most efficient solution for attenuating the negative effects of climatic changes. This happens by steadily re-establishing the hydrological equilibrium, together with creating an ecological equilibrium that has positive effects on the soil and waters. This paper emphasized the results of investigations realized in 2017 concerning the characteristics of forest protection cultures created on strongly and excessively degraded lands, followed by their hydrological and anti-erosion effects in the context of extreme meteorological phenomenon. As such, the runoff coefficient had values lower than 6.5% (from the total volume of precipitations in 24 hours), while the specific erosion was under 0.24 t/ha/an. The maximum charge of alluvium (erosion) produced by rain is of over 40 mm; their frequency and intensity has increased lately."


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