The impact of extreme hydro-meteorological events on the transformation of mountain river channels (Polish Flysch Carpathians)

2017 ◽  
Vol 61 (1) ◽  
pp. 75-89 ◽  
Author(s):  
Małgorzata Kijowska-Strugała ◽  
Łukasz Wiejaczka ◽  
Eugeniusz Gil ◽  
Witold Bochenek ◽  
Krzysztof Kiszka
Author(s):  
Gražina ŽIBIENĖ ◽  
Alvydas ŽIBAS ◽  
Goda BLAŽAITYTĖ

The construction of dams in rivers negatively affects ecosystems because dams violate the continuity of rivers, transform the biological and physical structure of the river channels, and the most importantly – alter the hydrological regime. The impact on the hydrology of the river can occur through reducing or increasing flows, altering seasonality of flows, changing the frequency, duration and timing of flow events, etc. In order to determine the extent of the mentioned changes, The Indicators of Hydrologic Alteration (IHA) software was used in this paper. The results showed that after the construction of Angiriai dam, such changes occurred in IHA Parameters group as: the water conditions of April month decreased by 31 %; 1-day, 3-days, 7-days and 30-days maximum flow decreased; the date of minimum flow occurred 21 days later; duration of high and low pulses and the frequency of low pulses decreased, but the frequency of high pulses increased, etc. The analysis of the Environmental Flow Components showed, that the essential differences were recorded in groups of the small and large floods, when, after the establishment of the Šušvė Reservoir, the large floods no longer took place and the probability of frequency of the small floods didn’t exceed 1 time per year.


Geomorphology ◽  
2007 ◽  
Vol 83 (3-4) ◽  
pp. 197-198 ◽  
Author(s):  
Anne Chin ◽  
Ellen Wohl

Zoosymposia ◽  
2016 ◽  
Vol 10 (1) ◽  
pp. 384-392
Author(s):  
RIE SAITO ◽  
KAZUKI SEKINÉ ◽  
KOJI TOJO

The channels of almost all rivers in Japan have been fixed through the construction of artificial riverbanks to control flooding. In addition, to prevent flooding, maintenance works including the removal of gravel from the channels must be conducted regularly. As a result, the level of most riverbeds within river channels has been lowered, and riverbanks have become far steeper. These large changes to riverside environments have significantly altered the type of habitats available to plants, causing the level of vegetation growth on the riverside to increase. To improve such flood control methods, a new excavation project has commenced in the central area of the Chikuma-gawa River basin, under the auspices of the newly commissioned “Government Nature Restoration Project”. As part of this project, a large shallow environment approximately 1 km in length along the river’s course was newly created. We have attempted to evaluate the impact of this project and the subsequent environmental response, focusing on two dominant benthos, Stenopsyche marmorata and Isonychia japonica, particularly the dynamics of their genetic structure and diversity. Following the excavation of riverbanks and channels, the population density reached the same levels as at the control site, in a relatively short period of time. This is because the research site was limited to a small area within the large-scale river basin, with robust habitats located both upstream and downstream. The two target species in this study represent typical dominant species in the central basin of this river, and occur at high density. In other words, they could be transferred smoothly from the surrounding robust habitats, especially by the flow from upstream.


1996 ◽  
Vol 47 (6) ◽  
pp. 851 ◽  
Author(s):  
BJ Robson

Densities of benthic invertebrates were counted over several weeks before and after a small winter spate (15.5 times base flow) in two riffle types of contrasting architectural complexity in Mountain River, Tasmania. Complex benthic architecture reduced the impact of this spate on invertebrate densities over the short term (seven days). Longer-term recovery (several weeks) was unaffected by riffle architecture, with one of the riffles recovering much more slowly than the others. Refuges from small spates in Mountain River may exist in mid channel in complex boulder-cobble riffles. Within its temporal context, the effects of the spate on the study sites were of a similar magnitude to other unexplained population fluctuations.


Water ◽  
2021 ◽  
Vol 13 (21) ◽  
pp. 3059
Author(s):  
Zijian Ji ◽  
Yali Cui ◽  
Shouquan Zhang ◽  
Wan Chao ◽  
Jingli Shao

Ecological water supplement relies on river channels to introduce surface water, to make a reasonable supplement of groundwater, to repair the regional groundwater environment and urban river ecosystem. Evaluating the degree of groundwater restoration after ecological water supplement (by taking appropriate measures) is a critical problem that needs to be solved. Thus, based on the Yongding River ecological water supplement in 2019 and 2020, we analyzed the groundwater monitoring situates in the ecological water supplement region. We established an unstructured groundwater flow numerical model in the study area through the quadtree grids. The model was calibrated with the measured water level. The simulated results could accurately reflect the real groundwater dynamic characteristics, and it showed that the water level rise was concentrated in the 3–6 km range of the Yongding River after the ecological water supplement. In 2019, the calculated ecological water infiltration amount was 101.28 × 106 m3, the affected area was 265.19 km2, and the average groundwater level rise in the affected area was 2.10 m. In 2020, the calculated ecological water infiltration amount was 102.64 × 106 m3, the affected area was 506.88 km2, and the average groundwater level rise in the affected area was 1.25 m. While the ecological water supplement had a positive impact on groundwater level restoration, the groundwater level around the typical buildings within the study area, including Beijing West Railway Station and Beijing Daxing International Airport, would not be significantly affected.


2020 ◽  
Vol 4 (2) ◽  
pp. 100
Author(s):  
Dewi Kartika Sari ◽  
Rina Sri Widayati2 ◽  
Yulaikha Istiqomah ◽  
Saftirta Gatra Dewantara ◽  
Sandy Anwar Mursito ◽  
...  

Flood is a natural event caused by the overflowing of water out of the river channel because the volume of water exceeds the capacity of the available river channels. An area of overflow from a river is referred to as a flood-plain area. Kampung KB which is located in Pucang sawit Village, Jebres, Surakarta, is located along the side of the Bengawan Solo river, making this location prone to the impact of the overflowing of the Bengawan Solo river in this extreme weather. Therefore, disaster mitigation activities in the form of flood disaster management are needed for the people of that area. The prevalence of heavy rain in Indonesia is increasing, resulting in an increased risk of flooding. The result of this problem is the lack of public knowledge regarding how to deal with flood disasters that may arise. The solution is with disaster training in the form of activating the role of youth family development in the KB village. The target output expected from this health education is the increasing number of people who know the procedures for handling floods in disaster locations, as well as youth being able to play an active role in disaster activities. Information on the Activation of Action and the Role of Youth in Flood Disaster Management in Kampung KB Pucangsawit, Surakarta was held on the 21st October 2020, followed by five students, two accompanying lecturers and audiences. During the counseling, a demonstration of first aid was carried out in the case of floods and questions and answers to clarify the understanding of the residents. After counseling about first aid to flood victims, we also did scene designs or actions in the field and practiced what had been taught directly on the banks of the Bengawan Solo river.


2020 ◽  
Author(s):  
Akos Kalman ◽  
Timor Katz ◽  
Alysse Mathalon ◽  
Paul Hill ◽  
Beverly Goodman-Tchernov

<p>Worldwide, rivers deliver sediments and nutrients into the marine system, and this discharge is naturally variable due to fluctuations in precipitation, climate, and the shifting morphology of river channels. The sedimentological fingerprint of these variations from cores has been used to reconstruct past trends and conditions. Today, many coastal rivers have been heavily altered by dam construction, flood control, harbors, irrigation canals, and other human activities; thus also changing the volume, location, and arrival intervals of sediment discharge into the shallow marine shelf. Therefore, differentiating between changes linked to natural versus anthropogenic causes is key to interpreting and understanding the long-term effects of human activity and better defining the Anthropocene in the sedimentological record. In this study, offshore sediment profiles from the shallow shelf northern Red Sea were used to investigate how their recent sedimentological signatures compare to those of the past few thousand years, during which larger climatic shifts influenced sedimentation. The results found that the sedimentological trends were more homogenous laterally prior to the most recent half century, after which channelization of the alluvial plain directed the majority of flashflood runoff to a single outlet. This led to an artificial ‘drought-like’ signature in areas recently cut-off from incoming sediments. Data from sediment cores collected from offshore the Mediterranean coast of Israel inside the Nile littoral cell, an area that may have been impacted by the immense decrease in sediment discharge from the Nile river following the building of the High Aswan Dam showed similar trends. The impact that anthropogenic manipulation has on river sedimentary discharge, and its sedimentary signature will be discussed.</p>


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