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EN
Freshwater reservoirs are limited and facing issues of over-exploitation, climate change effects and poor maintenance which have serious consequences for water quality. Developing countries face the challenge of collecting in situ information on ecological status and water quality of these reservoirs due to constraints of cost, time and infrastructure. In this study, a practical method of retrieval of two water clarity indicators, total suspended matter and secchi disk depth, using Sentinel-2 satellite data is adopted for preliminary assessment of water quality and trophic conditions in Khanpur reservoir, Pakistan. The study explores the synergy of utilizing two independent models, i.e., case 2 regional coast color analytical neural network model and semiempirical remote sensing algorithms to understand the spatiotemporal dynamics of water clarity patterns in the dammed reservoir, in the absence of ground measurements. The drinking water quality and trophic state of the reservoir water is determined based purely on satellite measurements. Out of the five months studied, the reservoir water has high turbidity and poor eutrophic status in three months. The results from both computational models are compared, which exhibit a high degree of statistical agreement. The study demonstrates the effective utilization of relevant analytical and semiempirical methods on satellite data to map water clarity indicators and understand their dynamics in both space and time. This solution is particularly useful for regions where routine ground sampling and observation of environmental variables are absent.
PL
Przedstawiono powody dla których budowa zbiorników wody słodkiej powoduje destrukcję delt i spowolnienie tworzenia fiordów. Podano przykłady problemów w utrzymaniu stanu posiadania lądu w warunkach załamania transportu osadu rzekami do morza.
EN
Some mechanisms of destructing deltas and speeding down creation of fiords by constructing large fresh water reservoirs have been described. The material has been illustrated by examples of problems with keeping the sea shore area the same as previously in the case of collapse of the sediment transportation by rivers to the sea.
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