Water Discharge Change in the Rivers of the South of the Boreal Forest Zone of Eastern European Russia at the End of the Late Holocene and in the Anthropocene: The Vyatka River by Artyom V. Gusarov, Achim A. Beylich

“…A gradual increase in the share of the so-called normal annual WD and a decrease in the abnormal (including extreme) annual WD were noted from 1878–1929 to 1978–2018 in the predominantly northern half of the river basin. …”
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Hydrological and chemical water regime in the catchments of Bystra and Sucha Woda, in the Tatra National Park by Monika Sajdak, Joanna Siwek, Anna Bojarczuk, Mirosław Żelazny

“…Low values of mineralization, electrical conductivity and concentration of main ions were accompanied by increased flows during the summer and autumn. In all the waters subjected to testing, there was also a marked decrease in the value of these parameters during the spring thaw. …”
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Sediment Particle Size Distribution behind the Check Dams of the Lashkaran Watershed, Salmas, West Azerbaijan by Afsaneh Jafari, Habib Nazarnejad, Saeed Najafi, farrokh asadzadeh

“…The amount of clay is constant with increasing distance, with increased silt and decreased sand percentages. …”
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Climate change impacts on flood risks in the Abou Ali River Basin, Lebanon: A hydrological modeling approach by Fouadi AlZaatiti, Jalal Halwani, Mohamed R. Soliman

“…Flood modeling with the Rainfall-Runoff-Inundation (RRI) model reveals a dramatic increase in inundation extent, from 8.78 km² to 26.05 km², and a rise in maximum depth from 6.5 m to 14.7 m, with urban and agricultural areas at significant risk. …”
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Spatiotemporal Variation Characteristics and Influencing Factors of Water Transparency in the Pilot Zone of Yangtze River Delta by WANG Yu, ZHOU Wei-qi, BAI Meng-yu, SU Han, HU Wei

“…The negative correlation between TP and SD was particularly significant in lake water (R=-0.71), and the C3 component (humic-like substances) of dissolved organic matter (DOM) shared a common origin with TP (R=0.64), indicating that TP in lake water mainly originated from soil erosion and surface runoff input. …”
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