Hydrochemical features of boggy river sources and lakes in central European Russia

Akmet’eva, N. P.; Simakina, Ya. I.; Belyaev, A. Yu.; Krichevets, G. N.; Solov’ev, A. I.

doi:10.1134/s0097807816010024

Cited by 2 publications

(1 citation statement)

References 4 publications

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“…For Western Dvina, the decrease in maximum streamflow was observed earlier after 1971. We speculate that this early break point onset could be related to a multiannual drainage experiment in the upstream part of this river in Russia [52,53]. The minimal summer runoff increased for the Dnepr River, while for the two other rivers, its changes were insignificant.…”

Section: Case Study: Hydrological Extremes At Three Stations Across B...mentioning

confidence: 97%

Changes of Hydrological Extremes in the Center of Eastern Europe and Their Plausible Causes

Danilovich,

Loginov,

Groisman

2023

Water

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Regional studies of precipitation changes over Europe show that its eastern part is characterized by small changes in annual precipitation and insignificant aridity trends compared to central and southern Europe. However, a frequency analysis over the past 30 years showed statistically significant increasing dryness trends in eastern Europe and an increase in the occurrence of extremely high rainfall as well as prolonged no-rain intervals during the warm season. The largest increase in aridity was observed in the western and central parts of Belarus. During 1990–2020, the frequency of dry periods doubled in all river basins along the Black, Caspian, and Baltic Sea water divide areas of eastern Europe. From 1970 to 1990, there were high streamflow rates during the winter low-flow season. Consequently, over the past 50 years, in spring, we observed here a continued decrease in maximal discharges across all river basins. In summer, we detected a statistically significant increase in the number of days with anticyclonic weather over eastern Europe, a decrease in rainfall duration by 15–20%, an increase in daily precipitation maxima by 20–30%, and an increase in the number of days with a low relative humidity by 1–4 days per decade.

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Section: Case Study: Hydrological Extremes At Three Stations Across B...mentioning

confidence: 97%

Changes of Hydrological Extremes in the Center of Eastern Europe and Their Plausible Causes

Danilovich,

Loginov,

Groisman

2023

Water

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The Chemical Composition of the Water of the Fresh Lake Beloe (Np «meshera») According to the Method of Atomic Emission Spectrometry With Inductively Coupled Plasma

Попова

Mikhailova

Моржухина

et al. 2019

Vestnik Mezhdunarodnogo Universiteta Prirody, Obshhestva i Chel

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The paper presents new data on the chemical composition of the water of Lake Beloye (FSFI «NP «Meshera», Ryazan region) for 2018, which supplement those obtained earlier – in 2013, 2014 and 2016. The choice of the method of analysis is justified – AES (OES) -ISP, as express and highly sensitive. The obtained data characterize the elemental composition of the Lake water, and are also ecological information for the state of the natural object. According to the available observations, it can be said that at present the waters of Lake Beloe are completely defined as «clean» by quality.

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Hydrochemical features of boggy river sources and lakes in central European Russia

Cited by 2 publications

References 4 publications

Changes of Hydrological Extremes in the Center of Eastern Europe and Their Plausible Causes

Changes of Hydrological Extremes in the Center of Eastern Europe and Their Plausible Causes

The Chemical Composition of the Water of the Fresh Lake Beloe (Np «meshera») According to the Method of Atomic Emission Spectrometry With Inductively Coupled Plasma

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