KFU. Card publication. Water Flow Changes In The Don River (European Russia) During 1891

KAZAN
FEDERAL UNIVERSITY

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WATER FLOW CHANGES IN THE DON RIVER (EUROPEAN RUSSIA) DURING 1891&NDASH;2019

Form of presentation

Articles in Russian journals and collections

Year of publication

2023

Язык

английский

Authors, employees of KFU

Gusarov Artem Viktorovich, author

Other authors

Borodin Oleg , author

Georgiadi Alexander , author

Milyukova Irina , author

Bibliographic description in the original language

Georgiadi A. G., Milyukova I. P., Borodin O. O., Gusarov A. V. (2023). Water Flow Changes In The Don River (European Russia) During 1891–2019 // Geography, Environment, Sustainability, 2(16), 6-17.

Annotation

The Don River near Razdorskaya Village had long phases (lasting 33–86 years) of increased/decreased naturalized annual and seasonal water flow, and their properties for 1891–2019 were identified. Long-term changes in the annual and snow-melt flood flow occurred in the opposite phase relative to changes in the winter and summer-autumn flow. Annual hydrographs in the phase of decreased flow were characterized by an increase in water discharge during the low-water seasons of the year, but a noticeable decrease in daily flood water discharge and maximum water discharge. The share of high-water years (years with a flow exceedance probability equal to or less than 25%) in the phase of increased flow is significantly higher than the share of low-water years (years with a flow exceedance probability equal to or more than 75%). And on the contrary. At the same time the cumulative share of low- and high-water years remains relatively stable. The total changes in the annual and seasonal flow, caused by both anthropogenic and climatic factors, throughout the entire period of modern global warming (since 1989) consisted in a decrease of the annual and snow-melt flood flow and an increase of flow values during low-water seasons.

Keywords

Hydrological change, long-term phase, high- and low-water year, global warming, anthropogenic factor, hydrograph transformation, cumulative deviation curve

The name of the journal

Geography, Environment, Sustainability

Please use this ID to quote from or refer to the card

https://repository.kpfu.ru/eng/?p_id=283915&p_lang=2

Resource files

File name	Size (MB)	Format
F_2023_Geography__Environment__Sustainability__2_16___6_17.pdf	2,45	pdf	show / download

Full metadata record

Field DC	Value	Language
dc.contributor.author	Gusarov Artem Viktorovich	ru_RU
dc.contributor.author	Borodin Oleg	ru_RU
dc.contributor.author	Georgiadi Alexander	ru_RU
dc.contributor.author	Milyukova Irina	ru_RU
dc.date.accessioned	2023-01-01T00:00:00Z	ru_RU
dc.date.available	2023-01-01T00:00:00Z	ru_RU
dc.date.issued	2023	ru_RU
dc.identifier.citation	Georgiadi A. G., Milyukova I. P., Borodin O. O., Gusarov A. V. (2023). Water Flow Changes In The Don River (European Russia) During 1891–2019 // Geography, Environment, Sustainability, 2(16), 6-17.	ru_RU
dc.identifier.uri	https://repository.kpfu.ru/eng/?p_id=283915&p_lang=2	ru_RU
dc.description.abstract	Geography, Environment, Sustainability	ru_RU
dc.description.abstract	The Don River near Razdorskaya Village had long phases (lasting 33–86 years) of increased/decreased naturalized annual and seasonal water flow, and their properties for 1891–2019 were identified. Long-term changes in the annual and snow-melt flood flow occurred in the opposite phase relative to changes in the winter and summer-autumn flow. Annual hydrographs in the phase of decreased flow were characterized by an increase in water discharge during the low-water seasons of the year, but a noticeable decrease in daily flood water discharge and maximum water discharge. The share of high-water years (years with a flow exceedance probability equal to or less than 25%) in the phase of increased flow is significantly higher than the share of low-water years (years with a flow exceedance probability equal to or more than 75%). And on the contrary. At the same time the cumulative share of low- and high-water years remains relatively stable. The total changes in the annual and seasonal flow, caused by both anthropogenic and climatic factors, throughout the entire period of modern global warming (since 1989) consisted in a decrease of the annual and snow-melt flood flow and an increase of flow values during low-water seasons.	ru_RU
dc.language.iso	ru	ru_RU
dc.subject	Hydrological change	ru_RU
dc.subject	long-term phase	ru_RU
dc.subject	high- and low-water year	ru_RU
dc.subject	global warming	ru_RU
dc.subject	anthropogenic factor	ru_RU
dc.subject	hydrograph transformation	ru_RU
dc.subject	cumulative deviation curve	ru_RU
dc.title	Water Flow Changes In The Don River (European Russia) During 1891–2019	ru_RU
dc.type	Articles in Russian journals and collections	ru_RU