On the Effect of Intermittent Nonstationarity of Long-Term Changes in the River Runoff

Based on the analysis of 162 longest (more than 100 years each) series of annual, maximal, and minimal runoff in rivers of different genetic types, the regularities of changes in the degree of stationarity/nonstationarity of the runoff changes are studied. It is shown that changes in the average ann...

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Published in:Water resources Vol. 45; no. Suppl 2; pp. 99 - 109
Main Authors: Solomonova, I. V., Yushkov, V. P., Dobrovolski, S. G.
Format: Journal Article
Language:English
Published: Moscow Pleiades Publishing 01-12-2018
Springer Nature B.V
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Abstract Based on the analysis of 162 longest (more than 100 years each) series of annual, maximal, and minimal runoff in rivers of different genetic types, the regularities of changes in the degree of stationarity/nonstationarity of the runoff changes are studied. It is shown that changes in the average annual and maximum runoff in the rivers of the “main” type—non-effluent, unregulated, as well as in the rivers of glacial feeding—throughout the period of observations generally correspond to the stationarity hypothesis. On the contrary, for a significant part of the runoff series of all types of effluents and regulated rivers, as well as the minimum flow of rivers of the main type, the alternation of segments of realizations of stationary and nonstationary processes with respect to mathematical expectation, is typical. To describe this effect, we propose the concept of “intermittent” nonstationarity. The nonstationarity parameters of the indicated type are compared with the nonstationarity parameters of the monotonous type.
AbstractList Based on the analysis of 162 longest (more than 100 years each) series of annual, maximal, and minimal runoff in rivers of different genetic types, the regularities of changes in the degree of stationarity/nonstationarity of the runoff changes are studied. It is shown that changes in the average annual and maximum runoff in the rivers of the “main” type—non-effluent, unregulated, as well as in the rivers of glacial feeding—throughout the period of observations generally correspond to the stationarity hypothesis. On the contrary, for a significant part of the runoff series of all types of effluents and regulated rivers, as well as the minimum flow of rivers of the main type, the alternation of segments of realizations of stationary and nonstationary processes with respect to mathematical expectation, is typical. To describe this effect, we propose the concept of “intermittent” nonstationarity. The nonstationarity parameters of the indicated type are compared with the nonstationarity parameters of the monotonous type.
Author Solomonova, I. V.
Yushkov, V. P.
Dobrovolski, S. G.
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  organization: Water Problems Institute, Russian Academy of Sciences
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10.1007/978-94-009-8514-8_28
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Keywords rivers
minimum runoff
mathematical expectation
annual runoff
maximal runoff
nonstationarity
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Snippet Based on the analysis of 162 longest (more than 100 years each) series of annual, maximal, and minimal runoff in rivers of different genetic types, the...
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StartPage 99
SubjectTerms Annual
Aquatic Pollution
Earth and Environmental Science
Earth Sciences
Effluents
Glacial periods
Hydrogeology
Hydrology/Water Resources
Long-term changes
Maximum runoff
Minimum flow
Parameters
Regulated rivers
River discharge
River flow
River regulations
River runoff
Rivers
Runoff
Waste Water Technology
Water Management
Water Pollution Control
Title On the Effect of Intermittent Nonstationarity of Long-Term Changes in the River Runoff
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