Abstract
The effect of different factors on the duration of spring ice jams and the flood water level in the Siberian rivers is considered. Observational data on the frequency of ice jams of different probabilities within some reaches of the Yenisei River are presented.
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REFERENCES
Gidrologicheskie ezhegodniki (1941–1991 gg.) (Hydrological Year-Book (1941–1991 Years)), Krasnoyarsk, 1992, vol. 7.
Lyutov, A.V. and Turutin, B.F., Trudy V konf. “Dinamika i termika rek, vodokhranilishch i pribrezhnoi zony morei” (Proc. V Conf. “Dynamics and Thermal Conditions of Rivers, Reservoirs, and Seashore Zones”), Moscow: Inst. Vodn.Probl. Ross. Akad. Nauk, 1999, p. 142.
Turutin, B.F. and Matyushenko, A.I., Trudy V konf. “Dinamika i termika rek, vodokhranilishch i pribrezhnoi zony morei” (Proc. V Conf. “Dynamics amd Thermal Conditions of Rivers, Reservoirs, and Seashore Zones”), Moscow: Inst. Vodn. Probl. Ross. Akad. Nauk, 1999, p. 155.
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Turutin, B.F., Matyushenko, A.I. Formation of Frazil Ice and Ice Jams on the Rivers of the Yenisei River Basin. Water Resources 28, 224–228 (2001). https://doi.org/10.1023/A:1010300305600
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DOI: https://doi.org/10.1023/A:1010300305600