Deleted Journal, Journal Year: 2025, Volume and Issue: 2(1), P. 2 - 2
Published: Jan. 22, 2025
Sediment transport in alluvial channels has a long history of intensive research. River ice could affect sediment and channel morphology through the impact various dynamic thermal processes. However, studies on under influence have been minimal until recent years. This phenomenon was partially due to complicated interactions between ice, flow, dynamics, which require good understanding river process, addition difficult field data collection conditions. paper reviews progress needs ice-related research morphology, including cover surface runs transport, effects frazil anchor bank stability with freeze-thaw effects.
Language: Английский