Sites with drainage areas ranging from 88 to 12,200 km2 were monitored on five streams in northern Alaska during the breakup in 1976 to determine (1) the effects of frozen bed and bank material on channel behavior, and (2) the importance of the annual breakup flood in forming the channels of arctic streams.
No takes yet. Share an insight, caveat, or question.
Kevin M. Scott (1978) studied this question.
Synapse has enriched 5 related papers. Consider them for comparative context: