Aspects of river ice hydrology in Japan
β Scribed by Kenichi Hirayama; Makoto Yamazaki; Hung Tao Shen
- Publisher
- John Wiley and Sons
- Year
- 2002
- Tongue
- English
- Weight
- 551 KB
- Volume
- 16
- Category
- Article
- ISSN
- 0885-6087
- DOI
- 10.1002/hyp.375
No coin nor oath required. For personal study only.
β¦ Synopsis
Abstract
Rivers in northern Japan are subjected to ice formation each winter. They are typically very steep with rapid changes in channel slope. As a result, ice covers are usually discontinuous with open water sections. Winter discharges in Japanese rivers are usually very small. Water temperature and ice production in these streams are very sensitive to the change in air temperature. The open water sections enable the formation of frazil and anchor ice during the winter. Owing to the relatively stable winter weather and heavy snow cover, premature breakβup and ice jams rarely occur, even though the channel geometry of these rivers is favourable for their occurrence. In this paper, hydrometeorological factors related to iceβcover formation, frazil and anchorβice development, and iceβjam formation, as well as measurements of the undercover discharge in rivers in northern Japan are discussed. Copyright Β© 2002 John Wiley & Sons, Ltd.
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