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Streamflow response from an ombrotrophic mireAuthor(s): E.S. Verry; K.N. Brooks; P.K. Barten
Source: In: Proceedings of the international symposium on the hydrology of wetlands in temperate and cold regions; 1988 June 6-8; Joensuu, finland. helsinki, Finland: International Peat Society/The Academy of Finland: 52-59.
Publication Series: Other
Station: Northern Research Station
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DescriptionStreamflow response to a rainstorm exceeding a 100-year return interval is documented in relation to the peat profile and microtopography. The water tab1e:discharge relation is corrected for specific yield and found to closely parallel the stage:discharge relationship for a level reservoir for flows up to a 25-year return interval. A faster water table:discharge relation occurs at higher flows when the mire develops wedge storage in the completely flooded, channel-like lagg around 2/3 of the mire perimeter. Flood frequency analysis was used to estimate a 25-year return interval peak flow of 350 liters per second per sq. km for a 10-hectare basin.
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CitationVerry, E.S.; Brooks, K.N.; Barten, P.K. 1988. Streamflow response from an ombrotrophic mire. In: Proceedings of the international symposium on the hydrology of wetlands in temperate and cold regions; 1988 June 6-8; Joensuu, finland. helsinki, Finland: International Peat Society/The Academy of Finland: 52-59.
Keywordspeatlands, wetlands, mires, hydrology, floods, design flows
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