File:Conceptual model describing the mechanisms of flow attenuation within a beaver wetland with an unconfined floodplain - hyp14735-fig-0008-m.webp

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English: Conceptual model describing the mechanisms of flow attenuation within a beaver wetland with an unconfined floodplain. As flow and therefore the depth of water behind the dam increases, the area of activated floodplain also increases; this results in the formation of new flow, infiltration and evapotranspiration pathways. These pathways become longer and more tortuous as the flooded area expands during a flow event. Canals likely play an important role in transporting water laterally into the floodplain further enhancing floodplain connection.
Date
Source Fig. 8 Graham, H. A., Puttock, A. K., Elliott, M., Anderson, K., & Brazier, R. E. (2022). Exploring the dynamics of flow attenuation at a beaver dam sequence. Hydrological Processes, 36( 11), e14735. doi:10.1002/hyp.14735.
Author Graham, H. A., Puttock, A. K., Elliott, M., Anderson, K., & Brazier, R. E. (2022)

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Conceptual model describing the mechanisms of flow attenuation within a beaver wetland with an unconfined floodplain

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13 October 2022

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current17:31, 3 November 2022Thumbnail for version as of 17:31, 3 November 20222,128 × 1,499 (243 KB)Daniel MietchenUploaded a work by Graham, H. A., Puttock, A. K., Elliott, M., Anderson, K., & Brazier, R. E. (2022) from Fig. 8 Graham, H. A., Puttock, A. K., Elliott, M., Anderson, K., & Brazier, R. E. (2022). Exploring the dynamics of flow attenuation at a beaver dam sequence. Hydrological Processes, 36( 11), e14735. doi:10.1002/hyp.14735. with UploadWizard
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