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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[edit]DescriptionConceptual model describing the mechanisms of flow attenuation within a beaver wetland with an unconfined floodplain - hyp14735-fig-0008-m.webp |
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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current | 17:31, 3 November 2022 | 2,128 × 1,499 (243 KB) | Daniel Mietchen (talk | contribs) | Uploaded 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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