1 - Channel length survey data
A newer version of this resource http://www.hydroshare.org/resource/f7f86bc8877d4232acebf230f6e27cea is available that replaces this version.
An older version of this resource https://doi.org/10.4211/hs.66c2d423c6bd4004829c157a55ce0773 is available.
| Authors: | |
|---|---|
| Owners: | Christine D Leclerc |
| Type: | Resource |
| Storage: | The size of this resource is 471.5 KB |
| Created: | Oct 07, 2020 at 4:09 a.m. |
| Last updated: | Dec 11, 2020 at 6:03 p.m. (Metadata update) |
| Published date: | Oct 07, 2020 at 5:19 p.m. |
| DOI: | 10.4211/hs.ad933d662a7449138c0f22e64c7ec481 |
| Citation: | See how to cite this resource |
| Content types: | Single File Content Single File Content Single File Content Single File Content Single File Content Single File Content Single File Content Single File Content Single File Content Single File Content Single File Content Single File Content Single File Content Single File Content Single File Content Single File Content Single File Content Single File Content Single File Content Single File Content |
| Sharing Status: | Published |
|---|---|
| Views: | 1683 |
| Downloads: | 316 |
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Abstract
This directory includes channel length survey data (outlet discharge and surveyed wetted channel extent for each survey). These data were used, in conjunction with discharge data, to find the scaling factor (α) and scaling exponent (β) for the power function that relates wetted channel extent and discharge (L = αQ^β) reported in the metadata table. Resources associated with channel length include survey data, data ‘thieved’ plots from studies where channel length survey data was reported in plot format.
Subject Keywords
Coverage
Spatial
Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
North Latitude
51.8800°
East Longitude
8.7300°
South Latitude
35.0500°
West Longitude
-123.7300°
Temporal
| Start Date: | 11/01/1937 |
|---|---|
| End Date: | 06/28/2020 |
Leaflet Map data © OpenStreetMap contributors
Content
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NOT stored in HydroShare, and we can't guarantee its availability, quality, or
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Additional Metadata
Related Resources
| This resource is referenced by | Lapides, D., Leclerc, C. D., Moidu, H., Dralle, D., & Hahm, W. J. (2020, August 14). Variability of headwater stream network extents controlled by flow regime and network hydraulic scaling. https://doi.org/10.31223/osf.io/mc6np |
| This resource has been replaced by a newer version | Leclerc, C. D. (2020). 1 - Channel length survey data, HydroShare, http://www.hydroshare.org/resource/f7f86bc8877d4232acebf230f6e27cea |
| This resource updates and replaces a previous version | Leclerc, C. D. (2020). 1 - Channel length survey data, HydroShare, https://doi.org/10.4211/hs.66c2d423c6bd4004829c157a55ce0773 |
| The content of this resource is derived from | Zimmer, M.: Duke Forest Research Watershed Data Archives, https://doi.org/https://doi.org/10.2737/RDS-2016-0025, updated 19 July 2019, 2017. |
| The content of this resource is derived from | Godsey, S. E. and Kirchner, J. W.: Dynamic, discontinuous stream networks: hydrologically driven variations in active drainage density,flowing channels and stream order, Hydrological Processes, 28, 5791–5803, https://doi.org/10.1002/hyp.10310, 00010, 2014. |
| The content of this resource is derived from | Jensen, C. K., McGuire, K. J., and Prince, P. S.: Headwater stream length dynamics across four physiographic provinces of the Appalachian Highlands, Hydrological Processes, 31, 3350–3363, https://doi.org/10.1002/hyp.11259, _eprint:https://onlinelibrary.wiley.com/doi/pdf/10. 2017. |
| The content of this resource is derived from | Lovill, S. M., Hahm, W. J., and Dietrich, W. E.: Drainage from the Critical Zone: Lithologic Controls on the Persistence and Spatial Extent of Wetted Channels during the Summer Dry Season, Water Resources Research, 54, 5702–5726, https://doi.org/10.1029/2017WR021903. 2017. |
| The content of this resource is derived from | Whiting, J. A. and Godsey, S. E.: Discontinuous headwater stream networks with stable flowheads, Salmon River basin, Idaho, HydrologicalProcesses, 30, 2305–2316, https://doi.org/10.1002/hyp.10790, _eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.10790, 2016. |
| The content of this resource is derived from | van Meerveld, H. J. I.: Expansion and contraction of the flowing stream network alter hillslope flowpath lengths and the shape of the travel time distribution, Hydrology and Earth System Sciences, 23, 4825–6604834, https://doi.org/10.5194/hess-23-4825-2019, publisher: Copernicus GmbH, 2019. |
| The content of this resource is derived from | Shaw,S.B.: Investigating the linkage between streamflow recession rates and channel network contraction in a mesoscale catchment in New York state, Hydrological Processes, 30, 479–492, https://doi.org/10.1002/hyp.10626, _eprint: https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.10626, 2016. |
| The content of this resource is derived from | Blyth, K. and Rodda, J.: A stream length study, Water Resources Research, 9, 1454–1461, 1973. |
Credits
Funding Agencies
This resource was created using funding from the following sources:
| Agency Name | Award Title | Award Number |
|---|---|---|
| Natural Sciences and Engineering Research Council of Canada | Undergraduate Student Research Award |
How to Cite
Leclerc, C. D. (2020). 1 - Channel length survey data, HydroShare, https://doi.org/10.4211/hs.ad933d662a7449138c0f22e64c7ec481
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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