Fifty years of recorded hillslope runoff on seasonally frozen ground: the Swift Current, Saskatchewan, Canada, dataset

<p>Long records of hillslope runoff and nutrient concentrations are rare – on seasonally frozen ground they are almost non-existent. The Swift Current hillslopes at the Swift Current Research and Development Centre on the Canadian Prairies provide such a long-term hydrological record. Runoff,...

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Main Authors: A. E. Coles, J. J. McDonnell, B. G. McConkey
Format: Article
Language:English
Published: Copernicus Publications 2019-09-01
Series:Earth System Science Data
Online Access:https://www.earth-syst-sci-data.net/11/1375/2019/essd-11-1375-2019.pdf
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spelling doaj-4738dc2711de4418b557713940f39fd62020-11-25T00:40:04ZengCopernicus PublicationsEarth System Science Data1866-35081866-35162019-09-01111375138310.5194/essd-11-1375-2019Fifty years of recorded hillslope runoff on seasonally frozen ground: the Swift Current, Saskatchewan, Canada, datasetA. E. Coles0A. E. Coles1J. J. McDonnell2J. J. McDonnell3B. G. McConkey4Global Institute for Water Security; School of Environment and Sustainability, University of Saskatchewan, 11 Innovation Boulevard, Saskatoon, SK S7N 3H5, CanadaWilfrid Laurier University, 5007 50th Avenue, Yellowknife, NT X1A 2P8, CanadaGlobal Institute for Water Security; School of Environment and Sustainability, University of Saskatchewan, 11 Innovation Boulevard, Saskatoon, SK S7N 3H5, CanadaSchool of Geography, Earth and Environmental Sciences, University of Birmingham, Birmingham, B15 2TT, UKSwift Current Research and Development Centre, Agriculture and Agri-Food Canada, P.O. Box 1030, Swift Current, SK S9H 3X2, Canada<p>Long records of hillslope runoff and nutrient concentrations are rare – on seasonally frozen ground they are almost non-existent. The Swift Current hillslopes at the Swift Current Research and Development Centre on the Canadian Prairies provide such a long-term hydrological record. Runoff, runoff nutrient concentration, snowpack depth, density and water equivalent, soil moisture, and soil nutrient concentration were monitored on the three 5&thinsp;ha hillslopes over a 50-year period (1962–2011). Digital elevation data are available for the three hillslopes at a 2&thinsp;m horizontal resolution, and, for one of the hillslopes (Hillslope 2), at a 0.25&thinsp;m horizontal resolution. Runoff from the hillslopes was generated episodically during snowmelt and occasional rainfall events. Hillslope runoff was measured with a 0.61&thinsp;m H-flume. Daily runoff nutrient concentration data are available for nitrate–N (March 1971–April 2011), ammoniacal–N (February 1996–April 2011), and phosphate-P (March–April 1971; June 1991–April 2011). Snowpack data (snowpack depth, density, and water equivalent) were determined via manual snow surveys carried out several times each winter, between January and March, between 1965 and 2011. Gravimetric soil moisture content was measured in October and April each year between 1971 and 2011 at five depth intervals (0–15, 15–30, 30–60, 60–90, and 90–120&thinsp;cm) at nine points on each hillslope. We provide these hillslope data in two publicly available repositories: (1) 1962–2011 data on runoff, runoff nutrients, snowpack, soil moisture, soil nutrients, and crop and tillage practices at <a href="https://doi.org/10.23684/hhn5-rz52">https://doi.org/10.23684/hhn5-rz52</a> (McConkey and Thiagarajan, 2018); and (2) digital elevation data at <a href="https://doi.org/10.20383/101.0117">https://doi.org/10.20383/101.0117</a> (Coles et al., 2018). Complete climate data recorded at a Environment and Climate Change Canada meteorological station located 390&thinsp;m from the three hillslopes are publicly available at <span class="uri">http://climate.weather.gc.ca/</span> (last access: 30 August 2019).</p>https://www.earth-syst-sci-data.net/11/1375/2019/essd-11-1375-2019.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. E. Coles
A. E. Coles
J. J. McDonnell
J. J. McDonnell
B. G. McConkey
spellingShingle A. E. Coles
A. E. Coles
J. J. McDonnell
J. J. McDonnell
B. G. McConkey
Fifty years of recorded hillslope runoff on seasonally frozen ground: the Swift Current, Saskatchewan, Canada, dataset
Earth System Science Data
author_facet A. E. Coles
A. E. Coles
J. J. McDonnell
J. J. McDonnell
B. G. McConkey
author_sort A. E. Coles
title Fifty years of recorded hillslope runoff on seasonally frozen ground: the Swift Current, Saskatchewan, Canada, dataset
title_short Fifty years of recorded hillslope runoff on seasonally frozen ground: the Swift Current, Saskatchewan, Canada, dataset
title_full Fifty years of recorded hillslope runoff on seasonally frozen ground: the Swift Current, Saskatchewan, Canada, dataset
title_fullStr Fifty years of recorded hillslope runoff on seasonally frozen ground: the Swift Current, Saskatchewan, Canada, dataset
title_full_unstemmed Fifty years of recorded hillslope runoff on seasonally frozen ground: the Swift Current, Saskatchewan, Canada, dataset
title_sort fifty years of recorded hillslope runoff on seasonally frozen ground: the swift current, saskatchewan, canada, dataset
publisher Copernicus Publications
series Earth System Science Data
issn 1866-3508
1866-3516
publishDate 2019-09-01
description <p>Long records of hillslope runoff and nutrient concentrations are rare – on seasonally frozen ground they are almost non-existent. The Swift Current hillslopes at the Swift Current Research and Development Centre on the Canadian Prairies provide such a long-term hydrological record. Runoff, runoff nutrient concentration, snowpack depth, density and water equivalent, soil moisture, and soil nutrient concentration were monitored on the three 5&thinsp;ha hillslopes over a 50-year period (1962–2011). Digital elevation data are available for the three hillslopes at a 2&thinsp;m horizontal resolution, and, for one of the hillslopes (Hillslope 2), at a 0.25&thinsp;m horizontal resolution. Runoff from the hillslopes was generated episodically during snowmelt and occasional rainfall events. Hillslope runoff was measured with a 0.61&thinsp;m H-flume. Daily runoff nutrient concentration data are available for nitrate–N (March 1971–April 2011), ammoniacal–N (February 1996–April 2011), and phosphate-P (March–April 1971; June 1991–April 2011). Snowpack data (snowpack depth, density, and water equivalent) were determined via manual snow surveys carried out several times each winter, between January and March, between 1965 and 2011. Gravimetric soil moisture content was measured in October and April each year between 1971 and 2011 at five depth intervals (0–15, 15–30, 30–60, 60–90, and 90–120&thinsp;cm) at nine points on each hillslope. We provide these hillslope data in two publicly available repositories: (1) 1962–2011 data on runoff, runoff nutrients, snowpack, soil moisture, soil nutrients, and crop and tillage practices at <a href="https://doi.org/10.23684/hhn5-rz52">https://doi.org/10.23684/hhn5-rz52</a> (McConkey and Thiagarajan, 2018); and (2) digital elevation data at <a href="https://doi.org/10.20383/101.0117">https://doi.org/10.20383/101.0117</a> (Coles et al., 2018). Complete climate data recorded at a Environment and Climate Change Canada meteorological station located 390&thinsp;m from the three hillslopes are publicly available at <span class="uri">http://climate.weather.gc.ca/</span> (last access: 30 August 2019).</p>
url https://www.earth-syst-sci-data.net/11/1375/2019/essd-11-1375-2019.pdf
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