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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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 ha hillslopes over a 50-year period (1962–2011). Digital elevation data are available for the three hillslopes at a 2 m horizontal resolution, and, for one of the hillslopes (Hillslope 2), at a 0.25 m horizontal resolution. Runoff from the hillslopes was generated episodically during snowmelt and occasional rainfall events. Hillslope runoff was measured with a 0.61 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 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 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 ha hillslopes over a 50-year period (1962–2011). Digital elevation data
are available for the three hillslopes at a 2 m horizontal resolution, and,
for one of the hillslopes (Hillslope 2), at a 0.25 m horizontal resolution.
Runoff from the hillslopes was generated episodically during snowmelt and
occasional rainfall events. Hillslope runoff was measured with a 0.61 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 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 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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