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This study examined opportunities and barriers for implementing evidence-based Social and Emotional Learning (SEL) programs in Prairie Canadian Schools. Educators from Manitoba, Saskatchewan and Alberta completed an online survey on SEL feasibility and reported on five feasibility domains: (1) attitudes about SEL, (2) knowledge about SEL, (3) job stress, (4) resources for implementing SEL, and (5) SEL practices. Results indicated that positive attitudes toward SEL significantly predicted increased perceived feasibility for evidence-based SEL implementation. Additionally, both knowledge and access to resources predicted increased SEL practice by Prairie Canadian educators. Analyses for open-ended responses paralleled quantitative results. Specifically, Canadian educators had positive views about SEL programing, but like previous research conducted in other countries, indicated that they require better access to SEL training, and resources (e.g., more time to plan and teach SEL, funding and program materials). A unique Canadian context-related finding from this study was that some Prairie Canadian educators indicated a paucity of French materials for SEL programs, which impeded implementation. In order to effectively implement evidence-based SEL in Prairie Canadian schools, policy makers must address the indicated barriers for Canadian educators, such as increased SEL training and resources, and easy access to appropriate French materials. [ABSTRACT FROM AUTHOR]

Croplands that experience seasonal soil freezing and thawing have been shown to be significant sources of N2O emissions. Yet, there is a paucity of year-round N2O emission data for one of the most significant crop production regions that seasonally freeze, the Prairies. Here, we present micrometeorological N2O fluxes measured over 4 years in Saskatchewan, Canada, to evaluate the magnitude of freeze-thaw N2O emissions and investigate its driving factors. Significant thaw related emissions occurred in 2 of the 4 years and were associated with relatively higher fall nitrate levels and a more gradual soil thawing period. Overall, fall soil nitrate levels were a strong explanatory variable for the differences in non-growing season (NGS) N2O emission (r² = 0.485). Measured cumulative N2O emissions for the NGS were 123-938 g N ha-1 and were much smaller than those obtained at other cold climate sites but amounted to 52% of annual totals on average. The November to April period contributed 30% of the annual total emissions in years without major thaw events, but 70% in years with significant thaws. NGS N2O emissions were not explained by cumulative freezing degree days unlike most other cold climate sites. We propose that NGS N2O emissions are more strongly influenced by thaw dynamics during freezing-thawing conditions in dry regions, whereas freezing intensity is the dominant factor for wetter regions. Our results indicate that even for a semi-arid region freezethaw is an important source of N2O emissions and must be considered for more accurate reporting and development of mitigation strategies. [ABSTRACT FROM AUTHOR]

A comparison was made of the supercooling points (SCPs) of questing Dermacentor variabilis adults from two populations located ca. 800 km apart on the Canadian prairies. This is also the first study to examine whether there are seasonal fluctuations in the SCP of questing D. variabilis adults. The SCPs of adult ticks from Lizard Lake Community Pasture, a recently established population in west-central Saskatchewan, varied over spring and summer, with the median SCP warming over time. In addition, the SCPs of ticks from Lizard Lake Community Pasture were significantly higher than those of adult ticks collected from Sandy Hook in Manitoba, a population that has been established for decades. The off-host survival of adults from Sandy Hook between summer and spring has been shown previously to be significantly greater than that of adults from Lizard Lake Community Pasture. The findings of the present study suggest that there may be geographical variation in the SCPs of D. variabilis adults which may be associated with differences in overwinter survival. The relatively low SCPs of questing D. variabilis adults, and the ability of some adults to survive off-host during winter, may be factors contributing to the range expansion of this tick species in Canada. [ABSTRACT FROM AUTHOR]

Soil organic carbon (SOC) sequestration assessment requires accurate and effective tools for measuring baseline SOC stocks. An emerging technique for estimating baseline SOC stocks is predictive soil mapping (PSM). A key challenge for PSM is determining sampling density requirements, specifically, determining the economically optimal number of samples for predictive soil mapping for SOC stocks. In an attempt to answer this question, data were used from 3861 soil organic carbon samples collected as part of routine agronomic soil testing from a 4702 ha farming operation in Saskatchewan, Canada. A predictive soil map was built using all the soil data to calculate the total carbon stock for the entire study area. The dataset was then subset using conditioned Latin hypercube sampling (cLHS), both conventional and stratified by slope position, to determine the total carbon stocks with the following sampling densities (points per ha): 0.01, 0.05, 0.1, 0.2, 0.3, 0.4, 0.5, 0.6, 0.7, and 0.8. A nonlinear error function was then fit to the data, and the optimal number of samples was determined based on the number of samples that minimized soil data costs and the value of the soil carbon stock prediction error. The stratified cLHS required fewer samples to achieve the same level of accuracy compared to conventional cLHS, and the optimal number of samples was more sensitive to carbon price than sampling costs. Overall, the optimal sampling density ranged from 0.025 to 0.075 samples per hectare. [ABSTRACT FROM AUTHOR]

Climate change (CC) poses a threat to agricultural sustainability, which is important in the Canadian Prairies, as agriculture is a major occupation and driver of the economy. Agriculture involves both the creation and mitigation of emissions related to CC. To implement adaptation and mitigation practices, producers should accept CC as fact. This study is based in Saskatchewan, Canada, where CC denial is prevalent in public comments. To assess the validity of this anecdotal impression, this study provided a snapshot of Saskatchewan agricultural producers' perceptions and observations of CC and assessed whether views on CC are associated with characteristics of political orientation and affiliation, mental flexibility, systems thinking, time orientation, climate knowledge, climate observations, and demographic variables. A survey was developed with the following four sections: (1) individual characteristics; (2) observed changes in climate-related variables; (3) knowledge and perceptions about CC; and (4) demographic variables. The survey included multiple-choice questions and items scored on a Likert scale. The survey was completed by 330 Saskatchewan agricultural producers (i.e., farmers and ranchers). The results indicated more CC denial in Saskatchewan producers than in other Canadian samples. Individual and socioeconomic characteristics of lower levels of formal education, identifying as male, conservative political affiliation and ideation, low trust in science, and low mental flexibility were associated with less acceptance and concern of CC. It is therefore necessary to consider socioeconomic and individual characteristics of producers in measures aiming to increase the acceptance of the reality of CC. Future intervention research should target male producers with lower levels of formal education, low trust in science, low mental flexibility, and right-leaning political ideation for the improvement of CC perceptions and examine different teaching methods (e.g., lectures, workshops, webinars) and dissemination methods (e.g., online versus in-person sessions) to see how various techniques may influence learning, as well as the way the information is used by particular groups. [ABSTRACT FROM AUTHOR]

Despite decades of effort, there remains an inability to measure snow water equivalent (SWE) at high spatial resolutions using remote sensing. Passive gamma ray spectrometry is one of the only well-established methods to reliably remotely sense SWE , but airborne applications to date have been limited to observing km-scale areal averages over shallow snowcovers. Noting the increasing capabilities of unoccupied aerial vehicles (UAVs) and miniaturization of passive gamma ray spectrometers, this study tested the ability of a UAV-borne gamma spectrometer and concomitant UAV-borne lidar to quantify the spatial variability of SWE at high spatial resolutions. Gamma and lidar observations from a UAV were collected over two seasons from shallow, wind-blown, prairie snowpacks in Saskatchewan, Canada with validation data collected from manual snow depth and density observations. The ability of UAV-gamma to resolve the areal average and spatial variability of SWE was promising with appropriate flight characteristics. Survey flights flown at a velocity of 5 m s-1, altitude of 15 m, and line spacing of 15 m were unable to capture the average or spatial variability of SWE within the uncertainty of the reference dataset. Slower, lower, and denser flight lines at a velocity of 4 m s-1, altitude of 8 m, and line spacing of 8 m were able to successfully observe areal average SWE and its variability at spatial resolutions greater than 22.5 m. Using a combination of UAV-based gamma SWE and UAV-based lidar snow depth improved the results substantially and permitted estimation of SWE at a spatial resolution of greater than 0.25 m with a ±14.3 mm SWE error relative to manual snow survey density and UAV-lidar based depths to estimate SWE. UAV-borne gamma spectrometry to estimate SWE is a promising and novel technique that has the potential to improve the measurement of shallow prairie snowpacks, and when combined with UAV-borne lidar snow depths, can provide high resolution, high accuracy estimates of prairie SWE. Research on optimal hardware, data processing, and interpolation techniques is called for to further improve this remote sensing product and explore its application in other environments. [ABSTRACT FROM AUTHOR]

Silver sagebrush (Artemisia cana) is a low shrub species that is common in northern mixed grass prairies and that provides important wildlife habitat. Silver sagebrush habitat has historically experienced frequent wildfires, but postsettlement fire control efforts have reduced fire frequencies. The effects of fire on silver sagebrush growth and regenera¬tion are not clearly understood; this study examined the effects of fire on silver sagebrush regeneration by evaluating post- fire plant size and distribution data from one season. Sites were located in the northern mixed prairie in Saskatchewan, Canada, and included pastures where the plant community was recovering from both prescribed fires and an intense wildfire. Silver sagebrush responded to fire by producing new shoots via rhizomes, with some plants also regenerating from the crown. No seedlings were observed. Larger plants and dense stands of silver sagebrush appeared to regenerate more successfully than did thin stands. These results demonstrated that silver sagebrush recovery is primarily vegetative, with clone mortality rare. [ABSTRACT FROM AUTHOR]

Overwintering in shallow habitats presents a serious obstacle for aquatic invertebrates. Here we investigated the little-known ability of water boatmen (Hemiptera: Corixidae), an aquatic insect, to survive the winter encased in air pockets within the ice of shallow wetlands. We extracted and experimentally thawed large blocks of ice from prairie wetlands in Saskatchewan, Canada, from which we examined the species composition and revival of corixids. While multiple corixid species were present in wetlands prior to freeze-up, a single species, Cymatia americana Hussey, 1920, comprised the vast majority of corixids that were found within the ice later in winter. Only 4%–9% of corixids, all Cymatia americana, revived after ice thawing over both study years. Being encased within an air pocket appeared to be necessary for the survival of corixids in the ice, with up to 300 individuals grouped together. Other invertebrate taxa also revived after thawing, including Haliplidae and Dytiscidae (Coleoptera) encased within air pockets both alongside corixids and on their own, as well as Coenagrionidae (Odonata), Phryganeidae and Leptoceridae (Trichoptera), Chironomidae (Diptera), and Physidae and Planorbidae (Basommatophora), which appeared to be encased in solid ice. The ability to overwinter inside ice represents a little understood survival mechanism of aquatic invertebrates in shallow wetlands, which could confer energetic and reproductive advantages to those that endure until spring. [ABSTRACT FROM AUTHOR]

The oomycete pathogen, Aphanomyces euteiches, was implicated for the first time in pea and lentil root rot in Saskatchewan and Alberta in 2012 and 2013. Subsequent surveys from 2014 to 2017 revealed that Aphanomyces root rot (ARR) was widespread across the Canadian prairies. The absence of effective chemical, biological, and cultural controls and lack of genetic resistance leave only one management option: avoidance. The objectives of this study were to relate oospore levels in autoclaved and non-autoclaved soils to ARR severity across soil types from the vast prairie landscape and to determine the relationship of measured DNA quantity of A. euteiches using droplet digital PCR or quantitative PCR to the initial oospore inoculum dose in soils. These objectives support a future end goal of creating a rapid assessment method capable of categorizing root rot risk in field soil samples to aid producers with pulse crop field selection decisions. The ARR severity to oospore dose relationship was statistically significantly affected by the soil type and location from which soils were collected and did not show a linear relationship. For most soil types, ARR did not develop at oospore levels below 100/g soil, but severity rose above this level, confirming a threshold level of 100 oospores/g soil for disease development. For most soil types, ARR severity was significantly higher in non-autoclaved compared to autoclaved treatments, demonstrating the role that other pathogens play in increasing disease severity. There was a significant linear relationship between DNA concentrations measured in soil and oospore inoculum concentration, although the strength of the relationship was better for some soil types, and in some soil types, DNA measurement results underestimated the number of oospores. This research is important for developing a root rot risk assessment system for the Canadian prairies based on soil inoculum quantification, following field validation of soil quantification and relationship to root rot disease severity. [ABSTRACT FROM AUTHOR]

Indigenous oral histories say that Treaty No. 6 (1876) was not only a legal transaction but rather a ceremony of adoption whereby incoming settler peoples became relatives. With Indigenous theories of relationality now informing many disciplines, how do white settler peoples take up the framework of kinship without using it only as a metaphor—and thereby as yet another tool of settler-colonial displacement? This essay examines this risk by considering the figurative use of kinship terms by Commissioner Alexander Morris at the negotiations for Treaty No. 6, in what is now Saskatchewan, Canada. Morris's reliance on a borrowed vocabulary of kinship was, like his participation in the ceremony of the sacred pipestem, an invocation of relationality as a rhetorical device aimed at securing the 'surrender' of the lands. While metaphor is a figure that can mislead, coerce, or yoke, however, it can also make relationships, make things akin. In light of the continued relevance of the Indigenous legal framework known as treaty, this discussion takes up the possibility of kinship metaphors as not only figurative but also as literal, binding, and central to the possibility of good relations in the prairies today. [ABSTRACT FROM AUTHOR]

This article focuses on the provenance of the Stanley Collection—a group of 69 items from reserves in the Touchwood Hills area of Saskatchewan. The items were collected by reserve farm instructor Edward Stanley and his wife Elizabeth at the turn of the century and then sold to the Saskatchewan Museum of Natural History in 1914. By analyzing historical documents, artifacts, and oral histories, this study shows that the Stanley Collection was acquired under a colonialist collecting model that was largely influenced by power relations and then became part of provincial identity building in the early 1900s. Such insight contributes to a growing body of literature on collecting in the Canadian Prairies and also seeks to address reconciliation efforts in Canada. As the first study of the Royal Saskatchewan Museum's founding ethnographic collection, this paper provides an intriguing look at early collecting practices and the formation of the first museum in the Prairie provinces. [ABSTRACT FROM AUTHOR]

The Canadian Prairie Provinces (Alberta, Saskatchewan and Manitoba) are home to species from 29 of the 45 spider families currently found in Canada. Here we provide a beginner-friendly dichotomous key to the spider families of the Canadian Prairies. The key includes numerous photos, line drawings, and simplified definitions of anatomical characters necessary for family-level identification. For each family we include an illustrated summary of important character states, a whole-body photo of an exemplar of the family, and number of species of the family currently reported from the Prairie Provinces. [ABSTRACT FROM AUTHOR]

Temperate grasslands are the most endangered and least protected biome in the world. Few significant parcels remain and strategies for ongoing protection are critical for conservation efforts worldwide. In southwestern Saskatchewan, three contiguous blocks of native grassland, known as the Prairie Pastures Conservation Area, are federally managed by Environment and Climate Change Canada. Previously, the 800‐km2space was managed by the Department of Agriculture as public rangeland in the Prairie Farm Rehabilitation Agency (PFRA). We interviewed 11 individuals, including NGO representatives and pasture patrons, familiar with the PFRA at a native prairie/grassland conference to enhance our understanding of the importance of the agency and the lands in the province to them, as well as to Canada and globally. Themes that emerged included benefits of historic PFRA management, reservations about privatization of pasturelands, and worries about mismanagement. We take these themes and build them into our recommendations for what Environment and Climate Change Canada should do with the Prairie Pastures Conservation Area going forward: enhance Indigenous collaboration, establish a conservation network, and increase public use and awareness. [ABSTRACT FROM AUTHOR]

Copyright of Canadian Water Resources Journal / Revue Canadienne des Ressources Hydriques is the property of Taylor & Francis Ltd and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Copyright of Canadian Veterinary Journal / Revue Vétérinaire Canadienne is the property of Canadian Veterinary Medical Association and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Significant challenges from changes in climate and land use face sustainable water use in the Canadian Prairies ecozone. The region has experienced significant warming since the mid-20th century, and continued warming of an additional 2 ∘ C by 2050 is expected. This paper aims to enhance understanding of climate controls on Prairie basin hydrology through numerical model experiments. It approaches this by developing a basin-classification-based virtual modelling framework for a portion of the Prairie region and applying the modelling framework to investigate the hydrological sensitivity of one Prairie basin class (High Elevation Grasslands) to changes in climate. High Elevation Grasslands dominate much of central and southern Alberta and parts of south-western Saskatchewan, with outliers in eastern Saskatchewan and western Manitoba. The experiments revealed that High Elevation Grassland snowpacks are highly sensitive to changes in climate but that this varies geographically. Spring maximum snow water equivalent in grasslands decreases 8 % ∘ C -1 of warming. Climate scenario simulations indicated that a 2 ∘ C increase in temperature requires at least an increase of 20 % in mean annual precipitation for there to be enough additional snowfall to compensate for enhanced melt losses. The sensitivity in runoff is less linear and varies substantially across the study domain: simulations using 6 ∘ C of warming, and a 30 % increase in mean annual precipitation yields simulated decreases in annual runoff of 40 % in climates of the western Prairie but 55 % increases in climates of eastern portions. These results can be used to identify those areas of the region that are most sensitive to climate change and highlight focus areas for monitoring and adaptation. The results also demonstrate how a basin classification-based virtual modelling framework can be applied to evaluate regional-scale impacts of climate change with relatively high spatial resolution in a robust, effective and efficient manner. [ABSTRACT FROM AUTHOR]

The North American Great Plains cover a large area of the Nearctic ecozone, and an important part of this biome is semiarid. The sustainable intensification of agriculture that is necessary to produce food for an ever-increasing world population requires knowledge of the taxonomic and functional structure of the soil microbial community. In this study, we investigated the influence of soil depth on the composition and functions of the microbial communities hosted in agricultural soils of a semiarid agroecosystem, using metagenomic profiling, and compared them to changes in soil chemical and physical properties. Shotgun sequencing was used to determine the composition and functions of the soil microbial community of 45 soil samples from three soil depths (0–15 cm, 15–30 cm, and 30–60 cm) under different agricultural land use types (native prairie, seeded prairie, and cropland) in southwest Saskatchewan. Analysis of community composition revealed the declining abundance of phyla Verrucomicrobia, Bacteroidetes, Chlorophyta, Bacillariophyta, and Acidobacteria with soil depth, whereas the abundance of phyla Ascomycota, Nitrospirae, Planctomycetes, and Cyanobacteria increased with soil depth. Soil functional genes related to nucleosides and nucleotides, phosphorus (P) metabolism, cell division and cell cycle, amino acids and derivatives, membrane transport, and fatty acids were particularly abundant at 30–60 cm. In contrast, functional genes related to DNA and RNA metabolism, metabolism of nitrogen, sulfur and carbohydrates, and stress response were more abundant in the top soil depth. The RDA analysis of functional genes and soil physico-chemical properties revealed a positive correlation between phages and soil organic P concentrations. In the rooting zone of this semiarid agroecosystem, soil microbes express variable structural patterns of taxonomic and functional diversity at different soil depths. This study shows that the soil microbial community is structured by soil depth and physicochemical properties, with the middle soil depth being an intermediate transition zone with a higher taxonomic diversity. Our results suggest the co-existence of various microbial phyla adapted to upper and lower soil depths in an intermediate-depth transition zone. [ABSTRACT FROM AUTHOR]

Copyright of Canadian Journal of Plant Science is the property of Canadian Science Publishing and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

Cold regions provide water resources for half the global population yet face rapid change. Their hydrology is dominated by snow, ice and frozen soils, and climate warming is having profound effects. Hydrological models have a key role in predicting changing water resources but are challenged in cold regions. Ground‐based data to quantify meteorological forcing and constrain model parameterization are limited, while hydrological processes are complex, often controlled by phase change energetics. River flows are impacted by poorly quantified human activities. This paper discusses the scientific and technical challenges of the large‐scale modelling of cold region systems and reports recent modelling developments, focussing on MESH, the Canadian community hydrological land surface scheme. New cold region process representations include improved blowing snow transport and sublimation, lateral land‐surface flow, prairie pothole pond storage dynamics, frozen ground infiltration and thermodynamics, and improved glacier modelling. New algorithms to represent water management include multistage reservoir operation. Parameterization has been supported by field observations and remotely sensed data; new methods for parameter identification have been used to evaluate model uncertainty and support regionalization. Additionally, MESH has been linked to broader decision‐support frameworks, including river ice simulation and hydrological forecasting. The paper also reports various applications to the Saskatchewan and Mackenzie River basins in western Canada (0.4 and 1.8 million km2). These basins arise in glaciated mountain headwaters, are partly underlain by permafrost, and include remote and incompletely understood forested, wetland, agricultural and tundra ecoregions. These illustrate the current capabilities and limitations of cold region modelling, and the extraordinary challenges to prediction, including the need to overcoming biases in forcing data sets, which can have disproportionate effects on the simulated hydrology. [ABSTRACT FROM AUTHOR]

Copyright of Canadian Water Resources Journal / Revue Canadienne des Ressources Hydriques is the property of Taylor & Francis Ltd and its content may not be copied or emailed to multiple sites or posted to a listserv without the copyright holder's express written permission. However, users may print, download, or email articles for individual use. This abstract may be abridged. No warranty is given about the accuracy of the copy. Users should refer to the original published version of the material for the full abstract. (Copyright applies to all Abstracts.)

The global crop sector is estimated to contribute about 10.4% of global GHGs annually. The Canadian crop sector is assessed as adding about 6.5% to total national emissions. These estimates over report the impact of farming as they ignore the complex interaction of cropping with the environment and the role land use, land use change and forestry (LULUCF) play in sequestering carbon. This study quantifies the contribution of land use to GHG emissions and removals in the Canadian Prairies crop sector between 1985 and 2016. The modeling effort explores how different farming practices (i.e., conventional tillage (CT), minimum tillage (MT), zero tillage (ZT), summerfallow, crop rotations, and residue retention) and input usage rates (i.e., fertilizer and fuel) affect GHG emissions in different soil climate zones and provinces in the Prairies region. The adoption of sustainable practices led to an 80% decline in GHG emissions in the crop sector between 1985 and 2016. Since 2005, the baseline for Canada's Paris commitment, sectoral emissions dropped 53%, more than is required to meet the 2030 target. Most promising, the crop sector was a net GHG sink between 2013 and 2016 in Alberta and between 2006 and 2016 in Saskatchewan. As positive as these developments have been, more can be done by directing research to identify options for reducing GHGs in Manitoba (which made only minimal improvements as farmers there faced conditions requiring continuous use of conventional tillage practices), to explore better nitrogen management (a major continuing source of GHG from cropping) and by searching for low carbon transport options. [ABSTRACT FROM AUTHOR]

Prairie moonwort (Botrychium campestre W.H. Wagner & D.R. Farrar) from the adder's tongue family (Ophioglossaceae) is a rare plant species in North America with a NatureServe designation of G3N2 (Globally Vulnerable, Nationally Imperiled). The species reaches its northern distribution limit in Saskatchewan, Canada. The range of B. campestre is described here from literature, herbarium data, and field studies. Two newly discovered peripheral populations are reported, and their habitats are characterized in detail. One of the new occurrences was monitored over a multiyear period, and changes in population and vegetation cover are described. Possible threats to the newest occurrences are identified. These results constitute the first reference on the status of B. campestre in Saskatchewan, which is important for the management and conservation of this rare plant species. Recommendations to protect these populations and to establish monitoring to track changes in their natural habitat are presented. [ABSTRACT FROM AUTHOR]

To assess the potential change in agroclimatic indices in western Canada, this study used a convection-permitting Weather Research Forecasting (WRF) model to conduct simulations for the current climate (CTL, 2000-2015) and future climate under the RCP8.5 scenario based on a pseudo-global-warming (PGW) approach. Both CTL and PGW simulations were bias-corrected to the GEM-CaPA dataset using a multivariate quantile mapping method. An evaluation of the CTL simulation of daily maximum and minimum temperatures and precipitation during the growing season against the gridded observations has been performed, indicating good agreements in the spatial patterns of air temperature and precipitation in western Canada. The PGW-CTL differences in several selected agroclimatic indices were then examined. Due to rising temperatures, substantial increases in growing degree-days (GDD) by 800-1,200◦ days and reductions in frost days by 10 to 20 days, favouring regional crop production, are found in southern Alberta and Saskatchewan. However, globalwarming also poses great risks to Canadian agriculture by modifying heat accumulations and water availability during the growing season. Plant heat stress will substantially increase by ∼50◦ days in southern Alberta and Saskatchewan, offsetting the positive effects caused by the reduction in frost days and increase in GDD. The southern Canadian Prairies will experience statistically significant increases in the number of dry days and precipitation deficit, suggesting an exacerbation of water stress on the Canadian Prairies by global warming. [ABSTRACT FROM AUTHOR]

Richardson's ground squirrel (Urocitellus richardsonii (Sabine, 1822)) is a widespread burrowing mammal on the northern Great Plains. This species is a prominent prey item for a variety of predators and its burrows provide important habitat for other wildlife; however, Richardson's ground squirrel is also considered an economically damaging agricultural pest. Despite the ecological importance of Richardson's ground squirrels and their status as pests, there are gaps in our knowledge about large-scale habitat associations for this species. In 2011 and 2012, we conducted 1840 roadside surveys in a 130 000 km2 area of southern Saskatchewan, Canada, to understand which habitat features are associated with Richardson's ground squirrel occurrence. Ground squirrels were observed on 8% of the surveys. Probability of ground squirrel occurrence was highest in areas with moderate amounts of grassland (approximately 30%), areas that were developed by humans (>30%), and had a high proportion of clay loam soils, presumably for burrowing. Our study highlights the importance of heterogeneous landscapes and that areas disturbed by humans may provide suitable vegetation structure for ground squirrels. This information can help to identify important habitat for species that rely on Richardson's ground squirrels and identify areas where Richardson's ground squirrels could come into conflict with agriculture. [ABSTRACT FROM AUTHOR]

• Analyzes Saskatchewan government consultations on agricultural land ownership. • Responses do discursive work of challenging and reifying current property relations. • Stories told reinforce private property regimes, justify settler colonialism. • Values expressed suggest different social relations regarding land are possible. • Persuasive stories of alternatives, communicating values, could help induce change. Global conflicts over land grabbing, financialization, and conservation have generated resistance from diverse local peoples who insist that land must be more than a commodity; it has social, cultural, and ecological value alongside its economic productivity. Saskatchewan's government has recently responded to similar conflicts over investment, privatization, and concentration of landholding, by engaging in public consultations on farmland ownership. Analyzing comments from public consultation surveys in 2015 and 2017, the paper employs insights from property theory, legal studies, geography, and scholarship on storytelling to analyze how respondents' values, expressed through stories, work to change or maintain property relations. As a resource, agricultural land is endowed with value that changes over time and space. Land tenure regimes consist of shifting social relations regarding this resource, and these relations are often arrived at and maintained through persuasive narratives framed through social value claims about heritage, identity, livelihoods, and community norms. These stories also have a material effect on resource use and property regimes. In Saskatchewan, as survey respondents employ stories to influence policy decisions on agricultural land tenure and advocate for the status quo, they utilize social values that justify their entitlements. Alternative property relations, advocated or proposed by some respondents, provide more fundamental challenges to absolutist notions of private property rights and thus face ideological barriers to acceptance and implementation through policy. However, telling different stories can be a way to alter property relations. [ABSTRACT FROM AUTHOR]

North Dakota is a significant producer of wind energy in the United States. In the first decades of this century, the state went from almost zero production to over 25% of its electricity sourced from wind energy. Across the border in Canada, the province of Saskatchewan—which has the same wind capacity as North Dakota—did not develop wind energy during this same time period. This paper looks at print news media coverage of renewable energy, especially wind energy, in the two jurisdictions between 2009–2018. The main finding is that news media coverage of renewable energy is similar despite the very different wind energy portfolios. This suggests a possible disjoint between the media and public discourse on renewable energy politics. Regardless of the size of the renewable energy sector, the media reports very little on it. Overall, the study concludes that more robust discussions around the environment-energy nexus would be beneficial as the jurisdictions continue to grow their energy portfolios and potentially transition toward more renewable energies. [ABSTRACT FROM AUTHOR]

We present findings of a general survey of pest wireworms in Alberta, Saskatchewan, and Manitoba conducted from 2004 to 2019; the first such survey of the Canadian Prairie provinces since that published by Glen et al. (1943). Samples were collected from 571 farmland locations where crop damage from wireworms was observed or suspected, and a total of 5,704 specimens (3,548 larvae, 2,156 beetles) were identified. Most specimens (96.9%) were identified as Hypnoidus bicolor (3,278), Selatosomus aeripennis destructor (1,280), Limonius californicus (842), and Aeolus mellillus (125). This suggests that H. bicolor has replaced S. a. destructor as the predominant species and that the relative importance of L. californicus as a pest species has increased since earlier reports. Despite the relatively small number of specimens collected per location (approx. 10), H. bicolor and S. a. destructor , and S. a. destructor and L. californicus were frequently collected at or near the same location (within 1 km). We provide species records and incidence of co-occurrence at different spatial scales, discuss potential reasons for and implications of shifts in species composition, implications of species co-occurrence for managing wireworm pests in crop production, and outline pertinent research needs. A path analysis approach used to correlate incidence of the main species with various soil characteristics indicated that organic matter, cation exchange capacity, and water retention capacity all had a significant species-specific influence on wireworm presence. [ABSTRACT FROM AUTHOR]

Waterbirds are important indicators of wetland health, and understanding their status and trends is necessary for appropriate management and conservation. However, certain species are challenging to survey due to their sensitivity to disturbance and the difficulty of accessing their breeding habitats. This is especially true for colonially breeding marshbirds, for which a multi‐species survey protocol that maximizes accuracy of counts and minimizes disturbance does not exist. Small drone aircraft have shown promise for conducting accurate and low‐disturbance surveys of colonial waterbirds. However, complex marsh vegetation structures and the cryptic nature of some marshbird nests make them difficult to detect in aerial imagery. We used synchronous high‐resolution visible imagery (0.8–2 cm/pixel) and thermal‐infrared imagery (6–16 cm/pixel) captured from a drone to count nests of five species of marshbirds at eight colonies in Saskatchewan, Canada. We compared counts from the imagery to those obtained from traditional ground‐based surveys, generally considered the most accurate survey method for these species. The two types of imagery proved highly complementary, as heat signatures helped detect and confirm nests not easily spotted in the visible imagery, while the detailed visible imagery allowed species identification. For four species (Western Grebe Aechmophorus occidentalis, Franklin's Gull Leucophaeus pipixcan, Forster's Tern Sterna forsteri, and Black‐crowned Night‐Heron Nycticorax nycticorax), drone‐based counts (range 74–1524 nests per colony) were within 5% of ground‐based counts (range 75–1582), while for smaller Black Tern Chlidonias niger colonies (range 3–7 nests), counts from the two methods were always within one nest of each other. Furthermore, an assessment of flight behavior before, during, and after drone surveys found no significant evidence of disturbance by the drone. Our drone‐borne dual visible‐thermal camera approach proved promising for surveying colonial marshbirds and could potentially be implemented in a range of situations where wildlife subjects are difficult to survey with visible or thermal imagery alone. [ABSTRACT FROM AUTHOR]

The Dakota skipper, Hesperia dacotae, (Hesperiidae) is an at-risk Lepidoptera species, limited in Canada to native mesic mixed-grass prairie habitat in Saskatchewan and Manitoba. Due to declines in the native mesic mixed-grass prairie the Dakota skipper population is threatened by loss of habitat. Currently, there is little knowledge about Dakota skipper and the availability and distribution of suitable habitat within Saskatchewan. Our objective was to map potential Dakota skipper habitat using a Generalized Linear Model (GLM) based species distribution model with climate, soil, and landscape predictor variables. Potential Dakota skipper habitat was found broadly in the mesic mixed-grass prairie region, however there is only ~217 km2 of potential habitat (probability of occurrence 0.7-1). Locations with high probability of occurrence had soils with a significantly higher soil ammonium ( NH 4 + ) and silt content than low probability locations. While the Dakota skipper is broadly distributed in native mesic mixed-grass prairie of southeastern Saskatchewan, environmental constraints likely restrict this species to a limited proportion of the intact native prairie. Implications for insect conservation: Mapping landscape-level species distributions will assist in the development of conservation and management plans for the Dakota skipper in southeastern Saskatchewan including targeted surveys for unknown populations in areas of high potential, identification of potential reintroduction sites, and selection of lands for conservation. [ABSTRACT FROM AUTHOR]

Shelterbelt agroforestry systems represent an actively managed historical agricultural resource for which farmers are the driving force, and their decisions have long-term consequences. For decades, detailed records were maintained of millions of trees and shrubs planted in shelterbelts on agricultural fields and farmyards across the Canadian Prairies. However, no records were collected regarding shelterbelt removals. This study quantified the length and carbon (C) stocks of all removed shelterbelts in Saskatchewan for the 2008–2016 period, and identified shelterbelt removal trends across five soil zones. Removals were detected using a recently developed integrated GIS and remote sensing approach, and were land-use features that were mapped as shelterbelts in an inventory map in 2008 but were missing in the classified map in 2016. A total of 2491.2 km of shelterbelts were removed, containing 190.7 GgC (1 Gg = 1000 Mg = 1000 tonnes). The majority of C stock removals were in shrub shelterbelts (107.2 GgC; 1676.6 km), followed by deciduous (78.1 GgC; 719.1 km) and coniferous shelterbelts (5.4 GgC; 95.5 km). Medium (2–3 rows) and wide (> 3 rows) shelterbelts had higher likelihood of being completely removed, while narrow (1 row) shelterbelts were only shortened. Removals in the < 50 m length designs were one- to three-orders of magnitude higher than any other shelterbelt length design. Future shelterbelt removal studies could serve to sustain the carbon sequestration effectiveness of the existing and extensive shelterbelt network on the Canadian Prairies in the long term, and to protect an important agricultural resource that took a very long time to establish. [ABSTRACT FROM AUTHOR]

Aims: We examined how restoration affects the structure and function of grasslands belowground by relating changes in the morphology and architecture of root systems of dominant plants to the structure of soil food webs. Methods: We measured changes in root traits of dominant plants (Bouteloua gracilis and Pascopyrum smithii) and related them to the diversity and feeding structure of soil nematodes across a restoration chronosequence in a mixed-grass prairie in Grasslands National Park, Saskatchewan, Canada. Results: Root architecture and morphology of dominant grasses changed with restoration, and soil food webs in recently restored prairies centred around resources provided by roots. In contrast, food webs in a native prairie centred around the decomposition of soil organic matter and plant litter. Conclusions: Our study demonstrates that changes in root traits following restoration can cascade through soil foodwebs, altering the function of restored prairies. Our study also highlights that the diversity and structure of soil nematodes can reflect changes in root traits of dominant plants. However, traits that generalize the whole root system may be insufficient to explain the causal relationship between root feeding nematodes and their resources. [ABSTRACT FROM AUTHOR]

Canada is one of the largest wheat producers in the world, and wheat is grown over an area spanning most of the southern latitudes, with the prairie region (provinces of Saskatchewan, Alberta, and Manitoba) being the main producer. Several pathogens and pests attack wheat, but at present fusarium head blight (FHB), stripe rust, and leaf spots are the most damaging diseases to wheat production in Canada. Historically, smuts, stem rust, and leaf rust caused major crop losses in Canada and can still pose serious threat if management practices are relaxed. Cropping practices used by Canadian farmers to grow and harvest wheat over the last century have influenced disease development and pathogen biology, affecting the severity, incidence, and prevalence of crop diseases over time. Changes such as reduced tillage coincide with emergence of residue‐borne diseases, such as FHB and leaf spots, while the deployment of resistant cultivars and increased fungicide use has resulted in the reduction of common bunt, stem, and leaf rust. This review will discuss the influence of long‐term cropping practices, alone or in combination, on the biology, emergence, and prevalence of wheat diseases in Canada over the last century. [ABSTRACT FROM AUTHOR]

The North American Great Plains contains thousands of lakes that vary in salinity from freshwater to hypersaline. Paleolimnological studies show that salinity levels in these lakes are tightly linked with climate, and current projections point to a more arid future in the region due to natural and anthropogenic climate change, potentially influencing lake salinity.Many zooplankton species are sensitive to changes in salinity, and their position near the base of the aquatic food web makes it important to understand how they might respond to increasing salinity levels. Zooplankton communities in lakes with rising salinity levels may exhibit changes in structure, including a shift toward more salinity‐tolerant species and a reduction in abundance, species richness, and diversity. However, it is possible that dispersal of zooplankton among lakes could mitigate such community changes when migrant populations replace sensitive zooplankton with those that are locally adapted to higher salinities.To test if dispersal could reduce salinity‐induced changes in zooplankton communities, we ran a field enclosure experiment at a freshwater lake in southern Saskatchewan where we manipulated salinity levels and zooplankton dispersal. We evaluated how salinity and dispersal influenced species identities and relative abundances (community structure) using multivariate statistics and comparing taxonomic and functional compositions among the different treatments (richness, diversity, and evenness).We found that increasing salinity levels in our enclosures above that in our study lake resulted in lower zooplankton abundances and species richness levels, primarily due to the loss of cladoceran species. However, patterns in our multivariate analyses suggested that cladocerans were maintained in enclosures with salinity levels of 2.5 and 5.0 g/L when those enclosures received immigration from nearby lakes.In contrast, our univariate analyses failed to find evidence that immigration affected community structure (richness, diversity, evenness). The lack of significant statistical differences could suggest that dispersal does not have an effect, or it may have been a problem with statistical power, as a power analysis suggested that fairly large effect sizes would have been required to achieve statistical significance.Based on our results, we were unable to reach a definitive conclusion on the role that dispersal might play in buffering zooplankton communities against salinity‐driven changes. However, our study provides two important insights for planning future work. First, our power analyses indicated that more replication may be needed given the variability among our experimental enclosures. Second, the patterns in our multivariate analyses suggested that cladocerans could be maintained in lakes undergoing salinity increases if they receive immigration from surrounding lakes with higher salinities. Future work examining how inter‐ and intraspecific salinity tolerance varies across lakes with a gradient of salinities would be helpful for understanding the role that dispersal might play in buffering against salinity‐driven losses of cladoceran zooplankton. [ABSTRACT FROM AUTHOR]

The Esterhazy Member of the western Canada Prairie Evaporite has been mined underground for sylvite (KCl) since the early 1960s. Although the geology of the Esterhazy Member ore body is largely considered a regional flat lying continuous series of thin potash hosting beds, there are numerous occurrences where the ore has been either replaced or removed leaving behind uneconomical halite-rich sections. An explanation of the underlying controls on the formation of these salt anomalies has been somewhat elusive although the overwhelming assumption remains that these features developed in lows on a salina. This paper proposes that salt anomalies formed because of two processes, early compaction of carbonate shoals of the Winnipegosis Formation and tectonics that resulted in multiple stages of block movement during the deposition of the upper Prairie Evaporite. Since these two processes can result in a significantly different size to a salt anomaly, encountering one or the other type can have a significant effect on the economics of the ore body. This paper looks at some of the geological methods that might provide geologists with means to predicting salt anomalies. [ABSTRACT FROM AUTHOR]

Anthropogenic development may influence the choices animals make and their resulting reproductive success and survival. If such choices are maladaptive, the impact of anthropogenic change can be catastrophic to small or declining populations. Over the past century, Canada's prairie landscapes have been altered dramatically, with over two‐thirds of its native grasslands now having been converted to cropland. The decline of the endangered Burrowing Owl Athene cunicularia population is assumed to have resulted from this landscape change, yet no causal link has been demonstrated. One hypothesis to explain this population decline is that owls get caught in an ecological trap, whereby they prefer to establish nests at the start of each breeding season in landscapes that later confer lower reproductive success. Agricultural landscapes represent a plausible potential ecological trap because the short and sparse vegetation in annual crops (seeded each spring) is predicted to be attractive nesting/foraging habitat for Burrowing Owls when they arrive from northward migration, yet crops become substantially taller and denser over the growing season so prey are predicted to become less accessible by the time broods have hatched. We tested this ecological trap hypothesis in a 3‐year study, involving 379 Burrowing Owl pairs, across the agricultural landscapes of southern Alberta and Saskatchewan. In support of the hypothesis, Burrowing Owls did prefer to settle in breeding home‐ranges that contained a higher proportion of cropland, and their prey‐delivery rates during brood‐rearing were lower at nests with a higher proportion of cropland growing in the surrounding landscape. However, in contradiction to a key prediction, the number of fledglings produced (range = 0–9) was higher, not lower, for pairs with more actively growing cropland in their landscapes. Therefore, the decline of the Burrowing Owl in Canada does not appear to result from cropland forming an ecological trap during the breeding season. We also found a significant positive relationship between the amount of summer fallow within Burrowing Owl home‐ranges and the quantity of vertebrate prey delivered to the nest and the number of juveniles fledged, highlighting the importance of this declining land use in raptor conservation. [ABSTRACT FROM AUTHOR]

• Compared alternative vs. conventional rotations on SOM and aggregate stability (AS) • Diverse crop rotations had no effect on SOM dynamics in the short term. • Adding pulse crops to cereal-dominated rotations improved AS. • Mineral-associated organic matter fraction strongly correlated with AS. • SOM and AS responses to crop rotations are site-specific. There is a need to develop and adopt novel, more resilient, or "climate-smart" cropping strategies on the Canadian prairies, which are crucial for sustainable agroecosystem management. To examine how crop rotation influences soil organic matter and aggregate stability (AS) dynamics, six crop rotations: (i) conventional (control), (ii) pulse/oilseed intensified, (iii) diversified, (iv) market-driven, (v) high-risk and high-reward, and (vi) soil health-enhanced were established in 2018 at three field sites: Lethbridge, Alberta and Swift Current and Scott, Saskatchewan under no-till management. After 4-year, soil organic carbon (SOC), total nitrogen (TN), particulate organic matter carbon (POM-C) and nitrogen (POM-N), or mineral-associated organic matter C (MAOM-C) and N (MAOM-N) concentrations were not significantly affected by crop rotation in the 0–7.5 cm soil depth. However, crop rotation significantly altered AS at two of three sites, with both soil health-enhanced and high-risk and high-reward rotations having the highest AS at Lethbridge and Swift Current. Across all three sites, strong positive correlations were found among SOC, TN, MAOM, and AS. Moreover, MAOM-C and MAOM-N showed stronger relationships with AS than POM, perhaps suggesting a positive feedback loop on the stability of SOC and aggregation. Overall, the inclusion of pulses in rotations showed the potential to sustain soil quality, likely by offsetting low residue quantity with better residue quality and diversity, thereby supporting SOC accrual and AS similar to or greater than conventional cereal- or oilseed-dominated rotations. [ABSTRACT FROM AUTHOR]

This paper has examined the relative significance of uncertainty in future climate projections from a subset of the coupled model intercomparison project phase 5 (CMIP5) global climate models for the Prairie Provinces of western Canada. This was undertaken by determining: (a) the contribution of model and scenario uncertainty and natural variability to the total variance of these future projections, and (b) the timing of climate signal emergence from the background noise of natural climate variability. We examined future projections of mean temperature, precipitation and summer climate moisture index (CMI). In this region, natural climate variability plays an important role in future uncertainty until the end of this century, particularly for precipitation and to a lesser extent, summer CMI. Model uncertainty also contributes to total uncertainty for these variables throughout this century, while scenario uncertainty becomes more important towards the end of the century. For the region as a whole, significant climate change (i.e., signal/noise >2) occurs earliest for summer mean temperature, with median time of emergence around 2035 for the RCP8.5 radiative forcing scenario. Although the median precipitation signal emerges from the noise (i.e., signal/noise >1) around the 2070s in winter and the 2080s in spring, significant values do not occur in any season for this variable before 2100. For summer CMI, the median time of emergence for significant change is around 2085. At the grid scale, signal‐to‐noise ratios are significant for all seasons for mean surface air temperature, with earliest times of emergence occurring in summer. In contrast, the summer precipitation signal is not significant this century; for summer CMI, significant values are obtained in the eastern half of the region, occurring from about 2065 onwards. Median times of emergence are towards the end of the century for summer CMI in western Saskatchewan and in Alberta, although some areas of Alberta do not exhibit significant signals this century. [ABSTRACT FROM AUTHOR]

Waterbird species face numerous threats and many are declining globally, but knowledge of distribution, abundance, and trend remains poor for many species. Five species of marsh-nesting colonial waterbirds are poorly monitored in Canada, and especially so in the core of their range in the Canadian Prairie Provinces (Alberta, Saskatchewan, and Manitoba). We summarized published and unpublished data on abundance and distribution of breeding colonies of Western Grebe (Aechmophorus occidentalis), Franklin's Gull (Leucophaeus pipixcan), Black Tern (Chlidonias niger), Forster's Tern (Sterna forsteri), and Black-crowned Night-Heron (Nycticorax nycticorax) in Alberta, Saskatchewan, and Manitoba. We also examined the degree of overlap in nesting phenology (egg dates) and summarized survey methods that have been used to monitor the species during the breeding season—information that may be useful for the development of a multispecies monitoring program. For all species, the largest number of records of breeding colonies occurred in Alberta, with records declining eastward through Saskatchewan and Manitoba. We identified a number of breeding colonies occurring outside of currently defined species ranges, especially for the poorly studied Forster's Tern. Of 137 waterbodies hosting a colony of at least one species over the past 10 yr, 57 (41.6%) hosted colonies of at least 2 species, and 3 (2.2%) hosted colonies of all 5 species. Species tended to be reasonably synchronous in their breeding phenology, but Franklin's Gulls and Black-crowned Night-Herons tended to initiate nesting slightly earlier than the other species. We conclude that a multispecies survey timed in late May or early June to count nests and/or incubating adults, using either ground-based or aerial surveys, would likely be the most appropriate for monitoring all species jointly in the Prairie Provinces. The approach we take to compiling data from multiple sources on species occurrence and breeding phenology may be applicable to others wishing to examine the feasibility of a multispecies monitoring plan. [ABSTRACT FROM AUTHOR]

Placement strategies for P fertilizer can affect P availability to crops and influence the amounts and forms of P removed from soil in runoff, contributing to eutrophication. On the Canadian prairies, most runoff occurs during snowmelt. Two adjacent farm fields in Saskatchewan, Canada, were used to assess the effects of spring P fertilizer placement on crop P uptake, residual soil P, and potential P export in simulated snowmelt. One was in conventional tillage (CT) with no history of P fertilization, and the other was in a no‐till (NT) system with multiyear P fertilization at recommended rates. Fertilization (monoammonium phosphate) treatments were no P fertilizer (control); seed placed, deep banded, and broadcast and incorporated at 20 kg P2O5 ha−1; and broadcast treatments at 20, 40, and 80 kg P2O5 ha−1. Yield and P uptake were not affected by placement method. Water‐extractable P at the soil surface after harvest was unaffected by placement or rate at either site but increased below the 5‐cm depth at the NT site in 2016. Broadcast treatments increased P in runoff relative to in‐soil P placement for the 20‐ and 80‐kg P2O5 ha−1 treatments at the CT site and for the 80‐kg P2O5 ha−1 treatment at the NT site. Thus, in‐soil application of P fertilizer appears to be an effective strategy to reduce the risk of P export in snowmelt runoff. Core Ideas: In‐soil fertilizer placement reduced P loss in snowmelt runoff from cropland.Broadcasting P fertilizer increased P loss in snowmelt runoff.Crop yield and P uptake were not affected by fertilizer placement method.Soil P was largely unaffected by placement over the 1 or 2 yr of the study. [ABSTRACT FROM AUTHOR]

Ken Wilson's 'Wood Mountain Walk: Afterthoughts on a Pilgrimage for Andrew Suknaski' reflects on a 250-kilometre walking pilgrimage made in honour of the late Canadian poet Andrew Suknaski. Wilson's autoethnographic essay considers the possibilities and challenges of walking as a way to engage with land and community; Suknaski's book Wood Mountain Poems and the issue of cultural appropriation; what it is like to walk in a sparsely populated and arid agricultural province where trespassing laws confine walkers to roads; and walking as both pilgrimage and artistic practice. [ABSTRACT FROM AUTHOR]

The North American prairie region is known for its poorly defined drainage system with numerous surface depressions that lead to variable contributing areas for streamflow generation. Current approaches of representing surface depressions are either simplistic or computationally demanding. In this study, a variable contributing area algorithm is implemented in the HYdrological Predictions for the Environment (HYPE) model and evaluated in the Canadian prairies. HYPE's local lake module is replaced with a Hysteretic Depressional Storage (HDS) algorithm to estimate the variable contributing fractions of subbasins. The modified model shows significant improvements in simulating the streamflows of two prairie basins in Saskatchewan, Canada. The modified model can replicate the hysteretic relationships between the water volume and contributing area of the basins. With the inclusion of the HDS algorithm in HYPE, the global HYPE modelling community can now simulate an important hydrological phenomenon, previously unavailable in the model. • HDS algorithm is implemented within the HYPE modelling framework. • HYPE-HDS shows significantly improved streamflow simulations compared to the original HYPE model. • HYPE-HDS can simulate the hysteretic relationship between depressional/basin storage and contributing area. [ABSTRACT FROM AUTHOR]

In semiarid and sub-humid Saskatchewan, Canada, there is growing interest in draining depressional areas within the landscape (prairie potholes) despite a clear understanding of the potential nutrient loss to nearby water sources. Nutrient fate and form can vary greatly depending on soil moisture regime; the aim of this study was to determine how drainage duration affects the nitrogen (n) and phosphorus (p) availability and mobility under varying moisture levels. A greenhouse experiment was conducted using four depressional soils from south-eastern Saskatchewan, which had been drained for 0, 14, 20, and 42 yr, and one undrained midslope soil for comparison. The potted soils were seeded with wheat (Triticum aestivum L.), three different moisture scenarios applied, and leachate was collected weekly. Drained soils had greater aboveground biomass and N and p plant uptake compared with undrained soil. These differences were most pronounced in the 20 yr drained soil, which had a 30% increase in growth, 45% greater N uptake, and 62% greater p uptake than the undrained soil. Nitrogen mineralization and water holding capacity appeared to affect nutrient losses. The soil that contributed the most to nutrient losses varied under different moisture scenarios; low water holding capacity contributed to nutrient leaching under lower moisture scenarios, whereas enhanced mineralization increased losses under above-average moisture. [ABSTRACT FROM AUTHOR]

Hydrological water balance closure is a simple concept, yet in practice it is uncommon to measure every significant term independently in the field. Here we demonstrate the degree to which the field-scale water balance can be closed using only routine field observations in a seasonally frozen prairie pasture field site in Saskatchewan, Canada. Arrays of snow and soil moisture measurements were combined with a precipitation gauge and flux tower evapotranspiration estimates. We consider three hydrologically distinct periods: the snow accumulation period over the winter, the snowmelt period in spring, and the summer growing season. In each period, we attempt to quantify the residual between net precipitation (precipitation minus evaporation) and the change in field-scale storage (snow and soil moisture), while accounting for measurement uncertainties. When the residual is negligible, a simple 1-D water balance with no net drainage is adequate. When the residual is non-negligible, we must find additional processes to explain the result. We identify the hydrological fluxes which confound the 1-D water balance assumptions during different periods of the year, notably blowing snow and frozen soil moisture redistribution during the snow accumulation period, and snowmelt runoff and soil drainage during the melt period. Challenges associated with quantifying these processes, as well as uncertainties in the measurable quantities, caution against the common use of water balance residuals to estimate fluxes and constrain models in such a complex environment. [ABSTRACT FROM AUTHOR]

Understanding the catchment areas of key stopover sites for migratory birds is important for their management and conservation. The Saskatchewan River Delta (SRD) in central Canada is North America's largest inland delta and an important spring and fall stopover site for migratory waterfowl, but there is little information on the origins of waterfowl that use the SRD. We used stable isotope analyses of hydrogen (δ²H) and sulfur (δ34S) in feathers of hunter-killed waterfowl on the SRD to infer natal or molt origins of 5 duck species, using spatially explicit assignment to a δ²H feather isoscape developed for waterfowl in North America. Initial classification with δ²H estimated that 50% were migrants from the north and 10% were assigned to regions south of the SRD, leaving only 39% of the sample with origins in the SRD. Using thresholds in feather δ34S values associated with prairie and forest biomes, we further reassigned 64% of SRD birds as having originated from nearby agricultural and forested areas that have similar δ²H values as the delta. Together, these results suggest that >80% of all waterfowl sampled were recent arrivals that were using the SRD as a stopover site. This demonstrates that stable isotope analyses of hunter-killed birds can be used to monitor changes in origins and recruitment into the fall waterfowl population of key stopover sites. [ABSTRACT FROM AUTHOR]

• Drought response of three disparate shelterbelt species is explored. • Severe and extreme 3-month droughts most greatly affect tree. • Scots pine and white spruce recover more quickly than green ash. Across western Canada, more frequent and severe droughts are expected to occur as a result of climate change. Forests are particularly vulnerable to drought as it often results in mortality events even years following a moisture deficit. Similar events have been observed in Saskatchewan shelterbelts, where many species are planted far outside their native range and are likely more vulnerable to environmental changes. Understanding how common shelterbelt species respond to drought will help landowners make better management decisions under a changing climate. This study looks at how three common shelterbelt species (green ash, Scots pine and white spruce) respond to different drought characteristics (severity, timing, and length) for up to five years following a moisture deficit using superposed epoch analysis. We identified that severe and extreme 3-month droughts greatly impact all three species. However, Scots pine and white spruce tend to recover more rapidly than green ash. Green ash is typically considered one of the most drought tolerant shelterbelt species, but its long recovery times suggest that this may be false. Scots pine was impacted by late summer droughts and white spruce was impacted by June droughts. Both Scots pine and white spruce also saw compensatory growth after their recovery period. This research augments our understanding of how drought characteristics impact three common shelterbelt species in Saskatchewan and how they are likely to recover under more frequent and severe drought events given projected climate change. [ABSTRACT FROM AUTHOR]

The Saskatchewan River Basin (SRB) is a vital and essential resource for the three Canadian prairie provinces of Alberta, Saskatchewan and Manitoba. The cumulative impacts of past and future development combined with the realities of climate change raise new questions about the current regime of water governance in the region. At present, multiple agencies affect different aspects of water governance across the SRB. This study is a preliminary assessment, based on key informant interviews, of existing water governance efficacy in the SRB. Using a range of probing questions, key informant perceptions regarding the strengths, weaknesses, and opportunities respecting water governance in the SRB are uncovered. The findings of this study suggest that the advantages of the current fragmented, multiagency regime of water governance in the SRB are outnumbered by the disadvantages. [ABSTRACT FROM AUTHOR]