51 research outputs found

    G. E. LEVY , ed. — The Diary of Joseph Dimock.

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    The Writing of State Histories

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    Nova Scotia's Sense of Mission

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    Local capacity to implement a source water protection plan in the South Saskatchewan River watershed

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    Following a number of waterborne disease outbreaks in Canada, the water resource management literature draws attention to source water protection (SWP). Source water protection is a drinking water management approach that attempts to improve drinking water quality by preventing contamination of untreated water at the source. The literature has identified methods for SWP planning; however, rates of implementation of SWP plans are variable and dependent on local capacity factors. Through key informant interviews, this study identifies factors that facilitate and constrain local capacity for implementation of a source water protection plan in the South Saskatchewan River watershed. Results are discussed according to four capacity areas for SWP: technical, institutional, financial, and social capacity. The results of this study show that capacity areas in need of improvement include access to data, training and educational opportunities for non-governmental organizations, greater enforcement of government legislation and regulations, financial security, community awareness and greater linkages and networks between organizations with similar objectives. Respondents identified adequate stakeholder involvement in the planning process, access to funding, and reliable information as examples of existing capacity. The results of this research contribute to the understanding of SWP plan implementation at the watershed scale in Canada and beyond

    A Synoptic Scale Meteorological Investigation of Springtime Frost Incidence in Cromwell

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    The onset of a frost can cause millions of dollars of lost profit due to damage to the grapevine buds utilized for the production of world class wines. The aim of this thesis is to assess the synoptic controls on springtime frost incidence in the complex terrain of Cromwell, Central Otago, New Zealand/Aotearoa (45.03°S and 169.20°E). The main research objectives of the research are to (1) identify a statistically significant synoptic signal that leads to springtime frost incidence using synoptic weather types and (2) to investigate the meteorological variables associated with specific synoptic weather types to separate a frost event from a non-frost event. An understanding of the relationships between synoptic weather types and the incidence of frost is desirable because of the practical, operational, and economic implications that frost incidence poses in this region. The implications are particularly important given that there is an acknowledged increase in the synoptic types (anticyclones) over New Zealand that are associated with the incidence of frost. Kidson types were temporally aligned with a historical weather dataset from NIWA’s CliFLo network (1950 - 2017) in such a manner that each frost or non-frost in the Austral spring (September, October, and November) were preceded by preceding noon Kidson type (PNKT) and midnight Kidson type (MKT). The model utilized was classified as being an excellent predictor given the metric of the receiver operator curve (ROC- score of 80.4%). The top ten most probable Kidson transitions were characterized by southwesterly winds (HW, SW, TSW Kidson types) at noon. The most probable midnight Kidson types to render a frost are characterized by anticyclonic activity (HW, HSE, R, NE). On the contrary, the ten least likely Kidson transitions to render a frost are those that are characterized by either noontime westerlies (H, W) or noontime northerly quarter winds (TNW, HE). Following this, the most probable midnight Kidson types to render a non-frost are characterized by being part of the trough (T, TSW, TNW) or zonal regime (W). The ERA-Interim reanalysis dataset was used to investigate the meteorological variables (mean sea level pressure (MSLP), MSLP anomalies, wind speed and direction, total column water (TCW) anomalies, and relative humidity (RH)) that separate a frost event from a non frost event, thereby achieving objective 2. Frost events are consistently characterized by higher pressures than that of non-frost events with regards to both MSLP and MSLP anomalies. Frosts are consistently characterized by less atmospheric moisture in both absolute and relative metrics (negative TCW anomalies, and lower RH values) when compared to non-frost events. With regards to wind, windspeeds are consistently lower within the interior of the South Island, and the incident synoptic winds are more meridional/southerly during fros events than non-frosts. The statistical link between the incidence of frost and synoptic types in this study was achieved in complex terrain, suggesting that it successfully captured the local response (particularly katabatic drainage winds) to synoptic processes with regards to the incidence of frost, and may have potential for utilization elsewhere in New Zealand. The climate reanalysis component of this study proved to be effective, as it was able to discern the meteorological variables that are influential on the incidence of frost. Thus, it is concluded that this thesis makes a significant contribution towards developing an understanding that leads to springtime frost incidence in Cromwell, and provides a means to differentiate the controlling factors on such events

    A Synoptic Scale Meteorological Investigation of Springtime Frost Incidence in Cromwell

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    The onset of a frost can cause millions of dollars of lost profit due to damage to the grapevine buds utilized for the production of world class wines. The aim of this thesis is to assess the synoptic controls on springtime frost incidence in the complex terrain of Cromwell, Central Otago, New Zealand/Aotearoa (45.03°S and 169.20°E). The main research objectives of the research are to (1) identify a statistically significant synoptic signal that leads to springtime frost incidence using synoptic weather types and (2) to investigate the meteorological variables associated with specific synoptic weather types to separate a frost event from a non-frost event. An understanding of the relationships between synoptic weather types and the incidence of frost is desirable because of the practical, operational, and economic implications that frost incidence poses in this region. The implications are particularly important given that there is an acknowledged increase in the synoptic types (anticyclones) over New Zealand that are associated with the incidence of frost. Kidson types were temporally aligned with a historical weather dataset from NIWA’s CliFLo network (1950 - 2017) in such a manner that each frost or non-frost in the Austral spring (September, October, and November) were preceded by preceding noon Kidson type (PNKT) and midnight Kidson type (MKT). The model utilized was classified as being an excellent predictor given the metric of the receiver operator curve (ROC- score of 80.4%). The top ten most probable Kidson transitions were characterized by southwesterly winds (HW, SW, TSW Kidson types) at noon. The most probable midnight Kidson types to render a frost are characterized by anticyclonic activity (HW, HSE, R, NE). On the contrary, the ten least likely Kidson transitions to render a frost are those that are characterized by either noontime westerlies (H, W) or noontime northerly quarter winds (TNW, HE). Following this, the most probable midnight Kidson types to render a non-frost are characterized by being part of the trough (T, TSW, TNW) or zonal regime (W). The ERA-Interim reanalysis dataset was used to investigate the meteorological variables (mean sea level pressure (MSLP), MSLP anomalies, wind speed and direction, total column water (TCW) anomalies, and relative humidity (RH)) that separate a frost event from a non frost event, thereby achieving objective 2. Frost events are consistently characterized by higher pressures than that of non-frost events with regards to both MSLP and MSLP anomalies. Frosts are consistently characterized by less atmospheric moisture in both absolute and relative metrics (negative TCW anomalies, and lower RH values) when compared to non-frost events. With regards to wind, windspeeds are consistently lower within the interior of the South Island, and the incident synoptic winds are more meridional/southerly during fros events than non-frosts. The statistical link between the incidence of frost and synoptic types in this study was achieved in complex terrain, suggesting that it successfully captured the local response (particularly katabatic drainage winds) to synoptic processes with regards to the incidence of frost, and may have potential for utilization elsewhere in New Zealand. The climate reanalysis component of this study proved to be effective, as it was able to discern the meteorological variables that are influential on the incidence of frost. Thus, it is concluded that this thesis makes a significant contribution towards developing an understanding that leads to springtime frost incidence in Cromwell, and provides a means to differentiate the controlling factors on such events

    Mary Rawlyk : The Apron Show

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    Farr views Rawlyk's apron prints as ridiculing the notion of glamour in women's household labour. Artist's statement. Biographical notes

    Delivery of Special Education Services in Saskatchewan

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    118 p.Thesis (Ph.D.)--University of Illinois at Urbana-Champaign, 1974.U of I OnlyRestricted to the U of I community idenfinitely during batch ingest of legacy ETD
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