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intitle:
The document title intitle:"climate education"
ispublisher:
The publishing organization ispublisher:CAPE
insummary:
Summary and key findings insummary:"conflict of interest"
hasconcept:
Climate tags, frame/perspective and analysis type hasconcept:"Climate Justice"
geography:
Regions the document covers or discusses geography:Canada
doctype:
Document type doctype:report
lang:
Document language, as an ISO code lang:fr
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One record, by its directory id cidid:iisd-000297
GeographyWinnipeg River basin
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  • The document discusses the use of high-frequency, networked water quality monitoring systems to improve data-driven decision making for watershed protection, specifically within the context of a pilot project in the Winnipeg River basin. While these systems provide larger volumes of near real-time data to address threats from climate change and pollution, they also introduce new technical, financial, and labour requirements.

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  • The report examines how high-frequency, real-time water quality monitoring can improve watershed management and decision-making, particularly in the Winnipeg River basin. It contrasts the advantages of automated sensors—such as rapid response to contamination and lower long-term cost per measurement—with limitations including sensor drift, maintenance costs, and data management burdens. Through case studies at the Powerview-Pine Falls drinking water facility and Lake 227, the document demonstrates the utility of real-time data for optimizing water treatment and tracking algal bloom dynamics.

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  • The document is a map-based fact sheet detailing the geographic, ecological, and socio-economic characteristics of the lower Winnipeg River basin (LWRB) and the broader Winnipeg River basin (WRB) in Manitoba, Ontario, and Minnesota. It includes data on land cover, surficial geology, zoning policies, Indigenous presence, and drinking water advisories.

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  • The lower Winnipeg River basin (LWRB) is characterized by a mean annual discharge of 1,008 ± 294 m3/s at the Pine Falls Generating system, with peaks typically occurring in June and July. The river is a critical contributor to Lake Winnipeg, accounting for 49% of the mean monthly discharge of all rivers and streams entering the lake and providing the largest volume of water to it. Six run-of-river hydroelectric stations in the LWRB generate 583 MW of electrical capacity, representing approximately 10% of Manitoba's energy needs. Climate projections for the 2050s suggest a 6.9% increase in mean annual precipitation and a 3.3% increase in runoff, which may impact downstream nutrient loading. While water levels at most hydrometric stations remain relatively constant, Nutimik Lake shows seasonal trends.

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  • The lower Winnipeg River basin (LWRB) is a sparsely populated area characterized by low population density and significant seasonal population fluctuations due to cottage developments. Between 2011 and 2016, the population across six census subdivisions grew by 4%, from 11,839 to 12,292. While towns like Pinawa, Lac du Bonnet, and Powerview-Pine Falls have high occupancy rates for usual residents, rural municipalities like Alexander and Lac du Bonnet have less than half of their dwellings occupied by permanent residents. The region has a strong Indigenous presence, including the Fort Alexander First Nation/Sagkeeng Anicinabe and Métis people, who traditionally use the land and water for harvesting and spiritual activities.

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  • The document describes the humid continental climate of the lower Winnipeg River basin and details historical increases in river discharge. It presents climate projections for the 2050s, indicating rising temperatures, precipitation, and runoff, which may impact hydroelectric development and aquatic ecosystems.

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  • The document identifies the lower Winnipeg River basin (LWRB) as being at high risk for the transport of aquatic invasive species (AIS) due to recreational activities. While spiny waterflea is confirmed in the LWRB, other high-concern species like zebra mussels and rusty crayfish are present in the wider Winnipeg River basin but not the lower basin. The basin is noted to have moderate suitability for zebra mussel colonization based on calcium concentrations.

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