{"id":{"repo_id":"royalroads","oai_identifier":"oai:null:10170/486"},"canonical_url":"https://search.dev.ndltd.org/etd/royalroads/oai:null:10170/486","repository":{"repo_id":"royalroads","name":"Royal Roads University","base_url":"https://www.viurrspace.ca/server/oai/request"},"display":{"title":"Changes in the annual average temperature, flow rates and flood probability in Prince George, British Columbia","abstract":"Three key questions are identified and answered in this paper. Firstly, have the average annual temperatures in the Prince George Region changed in recent years? Secondly, have the seasonal flow rates changed for local waterways? Lastly, have the timing of the annual flood cycles in the Prince George, British Columbia changed? By reviewing data from local weather and hydrological monitoring stations, this paper identifies that the average annual temperature in Prince George, British Columbia has not only increased but also shifted to a pattern of warmer winters and cooler summers. The flow rates for the region were seen to have been altered as well, indicating increased flow rates in the winter and early spring and decreased flow rates in the summer and early fall. The magnitude of flood frequency events such as the 10, 25 and 100 year flood occurrence does not seem to have the increased in recent years.","abstract_html":"Three key questions are identified and answered in this paper. Firstly, have the average annual temperatures in the Prince George Region changed in recent years? Secondly, have the seasonal flow rates changed for local waterways? Lastly, have the timing of the annual flood cycles in the Prince George, British Columbia changed? By reviewing data from local weather and hydrological monitoring stations, this paper identifies that the average annual temperature in Prince George, British Columbia has not only increased but also shifted to a pattern of warmer winters and cooler summers. The flow rates for the region were seen to have been altered as well, indicating increased flow rates in the winter and early spring and decreased flow rates in the summer and early fall. The magnitude of flood frequency events such as the 10, 25 and 100 year flood occurrence does not seem to have the increased in recent years.","abstract_has_math":false,"creators":["Beckett, Matthew Campbell"],"institution":null,"degree_name":null,"degree_level":null,"degree_discipline":null,"degree_department":null,"school":null,"contributors":[],"advisors":["Ward, Peter","Noble, Michael-Anne"],"committee_chairs":[],"committee_members":[],"year":2012,"date_issued":"2012-04-25","date_published":"2012-04-25","updated_at":"2026-08-21T22:21:56Z","subjects":["Seasonal Flow Rates","Annual Flood Cycles","Average Annual Temperatures"],"languages":[],"rights":[],"rights_urls":[],"identifier_entries":[]},"links":{"outbound_url":"http://hdl.handle.net/10170/486","outbound_label":"Handle","outbound_source":"dc:identifier.uri"},"source_record":{"url":"https://www.viurrspace.ca/server/oai/request?verb=GetRecord&metadataPrefix=dim&identifier=oai%3Anull%3A10170%2F486","prefix":"dim"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:contributor.advisor","label":"Advisor","values":["Ward, Peter","Noble, Michael-Anne"]},{"key":"dc:creator","label":"Author","values":["Beckett, Matthew Campbell"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date.accessioned","label":"Dc Date Accessioned","values":["2012-04-25T22:30:44Z"]},{"key":"dc:date.available","label":"Dc Date Available","values":["2012-04-25T22:30:44Z"]},{"key":"dc:date.issued","label":"Date","values":["2012-04-25"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["Seasonal Flow Rates","Annual Flood Cycles","Average Annual Temperatures"]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier.uri","label":"Identifier URI","values":["http://hdl.handle.net/10170/486"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description.abstract","label":"Abstract","values":["Three key questions are identified and answered in this paper. Firstly, have the average annual temperatures in the Prince George Region changed in recent years? Secondly, have the seasonal flow rates changed for local waterways? Lastly, have the timing of the annual flood cycles in the Prince George, British Columbia changed? By reviewing data from local weather and hydrological monitoring stations, this paper identifies that the average annual temperature in Prince George, British Columbia has not only increased but also shifted to a pattern of warmer winters and cooler summers. The flow rates for the region were seen to have been altered as well, indicating increased flow rates in the winter and early spring and decreased flow rates in the summer and early fall. The magnitude of flood frequency events such as the 10, 25 and 100 year flood occurrence does not seem to have the increased in recent years."]},{"key":"dc:title","label":"Title","values":["Changes in the annual average temperature, flow rates and flood probability in Prince George, British Columbia"]}]}],"canonical_facts":{"dc:contributor.advisor":["Ward, Peter","Noble, Michael-Anne"],"dc:creator":["Beckett, Matthew Campbell"],"dc:date.accessioned":["2012-04-25T22:30:44Z"],"dc:date.available":["2012-04-25T22:30:44Z"],"dc:date.issued":["2012-04-25"],"dc:description.abstract":["Three key questions are identified and answered in this paper. Firstly, have the average annual temperatures in the Prince George Region changed in recent years? Secondly, have the seasonal flow rates changed for local waterways? Lastly, have the timing of the annual flood cycles in the Prince George, British Columbia changed? By reviewing data from local weather and hydrological monitoring stations, this paper identifies that the average annual temperature in Prince George, British Columbia has not only increased but also shifted to a pattern of warmer winters and cooler summers. The flow rates for the region were seen to have been altered as well, indicating increased flow rates in the winter and early spring and decreased flow rates in the summer and early fall. The magnitude of flood frequency events such as the 10, 25 and 100 year flood occurrence does not seem to have the increased in recent years."],"dc:identifier.uri":["http://hdl.handle.net/10170/486"],"dc:subject":["Seasonal Flow Rates","Annual Flood Cycles","Average Annual Temperatures"],"dc:title":["Changes in the annual average temperature, flow rates and flood probability in Prince George, British Columbia"]},"updated_at":"2026-08-21T22:21:56Z"}