Incorporation of non-stationary landcover into WATFLOOD climate change scenarios

dc.contributor.authorWruth, Shane
dc.contributor.examiningcommitteeAli, Genevieve (Geological Sciences) Rasmussen, Peter (Civil Engineering) Koenig, Kristina (Manitoba Hydro)en_US
dc.contributor.supervisorStadnyk, Tricia (Civil Engineering)en_US
dc.date.accessioned2014-01-14T14:31:54Z
dc.date.available2014-01-14T14:31:54Z
dc.date.issued2014-01-14
dc.degree.disciplineCivil Engineeringen_US
dc.degree.levelMaster of Science (M.Sc.)en_US
dc.description.abstractIn this thesis, a landcover simulator module is developed to incorporate non-stationary landcover into the hydrological model WATFLOOD. Objectives are to quantify the uncertainty inherent in assuming landcover stationarity in the Winnipeg River basin (WRB), and to improve the projections of future streamflow. Forest fires commonplace in the WRB are modelled through logistic regression and a generalized extreme value distribution for occurrence and extent respectively, fit from historical data. Fire regeneration and natural changes in landcover are modelled though a first order Markov chain, with transition probabilities derived from satellite imagery. Using satellite imagery directly into historical simulations in a sub-basin with substantial forest fire activity improved WATFLOOD results. With climate change, incorporating non-stationary landcover results in lower flows than assuming stationarity, albeit still greater than baseline (1971 - 2000) flows. Projected streamflow uncertainty under climate change also increases as a result of introducing non-stationary landcover in the WRB.en_US
dc.description.noteFebruary 2014en_US
dc.identifier.urihttp://hdl.handle.net/1993/23208
dc.language.isoengen_US
dc.rightsopen accessen_US
dc.subjectnon-stationaryen_US
dc.subjectlandcoveren_US
dc.titleIncorporation of non-stationary landcover into WATFLOOD climate change scenariosen_US
dc.typemaster thesisen_US
local.subject.manitobayesen_US
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