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dc.contributor.advisorChairperson, Graduate Committee: Alexander V. Zaleen
dc.contributor.authorVatland, Shane Jeffreyen
dc.contributor.otherRobert E. Gresswell and Geoffrey C. Poole were co-authors of the article, 'Quantifying stream thermal regimes at management-pertinent scales: combining thermal infrared and stationary stream temperature data in a novel modeling framework' in the journal 'Water resources research' which is contained within this thesis.en
dc.contributor.otherRobert E. Gresswell, Steve Hostetler and Alexander V. Zale were co-authors of the article, 'Effects of climate change on the thermal habitats of arctic grayling and non-native stream salmonids' submitted to the journal 'Global change biology' which is contained within this thesis.en
dc.coverage.spatialBig Hole River (Mont.)en
dc.date.accessioned2016-06-28T20:33:17Z
dc.date.available2016-06-28T20:33:17Z
dc.date.issued2015en
dc.identifier.urihttps://scholarworks.montana.edu/xmlui/handle/1/9460en
dc.description.abstractThe upper Big Hole River basin in southwestern Montana supports one of the last naturally-reproducing populations of fluvial Arctic grayling Thymallus arcticus in the coterminous United States. Warm summer water temperatures and negative interactions with non-native fish (brook trout Salvelinus fontinalis, rainbow trout Oncorhynchus mykiss, and brown trout Salmo trutta) have been identified as critical factors constraining this grayling population. Arctic grayling and these non-native fishes are all cold-water species with similar temperature requirements. Understanding when, where, and to what extent water temperatures are suitable for these fishes provides a physical basis for conservation planning. In chapter 2, I used a combination of thermal infrared (TIR) imagery and stationary temperature recorders to estimate water temperatures at a relatively fine spatial (every ~ 100 m of stream length) and temporal (continuous) resolution over a large extent of the Big Hole River (~ 100 km) during the warmest part of the summer in 2008. This modeling revealed considerable spatial and temporal heterogeneity in water temperature and highlighted the value of assessing thermal regimes at relatively fine spatial and temporal scales. In chapter 3, I assessed the potential effects of climate change on thermal suitability of summer water temperatures for these salmonids. Water temperature simulations projected significant warming from the 1980s through the 2060s. Despite this warming, water temperatures in some sections of stream remained below thermal tolerance thresholds through the 2060s. These stream temperature data provide a critical foundation for understanding the dynamic, multiscale habitat needs of these mobile stream fish and can aid in developing conservation strategies for fluvial Arctic grayling.en
dc.language.isoenen
dc.publisherMontana State University - Bozeman, College of Letters & Scienceen
dc.subject.lcshSalmonidaeen
dc.subject.lcshWater temperatureen
dc.subject.lcshClimatic changesen
dc.titleEffects of stream temperature and climate change on fluvial arctic grayling and non-native salmonids in the upper Big Hole River, Montanaen
dc.typeDissertationen
dc.rights.holderCopyright 2015 by Shane Jeffrey Vatlanden
thesis.catalog.ckey3094707en
thesis.degree.committeemembersMembers, Graduate Committee: Robert E. Gresswell; Wyatt F. Cross; Jeff Kershneren
thesis.degree.departmentEcology.en
thesis.degree.genreDissertationen
thesis.degree.namePhDen
thesis.format.extentfirstpage1en
thesis.format.extentlastpage119en
mus.data.thumbpage125en


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