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dc.contributor.authorTape, Ken
dc.date.accessioned2015-02-24T19:55:04Z
dc.date.available2015-02-24T19:55:04Z
dc.date.issued2004-12
dc.identifier.urihttp://hdl.handle.net/11122/5004
dc.descriptionThesis (M.S.) University of Alaska Fairbanks, 2004en_US
dc.description.abstractEvidence from arctic Alaska suggests that the terrestrial landscape is changing in response to warming. Between 1946 and 1951, several thousand low-altitude panchromatic oblique aerial photographs were taken as part of geologic reconnaissance and exploration of Alaska's Arctic Slope and Brooks Range. For this study, 202 of the landscapes in the old photographs were re-photographed. Comparison of the old and new photographs revealed an increase in shrub cover in the last half-century. The changes were observed over a 220,000 km2 tract of arctic tundra, and it is likely that they are more widespread. A quantitative method for comparing the photographs yielded an increase in alder shrub cover from 14 to 20%, with similar increases observed for willow and birch shrubs. This shrub expansion was observed in many landscape positions, including hill slopes, river terraces, and also river floodplains, where the increase in shrub vegetation has resulted in the narrowing and stabilization of floodplains. The regional expansion of shrubs documented in the photographs can only be explained by a perturbation operating on a similarly large scale. In the absence of large-scale disturbances like fire, the increase in shrubs documented here is most likely to be a product of elevated temperatures and other changes in climate favorable to shrub growth.en_US
dc.language.isoen_USen_US
dc.titleShrub expansion in Arctic Alaska: 50 years of change documented using aerial photographyen_US
dc.typeThesisen_US
dc.type.degreemsen_US
dc.identifier.departmentDepartment of Geology and Geophysics
dc.contributor.chairLi, Shusun
dc.contributor.chairSturm, Matthew
dc.contributor.committeeChapin, F. Stuart III
dc.contributor.committeeRomanovski, Vladimir
refterms.dateFOA2020-03-20T01:08:25Z


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