The vast majority of theses in this collection are open access and freely available. There are a small number of theses that have access restricted to the WWU campus. For off-campus access to a thesis labeled "Campus Only Access," please log in here with your WWU universal ID, or talk to your librarian about requesting the restricted thesis through interlibrary loan.
Date Permissions Signed
5-12-2016
Date of Award
Spring 2016
Document Type
Masters Thesis
Degree Name
Master of Science (MS)
Department
Environmental Sciences
First Advisor
Bunn, Andrew Godard
Second Advisor
Flower, Aquila
Third Advisor
Wallin, David O.
Abstract
Great Basin bristlecone pine (Pinus longaeva) and foxtail pine (Pinus balfouriana) are valuable paleoclimate resources due to the climatic sensitivity of their annually-resolved rings. Recent treeline research has shown that growing season temperatures limit tree growth at and just below the upper treeline. In the Great Basin, the presence of precisely dated remnant wood above modern treeline shows that this ecotone shifts at centennial timescales tracking long-term changes in climate; in some areas during the Holocene climatic optimum treeline was 100 meters higher than at present. Such phenomena has motivated this analysis; regional treeline position models built exclusively from climate data may identify characteristics specific to Great Basin treelines and inform future physiological studies, and provide a measure of climate sensitivity specific to bristlecone and foxtail pine treelines. This study implements a topoclimatic analysis—using topographic position to explain patterns in surface temperatures across complex mountainous terrain—to model treeline position of three semi-arid bristlecone and/or foxtail pine treelines in the Great Basin as a function of topographically modified climate variables calculated from in situ measurements. Results indicate: (1) the treelines used in this study require a growing season length of between 143 - 152 days and average temperature ranging from 5.5 - 7.6 °C, (2) site-specific treeline position models may be improved through topoclimatic analysis—specifically the inclusion of an integrated measure of climate rather than a growing season isotherm measured in degrees, (3) treeline position in the Great Basin is likely out of equilibrium with the current climate indicating a potential shift in the primary growth-limiting factor at the highest elevations where trees are found.
Type
Text
DOI
https://doi.org/10.25710/qbdk-4h40
Publisher
Western Washington University
OCLC Number
949905654
Subject – LCSH
Great Basin bristlecone pine--Southwest, New; Foxtail pine--Southwest, New; Topoclimatology--Southwest, New--Analysis; Timberline--Climatic factors--Southwest, New; Ecotones--Climatic factors--Southwest, New
Geographic Coverage
Southwest, New
Format
application/pdf
Genre/Form
masters theses
Language
English
Rights
Copying of this document in whole or in part is allowable only for scholarly purposes. It is understood, however, that any copying or publication of this thesis for commercial purposes, or for financial gain, shall not be allowed without the author's written permission.
Recommended Citation
Bruening, Jamis M., "Fine-scale Topoclimate Modeling and Climatic Treeline Prediction of Great Basin Bristlecone Pine (Pinus longaeva) in the American Southwest" (2016). WWU Graduate School Collection. 488.
https://cedar.wwu.edu/wwuet/488