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THESIS APPROVAL The abstract and thesis of Thomas H. Nylen for the Master of Science in Geology presented October 25, 2001, and accepted by the thesis committee and the department. COMMITTEE APPROVALS: _______________________________________ Andrew G. Fountain, Chair _______________________________________ Scott F. Burns _______________________________________ Christina L. Hulbe _______________________________________ Keith S. Hadley Representative of the Office of Graduate Studies DEPARTMENTAL APPROVAL: _______________________________________ Michael L. Cummings, Chair Department of Geology ABSTRACT An abstract of the thesis of Thomas H. Nylen for the Master of Science in Geology presented October 25, 2001. Title: Spatial and Temporal Variations of Glaciers (1913-1994) on Mt. Rainier and the Relation with Climate Databases have been constructed for the purpose of studying glacier changes at Mt. Rainier. Glacier cover on Mt. Rainier decreased 18.5% (112.3 km2 to 88.1 km2) between 1913 and 1971 at a rate of about -0.36 km2 a-1. The total area in 1994 was 87.4 km2, which equates to a rate of -0.03 km2 a-1 since 1971. Glaciers with southerly aspect lost significantly more area than those with a northerly aspect, 26.5% and 17.5% of the total area, respectively. Measured and estimated total volumes for Mt. Rainier glaciers also decreased. From 1913 to 1971 the total volume decreased 22.7% from 5.62 km3 to 4.34 km3 and from 1971 to 1994 decreased 3.1% to 4.21 km3. Nisqually Glacier shows three cycles of retreat and advance but an overall loss of 0.44 km2 since 1931. Cross-correlation with snowfall suggests about a decade response time for the glaciers. The pattern of terminus change through this century has been consistent between the glaciers. Between 1913 and the late 1950s, the major glaciers were retreating, with an average retreat of 1,318 m. Following this period and up to the early 1980s the glaciers advanced an average distance of 390 m. Since 1980, the terminus positions of all but three glaciers, Emmons, Winthrop and Cowlitz, retreated. Though the response has been similar, spatial variations exit in the magnitude of response. Southern glaciers, which are on average smaller decreased in area, volume and length more than the northern glaciers. The northern glaciers decreased in area by 17.5%, while the southern glaciers decreased by 26.5%. As for the terminus positions, the southern glaciers retreated on average 1,957 m, which is approximately three times as far as the average for the northern glaciers. The spatial variations in area and volume of the glaciers are caused primarily by differences in incoming solar radiation, size and elevation range. With more solar radiation the southern glaciers have smaller mass balances and over time cause spatial differences in the size of the glaciers. Smaller glaciers appear to be more sensitive to climate changes than larger glaciers because they have smaller elevation ranges. SPATIAL AND TEMPORAL VARIATIONS OF GLACIERS (1913-1994) ON MT. RAINIER AND THE RELATION WITH CLIMATE by THOMAS H. NYLEN A thesis submitted in partial fulfillment of the requirements for the degree of MASTER OF SCIENCE in GEOLOGY Portland State University 2004 i Acknowledgments This project was supported by research grants from the US National Park Service (Mt. Rainier National Park). Special thanks go to my thesis advisor Andrew G. Fountain and the other members of the thesis committee Scott Burns, Christina L. Hulbe, and Keith S. Hadley for their guidance. Additional thanks go to Barbara Samora and Darin Swinney (Mt. Rainier National Park), and Carolyn Driedger (Cascade Volcanic Observatory). ii Table of Contents Acknowledgments ..........................................................................................................i List of Figures...............................................................................................................iv List of Tables..............................................................................................................viii I. Introduction ...........................................................................................................1 II. Study Site...............................................................................................................6 A. General Description........................................................................................6 B. Prior Research ................................................................................................8 III. Glaciers................................................................................................................12 A. Sources and Methods....................................................................................12 1. Data Source and Description..................................................................12 2. Data Conversion.....................................................................................15 3. Measurements.........................................................................................18 4. Errors Estimates......................................................................................20 B. Results ..........................................................................................................24 1. Terminus Changes..................................................................................24 2. Glacial Area............................................................................................37 3. Debris Area.............................................................................................43 4. Volume Changes....................................................................................45 IV. Climate ................................................................................................................50 A. Introduction ..................................................................................................50 B. Regional Climate..........................................................................................50 C. Source and Methods .....................................................................................53 1. Meteorological Data ...............................................................................53 2. Solar Radiation Modeling.......................................................................55 3. Cloud Cover............................................................................................56 D. Results ..........................................................................................................59 1. Meteorological Measurements ...............................................................59 2. Incoming solar radiation modeling.........................................................68 iii 3. Cloud Cover............................................................................................69 V. Comparison of Glacier Response to Climate Variations.....................................70 VI. Discussion............................................................................................................76 VII. Conclusions .........................................................................................................87 VIII. References ...........................................................................................................90 Appendix A: Measured terminus position changes..................................................105 Appendix B: Winter (October to April) Precipitation Totals...................................107 Appendix C: Winter (October to April) Snowfall Totals.........................................109 Appendix D: Summer (May to September) Temperature Totals .............................111 Appendix E: Percentage area-altitude distribution per 100 meters of elevation ......113 iv List of Figures Figure 1: Mt. Rainier glaciers and insert map showing location (Topinka, 1997)........6 Figure 2: Features digitized on the glaciers.................................................................17 Figure 3: Approximate centerline (thicker line) of Emmons Glacier used to measure length changes between different terminus positions. Former positions are denoted by the thinner lines and years..................................................................19 Figure 4: Plot of the uncertainty in glacier area versus the perimeter of nine glaciers from the 1913 map................................................................................................23 Figure 5: Cumulative terminus changes for Carbon Glacier between 1913 and 1994. ..............................................................................................................................25 Figure 6: Cumulative terminus changes for Cowlitz Glacier between 1913 and 1994 ..............................................................................................................................26 Figure 7: Cumulative terminus changes for Emmons Glacier between 1913 and 1994 ..............................................................................................................................27 Figure 8: Cumulative terminus changes on Nisqually Glacier between 1913 and 1994 ..............................................................................................................................28 Figure 9: Adjusted version of the cumulative terminus changes on Nisqually Glacier between 1913 and 1994 ........................................................................................30
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