Physical Sciences and Mathematics Commons^™

The Photochemical Evolution Of Dissolved Black Carbon In Snow: A Case Study From The North Cascades, Molly Peek

WWU Graduate School Collection

Black carbon (BC) is partially combusted organic material from natural and anthropogenic sources, and is a highly effective driver of melt in the cryosphere. BC has been found in both populated and remote areas around the globe. This study follows the evolution of UV-exposed dissolved BC (DBC) in the cryosphere using the Benzenepolycarboxylic Acid (BPCA) markers B4CA, B5CA, and B6CA. Samples were collected from Mount Baker, Washington, and from both an in situ field study and a controlled photodegradation study, both using natural and anthropogenic BC standards. Both natural and experimental samples had a dominance of B5CA relative to other …

Conifer Establishment And Encroachment On Subalpine Meadows Around Mt. Baker, Wa, Ben Hagedorn

WWU Graduate School Collection

The subalpine ecotone is experiencing significant change in habitat availability and connectivity as a result of climate change and climate variability. To understand how these changes vary temporally and spatially in the Pacific Northwest, we collected cross-sections and counted whorls of conifers along four transects around Mt. Baker, Washington in the North Cascades. In addition to the samples collected, we also gathered data on microsite conditions that impact seedling establishment. Using partial correlation analyses, we compared establishment dates to climate variables in five-year bins, and used normal correlation analyses along with other statistical tests to determine the effect of various …

Testing The Potential For Using Structure From Motion Photogrammetry Methods To Estimate Seasonal Mass Balance On Lower Easton Glacier, Mount Baker, Wa, Elizabeth Kimberly

WWU Graduate School Collection

The traditional glaciological method of measuring glacier mass balance is labor-intensive and relies on broad extrapolation of sparse ablation stake data collected in the field to assess mass change across the glacier. In contrast, digital elevation models (DEMs) obtained from unmanned aerial vehicle (UAV) imagery and Structure-from-Motion (SfM) photogrammetry resolve a spatially distributed data set of surface elevation change. In this study, I compare seasonal mass balance estimated by field-based glaciological methods and UAV-SfM methods during summer 2018 on the Easton Glacier, Mount Baker, WA. Total snow and ice surface melt was measured at five ablation stakes between May 20th …

The Generation Of A Diverse Suite Of Late Pleistocene And Holocene Basaltic-Andesite Through Dacite Lavas From The Northern Cascade Arc At Mount Baker, Washington, Troy D. Baggerman

WWU Graduate School Collection

This study highlights geochemical diversity in a spectrum of basaltic andesite through dacite lavas from Mount Baker, WA, and describes processes that are responsible for their generation. Petrographic observations, mineral chemistry, along with whole rock major oxide concentrations, and trace and REE data are provided for three Late Pleistocene and Holocene lava flows: the basaltic andesite of Sulphur Creek (SC) (52.5-55.8 wt.% Si02, Mg# 57-54), the andesite of Glacier Creek (GC) (58.3-58.7 wt.% Si02, Mg # 63-64), and the andesite and dacite of Boulder Glacier (BG) (60.2-64.2 wt.% Si02, Mg # 50-57). Major oxide concentrations for SC and BG display …

Volcanology And Geochemistry Of The South Flank Of Mount Baker, Cascade Range, Washington, Douglas Mckeever

WWU Graduate School Collection

Major element chemical analysis of 97 rocks from the south side of Mount Baker was performed by energy dispersive x-ray fluorescence. Conclusions based on chemistry are:

1) Variation diagrams based on a large number of samples show that variation is not continuous nor, in general, smooth. Rocks from two major stratigraphic positions exhibit compositional coherency within each group and are interpreted as eruptive groups which were extruded over time intervals which were short compared to the lifetime of the volcanic center. The older of the two groups is called the Park Butte phase, and the younger is the Koma Kulshan …