Now showing items 1-20 of 1943

    • @Egan Newsletter 2018 Convocation Edition

      University of Alaska Southeast, 2018-08
    • @Egan Newsletter 2017 Convocation Edition

      University of Alaska Southeast, 2017-08
    • @Egan Newsletter 2016 Convocation Edition

      University of Alaska Southeast, 2016-08
    • Snow avalanches and the impact of climate‐linked extreme events on mountain wildlife population dynamics and resilience

      White, Kevin S.; Levi, Taal; Hood, Eran; Darimont, Chris T. (Wiley, 2025-09-24)
      Climate is changing rapidly in mountain environments, giving rise to increasing variability in weather, incidence of extremeevents, and alteration of the cryosphere. Natural hazards, such as snow avalanches, and the ecological communities they impactmay be particularly sensitive to such change. While avalanches may impose both ‘good’ and ‘bad’ effects on mountain ecosys-tems, the direct impacts that lead to mortality have particularly important implications for future viability and resilience ofslow-growing alpine wildlife populations. Here, we studied a sentinel species of coastal Alaskan mountain environments—themountain goat (Oreamnos americanus) – using long-term field data from individually marked animals (600 individuals over44 years) in a quantitative modeling framework to understand how avalanches influence demographic processes. Specifically, wedeveloped and parameterized a sex- and age-specific population modeling approach to simulate the effects of avalanche-causedmortality on population growth rate (λ). We examined a range of ecologically relevant scenarios based on empirically observedstates of avalanche-caused mortality. During years when avalanche impacts are severe, populations can experience significantadditive mortality and population declines (up to 15%). Due to low reproductive rates, such impacts can lead to long demographicrecovery times (up to 11 years, or ~1.5 mountain goat generations). Thus, during the course of a typical mountain goat lifetime,significant avalanche-linked perturbations can be expected to occur, suggesting that meaningful demographic signatures of av-alanche impacts are generationally recurrent and routinely imbedded in population histories. From a conservation perspective,such impacts are striking and highlight the utility of employing a quantitative modeling approach to predict possible effects ofavalanches and extreme events more broadly on mountain ungulate population dynamics and viability. Our work explicitlybuilds upon recent findings about the importance of avalanches on mountain-adapted animal populations and has implicationsfor the cultural and ecological communities that depend on them.
    • The art of compassion: how viewing art affects prosocial intentions

      Dolese, Melissa (Routledge Taylor & Francis Group, 2025-09-02)
      Art functions as a communicative medium that evokes emotion and fosters social connection potentially motivating prosocial behavior. Grounded in theories of elevation and social cognition, this research investigated whether viewing art, regardless of its thematic content, would influence compassionate intentions toward individuals across varying relational distances (self, friend, stranger). The studies also examined if the types of imagined compassionate actions, categorized by expressive modalities (Chapman’s Love Languages, Gestures of Kindness, and Hedonic Pleasures), varied with relational closeness. Study 1 found that compassion-themed art influenced compassionate intentions toward strangers, with artistic communication predicting these intentions more strongly than explicit compassion messaging. Study 2 demonstrated that elevation, elicited by non-compassion-themed art, predicted compassionate intentions, particularly toward strangers. Across both studies, participants envisioned more intimate, close-proximity actions toward relationally close others. These findings indicate that art functions as a socially meaningful stimulus, activating emotional and cognitive mechanisms that support context-sensitive prosociality.
    • Community-based, culturally relevant STEM: Engaging rural and Indigenous students through partnerships, institutional flexibility, and One Health

      Chenoweth, Ellen; Cotter, Paul; Straley, Janice; Lanphier, Kari (Springer, 2025-07-02)
      Rural and Indigenous students face many barriers to persistence in biomedical and STEM trajectories including poor access to science experiences, a dearth of relatable educational resources, and educational structures misaligned with rural and Indigenous student and community needs. Rural Alaska Students in One Health Research (RASOR) is designed to provide a positive first college experience for rural and Indigenous students. Key innovations include 1) a partnership between the University of Alaska and tribal governments to allow for culturally relevant, locallymentored research experiences and 2) a customizable program structure. We also surveyed adults in the region regarding attitudes about science, its community relevance, and science opportunities for young people. One Health—the connection of human, animal, and environmental health—resonated with both adults and students. Student interest in both animal/environmental and human research increased during RASOR, as did measures of science self-efficacy, identity, and science aspirations. Community members view science as important and strongly support students’ scientific interests. However, perceptions remain that science training results in students leaving their communities, despite tribal leadership efforts to “grow-theirown” STEM opportunities and professionals in these same communities. We suggest One Health is a culturally meaningful pathway to promote engagement of rural and Indigenous students in biomedical and STEM fields and is enhanced by educator and institutional flexibility and community partnership.
    • Calving as a source of acute and persistent kinetic energy to enhance submarine melting of tidewater glaciers

      Shaya, M. F.; Nash, J. D.; Pettit, E. C.; Amundson, Jason M.; Jackson, R. H.; Sutherland, D. A.; Winters, D. (American Geophysical Union, 2025-10-07)
      Calving icebergs at tidewater glaciers release large amounts of potential energy. This energy—in principle—could be a source for submarine melting, which scales with near‐terminus water temperature and velocity. Because near‐terminus currents are challenging to observe or predict, submarine melt remains a key uncertainty in projecting tidewater glacier retreat and sea level rise. Here, we study one submarine calving event at Xeitl Sít’ (LeConte Glacier), Alaska, to explore the effect of calving on ice melt, using a suite of autonomously deployed instruments beneath, around, and downstream of the calving iceberg. Our measurements captured flows exceeding 5 m/s and demonstrate how potential energy converts to kinetic energy (EK). While most energy decays quickly (through turbulence, mixing, and radiated waves), near‐terminus EK remains elevated, nearly doubling predicted melt rates for hours after the event. Calving-induced currents could thus be an important overlooked energy source for submarine melt and glacier retreat.
    • Fine-scale variability in iceberg velocity fields and implications for an ice-associated pinniped

      Kaluzienski, Lynn M.; Amumdson, Jason M.; Womble, Jamie N.; Bliss, Andrew K.; Pearson, Linnea E. (Copernicus Publications / European Geosciences Union, 2025-06-24)
      Icebergs found in proglacial fjords serve as important habitats for pinnipeds in polar and subpolar regions. Environmental forcings can drive dramatic changes in the overall reduction in ice coverage across fjords in the circumpolar regions, with implications for pinnipeds that use ice for critical life-history functions, including pupping and molting. To better understand how pinnipeds respond to changes in iceberg habitat, we combine (i) iceberg velocity fields over hourly to monthly timescales, derived from high-rate time-lapse photogrammetry of Johns Hopkins Glacier and Inlet, Alaska, with (ii) aerial photographic surveys of harbor seals (Phoca vitulina richardii) conducted during the pupping (June) and molting (August) seasons. Iceberg velocities typically followed a similar diurnal pattern: flow was weak and variable in the morning and strong and unidirectional in the afternoon. The velocity fields tended to be highly variable in the inner fjord across a range of timescales due to changes in the strength and location of the subglacial outflow, whereas, in the outer fjord, the flow was more uniform, and eddies consistently formed in the same locations. During the pupping season, seals were generally more dispersed across the slow-moving portions of the fjord (with iceberg speeds of < 0:2 ms−1). In contrast, during the molting season, the seals were increasingly likely to be found on fastmoving icebergs in or adjacent to the glacier outflow plume. The use of slow-moving icebergs during the pupping season likely provides a more stable ice platform for nursing, caring for young, and avoiding predators. Periods of strong glacier runoff and/or katabatic winds may result in more dynamic and less stable ice habitats, with implications for seal behavior and distribution within the fjord.
    • Laboratory experiments reveal transient fluctuations in ice mélange velocity and stress during periods of quasistatic flow

      Nissanka, Kavinda; Vora, Nandish; Méndez Harper, Joshua; Burton, Justin C.; Amundson, Jason M.; Robel, Alexander A.; Meng, Yue; Lai, Ching-Yao (Wiley, 2025-09)
      Accurately predicting Greenland's ice mass loss is crucial for understanding future sea level rise. Approximately 50% of the mass loss results from iceberg calving at the ice-ocean interface. Ice mélange, a jammed, buoyant granular material that extends for 10 km or more in Greenland's largest fjords, can inhibit iceberg calving and discharge by transmitting shear stresses from fjord walls to glacier termini. Direct measurements of these resistive force dynamics are not possible in the field, thus, we created a scaled-down laboratory experiment to study jammed-packed ice mélange mechanics. We recorded videos of the mélange surface motion and subsurface profile during slow, quasistatic flow through a rectangular fjord, and recorded the total force on a model glacier terminus. When the wall friction is low, the ice mélange moves as a solid plug with little or no particle rearrangements. When the wall friction is larger than the internal friction, shear zones develop near the walls, and the buttressing force magnitude and fluctuations increase significantly. Associated discrete particle simulations illustrate the internal flow in both regimes. We also compare our experimental results to a continuum, depth-averaged model of ice mélange and find that the thickness of the mélange at the terminus provides a good indicator of the net buttressing force. However, the continuum model cannot capture the stochastic nature of the rearrangements and concomitant fluctuations in the buttressing force. These fluctuations may be important for short-time and seasonal controls on iceberg calving rates in fjords with thick and persistent ice mélange.
    • @Egan Newsletter 2025 Convocation Edition

      Henrickson, Kaia; Cox, David; Broussard, Ramona; Goodman, Jessy; Ward, Jennifer (University of Alaska Southeast, 2025-08)
    • UAS Academic Catalog 2004/2005

      University of Alaska Southeast, 2004
    • UAS Academic Catalog 2003/2004

      University of Alaska Southeast, 2003
    • UAS Academic Catalog 2002/2003

      University of Alaska Southeast, 2002
    • UAS Academic Catalog 2001/2002

      University of Alaska Southeast, 2001
    • UAS Academic Catalog 2000/2001

      University of Alaska Southeast, 2000
    • UAS Academic Catalog 1999/2000

      University of Alaska Southeast, 1999
    • UAS Academic Catalog 1998/1999

      University of Alaska Southeast, 1998
    • UAS Academic Catalog 1997/1998

      University of Alaska Southeast, 1997
    • UAS Academic Catalog 1996/1997

      University of Alaska Southeast, 1996
    • UAS Academic Catalog 1995/1996

      University of Alaska Southeast, 1995