Events
Upcoming Events | Past Events
S.T. Lee Presentation
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S.T. Lee Visiting Scholar Lecture: Arctic Sea Ice Changes
Akasofu 401 2160 Koyukuk Dr, Fairbanks, AK, United StatesArctic sea ice changes - from quiet to more dynamical regime Speaker: Mass balance of the Arctic Sea ice depends on thermodynamical and dynamical factors. Thermodynamical and mechanical sea ice…
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S.T. Lee Visiting Scholar Lecture: Poungawai, A Digital River
Māori design and digital technology give voice to water through art Speakers: For Māori, the concepts of mana (power) and mauri (life force) are fundamental to understanding and ensuring the…
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S.T. Lee Young Scientist Exchange: Bacterial rhodopsin in Antarctic sea ice
Description: Ian Blixt, a PhD Candidate at Victoria University of Wellington in New Zealand, will present at IARC as part of the S.T. Lee Young Scientist Exchange. Blixt will discuss…
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S.T. Lee Fellowship Presentation: Climate solutions for Pacific Island resilience
Akasofu 401 2160 Koyukuk Dr, Fairbanks, AK, United StatesTitle: Climate Solutions for Pacific Island Resilience – the Pacific RISA Program Description: Laura Brewington (Arizona State University, the East-West Center) will provide an introduction to the Pacific Regional Integrated…
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S.T. Lee Young Scientist Exchange Lecture – Anthropogenic forcing: effects on extreme glacier mass-loss
Akasofu 401 2160 Koyukuk Dr, Fairbanks, AK, United StatesThis lecture is part of the S.T. Lee Young Scientist Exchange with Victoria University of Wellington, New Zealand. Visiting scientist: Lauren Vargo Talk overview: Glaciers are unique indicators of climate change, and extreme glacier mass loss is becoming more common globally. While decadal glacier decline has been attributed to anthropogenic forcing, direct links between anthropogenic…
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S.T. Lee Fellowship Presentation- Stratovolcano mapping and paleoclimate: a complementary story of lava and ice
Stratovolcanic deposits are potentially powerful paleoclimatic records: lavas can be radiometrically dated, lava geometries describe the thicknesses of ice masses at particular elevations, and water-supported deposits (e.g., hyaloclastites) describe subglacial ice structures. Although glaciovolcanism is not a new concept, it is underutilised in both stratovolcano mapping and paleoclimate studies. This talk looks beyond the well-known relationships between large volcanic eruptions and climatic response.