Related Experiment Video
Updated: Mar 3, 2026

06:10
Using Generative Art to Convey Past and Future Climate Transitions
Published on: March 31, 2023
1.5K
Climate strategies: thinking through Arctic examples
Barbara Bodenhorn1, Olga Ulturgasheva2
1Department of Social Anthropology, University of Cambridge, Free School Lane, Cambridge CB2 3RD, UK bb106@cam.ac.uk.
Summary
Extreme weather in Siberia and Alaska is increasing, requiring flexible adaptation strategies. Local responses and flexibility are crucial for survival, alongside mitigation and adaptation policies for Arctic communities.
Area of Science:
- Environmental Science
- Climate Change Studies
- Arctic Research
Background:
- Frequent and unpredictable extreme weather events in Siberia and Alaska are causing significant infrastructure damage and threatening indigenous livelihoods.
- The Arctic region acts as a global climate driver, with future resource potential creating a conflict between environmental preservation and development goals.
Purpose of the Study:
- To analyze the impact of increasing extreme weather events in Siberia and Alaska.
- To evaluate the effectiveness of local adaptive strategies and challenge centralized planning assumptions.
- To propose flexibility as a key survival value for Arctic communities and planners.
Main Methods:
- Drawing on material and case studies from Siberia and Alaska.
- Analyzing the interplay of local politics and strategic planning in extreme event response.
- Examining the tension between environmental and development objectives in the Arctic.
Main Results:
- Extreme weather events are becoming normalized in the Arctic, leading to fluctuating material demands and challenges in future needs assessment.
- Local-level responsive strategies are vital and should be integrated into planning, moving beyond a 'center-out' approach.
- Flexibility is identified as a critical survival value for diverse stakeholders, from reindeer herders to urban planners.
Conclusions:
- Arctic communities require integrated mitigation and adaptation policies to address the normalization of extreme weather.
- Promoting adaptive capacities, particularly in younger generations, is essential for future resilience.
- Rethinking material demand reduction strategies to include substitution alongside reduction is necessary.
Related Concept Videos
Global Climate Change
29.2K
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
29.2K
What is Climate?
21.1K
Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
21.1K
Adaptations that Reduce Water Loss
28.4K
Though evaporation from plant leaves drives transpiration, it also results in loss of water. Because water is critical for photosynthetic reactions and other cellular processes, evolutionary pressures on plants in different environments have driven the acquisition of adaptations that reduce water loss.
28.4K
Responses to Heat and Cold Stress
15.3K
Every organism has an optimum temperature range within which healthy growth and physiological functioning can occur. At the ends of this range, there will be a minimum and maximum temperature that interrupt biological processes.
15.3K
The Carbon Cycle
44.7K
Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
44.7K
Radiation: Applications
1.9K
The average temperature of Earth is the subject of much current discussion. Earth is in radiative contact with both the Sun and dark space; it receives almost all its energy from the radiation of the Sun and reflects some of it into outer space. Dark space is very cold, about 3 K, so Earth radiates energy into it. For instance, heat transfer occurs from soil and grasses, the rate of which can be so rapid that frost can occur on clear summer evenings, even in warm latitudes.
The average...
The average...
1.9K

