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Between Earth and Sky - Climate Change on the Last Frontier

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Science and Nature

Summary

The documentary presents Alaska as an early-warning region for climate change, showing changes in snow, glaciers, permafrost, forests, coastal communities, and wildlife. It also considers the tension between extracting energy resources and protecting natural landscapes.

Observed Changes and Natural Processes

  • Less snow and changing winter conditions: Anchorage’s Iditarod trail organizers describe unusually low snowfall—about 27–28 inches at the time of filming, roughly half the usual amount. They had to stockpile and truck in snow, shorten or reroute parts of the course, and prioritize the safety of dogs and competitors.
  • Earlier plant growth: Willows and alders near the Knik Glacier were emerging and blooming unusually early in spring. A speaker connects this observation with reports of exceptionally warm winters and summers, while noting that the effects on plant longevity are uncertain.
  • Glacier retreat and windblown silt: The Knik Glacier is described as having retreated about two miles in 20 years. Glacial grinding produces fine silt, or loess, which winds carry into nearby communities. Loess deposits contribute to the fertile soils around Palmer, though those soils are low in nitrogen and phosphorus and often need organic amendments.
  • Permafrost thaw and carbon release:
    • Permafrost is defined in the documentary as earth material at or below 0°C for at least two consecutive years. It may occur continuously across a landscape or in discontinuous patches.
    • Organic soils insulate the ground. As they warm and decompose, that insulating layer can collapse or diminish, allowing deeper ground and permafrost to warm further.
    • The film describes Arctic and subarctic uplands as holding a major store of soil carbon. Thaw and decomposition can release carbon dioxide and methane, reinforcing warming.
  • Infrastructure vulnerability: Asphalt absorbs and conducts heat into the ground, contributing to permafrost thaw beneath roads. The documentary cites estimates of billions of dollars in added road and building maintenance costs in interior Alaska as permafrost degrades.
  • Methane from thaw lakes: When ice wedges melt, the ground can collapse into water-filled depressions. The water is warmer than the surrounding frozen ground, so thaw can expand. Microbes consume thawed organic matter and produce methane and carbon dioxide. Bubbles can become trapped in winter lake ice and escape when it melts. The film describes this as a positive feedback loop: warming causes thaw, thaw fuels greenhouse-gas production, and those gases contribute to further warming.
  • Forest and ecosystem effects: Speakers describe larger and more frequent forest fires, trees tilting as thaw destabilizes the ground (“drunken forests”), and changes to vegetation and hydrology. One researcher says that permafrost has disappeared from some temperature-sensitive areas of western Alaska over roughly the previous 30 years.
  • Coastal erosion and village risk: Reduced and later-forming sea ice leaves coastal settlements more exposed to storms. Thawing permafrost makes shorelines less stable, while storm surges and waves can remove large sections of coast. The documentary reports that more than 30 communities faced some form of erosion, flooding, or storm-surge risk.
  • Impacts on Shishmaref: Residents describe strong ties to the land and sea, which provide food and support cultural practices. They report worsening erosion and storm exposure, and fear losing homes, livelihoods, and cultural knowledge if the village must relocate. Relocation costs are discussed as potentially extremely high, while funding and long-term plans remain uncertain.
  • Climate observations and uncertainty: Some residents say they have not noticed major changes or argue that individual unusual years fall within natural variability. Other speakers point to multiple long-term indicators—including warming, glacier retreat, permafrost loss, fire, and changing sea ice—and describe climate change as already underway. The documentary also warns of possible climatic tipping points, while acknowledging that their timing is uncertain.
  • Resource use and conservation: The film discusses Alaska’s dependence on oil revenues alongside the environmental costs of fossil-fuel extraction. It argues for reducing fossil-fuel use, conserving energy, and developing lower-carbon energy sources. Kotzebue is presented as an example of wind power reducing diesel consumption, with solar power also being considered.
  • Broader significance: Speakers characterize Alaska as a “canary in the coal mine,” because changes in its ice, frozen ground, forests, and communities may foreshadow risks elsewhere. The film also links climate-related pressures to wider challenges, including crop loss, displacement, and stress on fisheries.

Methods and Actions Described

  • Monitor and quantify soil resources: Soil surveys and field observations can establish what soils are present and estimate stored carbon and methane. The documentary argues that this information is needed for informed policy and resource-management decisions.
  • Document soils in the field and laboratory: Soil scientists describe examining soil profiles, mapping landscape variability, and using specialized tests suited to Arctic soils.
  • Track environmental indicators: Measurements of permafrost, sea ice, glaciers, and snow accumulation and melt are presented as ways to detect environmental change.
  • Estimate personal emissions: A carbon calculator—such as the one attributed to the EPA—can help people identify major sources of their household emissions and possible ways to reduce them.
  • Reduce emissions and support action: Suggested steps include using less energy, adopting renewable sources such as wind and solar, making lower-carbon personal choices, and voting for representatives and policies that address climate change.
  • Plan for resilient communities: The documentary emphasizes preparing for erosion and other hazards while weighing relocation, infrastructure, cultural continuity, and conservation.

Researchers and Sources Featured

The auto-generated subtitles do not provide full names for most interviewees. They refer to:

  • “Chin Lou” / “Chin Lew” — a soil scientist whose name is unclear in the subtitles; credited by interviewees with Arctic-soil research, publications, and teaching many students.
  • “Chandler” — a researcher whose work on landscape dynamics and Arctic-soil variability is mentioned; no first name is given.
  • “Mark” — a soil-survey professional described as having extensive field experience; no surname is given.
  • Unnamed researchers and specialists in soil science, forestry, climate, and land management, as well as residents of Shishmaref and other Alaskan communities.
  • U.S. Environmental Protection Agency (EPA) — cited as providing a carbon calculator.
  • Paris Accord — discussed in connection with the 2015 climate agreement and its temperature goals.
  • Atlantic Richfield Company — mentioned in the historical account of oil development at Prudhoe Bay.
  • Soil surveys and climate records — cited as sources of information about soil conditions and long-term environmental change.

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