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Sub-challenge: observed changes in migrations and other animal behaviour relevant to traditional way of life (reindeer husbandry, whaling, fishing)
Climate change can have both direct and indirect effects on the natural environment. Rising (sea) temperatures or melting sea-ice can be seen as direct effects, whereas ecological systems including (human) behaviour can be affected indirectly. Polar regions show results of climate change at a much faster pace than other regions will (Berkes & Jolly, 2001, Hobbie et al., 2017). This makes the Arctic an ideal study environment for assessing effects of climate change, including the effects on (human) behaviour. However, before we can study the impact of climate change on the traditional way of life of humans, we first need to study climate change in the Arctic, the ‘traditional way of life’ and the animals related to this.
How is the Arctic climate changing?
The Arctic climate has two main patterns of circulation (Figure 1). In the positive phase, cold air is kept within the Arctic, which is favourable for sea ice formation and associated ecosystems (Thompson and Wallace, 1998). More recently the negative phase is getting increasingly common, leading to more snow in the mid-latitude North America, Europe and eastern Asia. With more cold air escaping the Arctic, the Arctic itself warms up and sea-ice retreats and the length of open water periods in the Beaufort and Chukchi Seas is increasing (Thomson et al, 2016).
Figure 1: Different phases of the Arctic Oscillation, associated with different winds and storm tracks in the Arctic. Positive phase on the left, negative phase on the right. Courtesy of Dr. Dave Thomson, Colorado State University.
The length of the melt season in the Arctic has increased approximately by one day every two years since 1979 (Stroeve et al, 2014, see also Markus et al 2009). As open water absorbs more solar radiation than ice cover, sea surface temperature (SST) in the Arctic has increased by 0.5-1.5?C over the last decade (see also the Temperature sub-challenges), leading to delays in the timing of freeze-up initiation (Markus et al, 2009). This has resulted in changes in the overall ice thickness of Arctic sea ice (Animations of changing sea ice export and ice thickness are available from NASA Goddard's Scientific Visualization Studio: https://www.nasa.gov/feature/goddard/2016/arctic-sea-ice-is-losing-its-bulwark-against-warming-summers). Timing of migratory species has changed with the sea ice, e.g. the autumn migration of Beluga whales has delayed an average of 4 days/year, based on data from 2008-2014 (Hauser et al, 2016).
Traditional way of life
The ‘traditional way of life’ can be linked to indigenous people, keeping to traditions set many generations ago, often making use of subsistence herding, gathering, hunting or fishing. During the last century, Arctic regions have modernized enormously. For example, in Greenland subsistence hunting and fishing is still widespread, but it has increasingly become a leisure activity in comparison to a ‘way of life’ (Curtis et al. 2005). A similar change can be found in Northern Siberia (Koptseva & Kirko, 2014), Alaska (Moerlein & Carothers, 2012), as well as in the far north of Canada (Berkes & Jolly, 2001; Searles, 2008), where supermarkets and imported foods now add to the diet collected by traditional gathering and hunting (Lougheed, 2010). For this study, no distinction is made between people fully depending on a subsistence way of life, partly depending on it, or not depending on it but still using it for traditional or other purposes.
Because of modernization, social, economic, and demographic change, as well as resource development, trade barriers and animal-rights movements, there have been many changes in human behaviour with regards to the ‘traditional way of life’ (Nuttall et al., 2005). It is hard to filter out which change led to which effect, as many of the changes link together and influence each other.
Effects of climate change on the traditional way of life
Climate change can affect species used for subsistence, but it also affects the means of gathering them. For example, summer sea-ice retreat can lead to a smaller hunting area, extreme weather can damage village infrastructure, melting permafrost can lead to altered spring run-off patterns and changing sea levels and tidal fluctuations can pose dangerous fishing conditions. Unpredictable weather due to climate change has impact on many aspects, as shown in Figure 3.
The impact of climate change on traditional life is not always linear, it can be a complex network of relationships and effects, each in turn connected to many other aspects. For example, due to the rapid changes in climate, elders are unable to predict weather compared to their former knowledge and experience, and they cannot pass this knowledge on to the next generation. Lower predictive skill means increased risks of failure or accidents during hunting, migration, food collection and camp formation. Loss of these traditional skills changes the way of life rapidly. Efforts to map traditional knowledge in peer reviewed scientific studies have been limited in success due to the difference in the types of information: historical knowledge and experience vs. experimental or observational studies.
Figure 3: Observation, impact & adaptation diagram for Canadian Inuit regions on unpredictable weather. Source: Nickels et al. 2005.
Fish is the most reliable subsistence resource in Alaska (Moerlein & Carothers, 2012). In several communities in north-western Alaska the catch contains chum salmon (Oncorhynchus keta), dolly varden (Salvelinus malma) and several species of whitefish (Moerlein & Carothers, 2012). Fishing and hunting practices are extremely flexible in response to changing conditions and needs (Moerlein & Carothers, 2012).
Musk-ox (Ovibos moschatus), lesser snow goose (Anser caerulescens), ringed seal (Phoca hispida), and various fish species are the main species for hunting in the Canadian Arctic (Berkes & Jolly, 2001). During winter, people hunt musk-ox and, to a lesser extent, caribou (Rangifer tarandus), arctic foxes (Alopex lagopus), wolves (Canis lupus), polar bears (Ursus maritimus), and ringed seals (Pusa hispida). The study provides a list of examples of local environmental changes and effects on subsistence activity described by members of the community. This includes impacts on access, safety, predictability and species availability. For example, old ice doesn't come in close to the settlement in summer anymore which makes it more difficult to hunt seals; open sea-ice in winter makes travel dangerous; the arrival of spring differs from year to year; and more rain in the fall increases chances of freezing rain, which can lead to caribou starving. The effects of these changes and the response strategies of the affected people vary. Because of modernisation most communities have a wider range of food options now, making it less vital for a direct need to adapt to the environmental changes. Response strategies on a short-term such as use of other vehicles for travel, changing hunting areas or waiting for the appropriate timing are applied (Berkes & Jolly, 2001). Long-term adaption strategies are only speculated. Climate Change may not always have a negative effect. For example, with seawater temperatures rising, marine fishes of a more temperate origin move northward into the Arctic seas (Christiansen, Mecklenburg, & Karamushko, 2014). Two species of Pacific Salmon were welcomed by local inhabitants.
A combination of modernisation, globalisation and Climate Change has affected subsistence living conditions in Upernavik in northern Greenland (Hendriksen & Jørgensen, 2015). Since the 1980s Greenland Halibut fishing in dinghies has been a major source of income for the local community in summer. Dangerous situations arise when the shorter period of sea-ice forces fishing to be carried out in the dark winter period as well. The same applies for hunting of whales and seals. Local communities have been rather resilient and adaptive in meeting the challenges set by Climate Change, due to their traditional and local knowledge (Hendriksen & Jørgensen, 2015). They point out that governance (such as restrictions in hunting or fishing methods or set quotas) is even more challenging than the changes in their natural environment; it is not only Climate Change which threatens the traditional way of life.
The migratory behaviour of caribou
Distribution and ecology
Caribou (Rangifer tarandus) is a species of deer native to the Arctic environment. There are many subspecies within the circumpolar distribution (see Figure 4). Some of the populations are sedentary while others are typically migratory. Caribou are unique ruminants, feeding mainly on lichens and some senescent browse in wintertime (Parker et al. 2005).
An interactive map with caribou habitats can be found here: http://carma.caff.is.
The species Rangifer tarandus is called ‘reindeer’ in Europe and Asia and ‘caribou’ in North America. However, there seems to be genetic diversity between the two, with two original lineages: one originating from and confined to Northeastern America, and the other originating from Euro-Beringia but also currently distributed in western North America (Yannic et al. 2013). For this report however, no distinction is made between the two and Rangifer tarandus is used for both caribou and reindeer and ‘caribou’ is used to indicate Rangifer tarandus.
Effects of Climate Change of caribou
Climate Change can impact caribou in many ways. For example through changes in habitat and food accessibility, and in temperature, see Table 1 (source: CARMA, CircumArctic Rangifer Monitoring and Assessment Network, accessed on April 11, 2017).
Table 1: Climate Change impacts on caribou. Source: http://carma.caff.is
|Climate Change Condition
||Impact on Habitat
||Impact on Movement
||Impact on Body Condition
||Impact on Productivity
|Earlier snowmelt on coastal plain
||Higher plant growth rate
||Core calving grounds move further north Less use of current calving grounds
||Cows replenish protein reserves faster Higher calf growth rate
||Higher probability of pregnancy Higher June calf survival
||Need for wider calving ground protection
|Warmer, drier summer
||Earlier peak biomass Plants harden earlier Reduction in mosquito breeding sites Increased oestrid harassment Increased frequency of fires on winter range Fewer “mushroom” years
||Movement off of calving grounds earlier More use of insect relief habitat in July Avoidance of recently burned winter habitat
||Increased harassment will lower fall body condition
||Reduced probability of pregnancy
||Protection of insect relief areas important
|Warmer, wetter fall
||More frequent icing conditions
||Caribou abandon ranges with severe surface icing
||Higher winter mortality Earlier weaning
|Warmer, wetter winters
||Deeper denser snow Icing conditions, especially in tundra and arctic islands
||Increased dependence on low snow regions stay on winter range longer
||Greater over winter weight loss higher incidence of extended lactation
||lower over winter mortality on calves
||Need to consider protection of low snow regions
||More freeze/thaw cycles during spring migration Faster spring melt
||Movement slowed and/or movement unto drier windswept ridges
||Accelerated weight loss in spring
||Higher wolf predation on cows and calves due to use of windswept ridges
||Concern over timing and location of spring migration in relation to traditional harvesting areas
In very general terms the calving range improves but movement and reliance on more northern portions of the calving range; animals leave calving range earlier; cows and calves suffer reduced summer and autumn body reserves due to increase in oestrid fly harassment; mosquito harassment may be reduced if summers are drier; more frequent icing on autumn, winter and spring ranges which, depending on the location of these ranges may have moderate to severe implications to body condition and survival.
In relation to management, there will be an overall need to assess habitat protection in relation to climate trends, need to factor climate change impacts on harvest strategy, need to communicate impacts of climate on harvest patterns and timing and a need to set up comprehensive monitoring programs.
Behaviour of two herds of caribou in Canada is described as: “Migratory caribou appeared to prefer regions with higher snowfall and lichen availability in the fall and winter. In the summer, caribou preferred cooler areas likely corresponding to a lower prevalence of insects, and they avoided disturbed and recently burnt areas (Sharma et al. (2009).” Models were used to indicate possible responses of these herds to Climate Change. The results are variable, as responses depend on the current migratory pattern and habitats and the possible effect of Climate Change in this. This limits the range of one herd but increases the range of the other, limiting both to a certain region (Sharma et al. 2009).
Influence of climate change on the behaviour of caribou and the traditional way of life
Caribou are an important source of food in the traditional way of life all over the Arctic. Impacts of climate change on the traditional way of life can include the loss of possible hunting areas or herds either in certain periods of time or permanently, as well as the other way around. Freezing rain in fall can lead to caribou starvation which would lead to a lower prey availability for subsistence hunting (Berkes & Jolly, 2001). On the contrary, increased availability of summer forage and more wind as favourable conditions may lead to a higher prey availability.
Traditional knowledge gives subsistence hunters flexibility in dealing with climate change (Pearce et al., 2015). For example, knowledge of caribou husbandry but also knowledge on how to deal with and prepare for hazardous hunting conditions can give the hunters footholds when conditions change.
In conclusion, climate change has a direct effect on caribou behaviour which in turn influences the traditional way of life. However, effects of climate change on caribou are variable, resulting in both positive and negative effects for subsistence hunters. The effects depend on (among others) location and normal migration behaviour of the caribou, season, and (traditional) knowledge and flexibility of the hunters.
Distribution and ecology
Bowhead whales (Balaena mysticetus) typically live in the Arctic and are divided in four stocks: Bering-Chukchi-Beaufort Seas (US (Alaska), Canada, and Russian Federation); eastern Canada – west Greenland (Canada and Denmark (Greenland)); Svalbard-Barents Sea (Spitsbergen) (Denmark (Greenland), Norway, and Russian Federation); and the Okhotsk Sea (Russian Federation and Japan) (COSEWIC, 2009; Reilly et al. 2012). The eastern Canada – west Greenland stock was previously thought to be two separate stocks (Hudson Bay-Foxe Basin; Davis Strait-Baffin Bay), however new research showed they belong to the same stock (COSEWIC, 2009; Wiig et al. 2009).
Figure 5: Four different stocks of the Bowhead Whale. 1. Okhotsk Sea, 2. Bering–Chukchi–Beaufort seas (BCB DU), 3. Eastern Canada – West Greenland (EC–WG DU), 4. Svalbard/Barents Sea. Question marks denote the Labrador coast where Inuit are historically reported to have harvested Bowheads. Basque whalers hunted Bowheads in the Strait of Belle Isle (C). Floating or stranded Bowhead carcasses were observed at Rattling Brook (B) in 1998 and Mobile Point (A) in 2005. Source: COSEWIC, 2009.
During summertime bowhead whales migrate to the high Arctic and they retreat to the sea-ice edges during wintertime (Reilly et al. 2012). Bowhead whales are very large animals with body lengths of over 19 meter and a body mass of over 80 metric ton (George et al. 2015). Despite their size, bowhead whales feed mostly on zooplankton in the form of medium-sized crustaceans such as krill and copepods (Reilly et al. 2012).
All bowhead whale stocks have been severely overexploited during the commercial whaling periods of the 18th and 19th century. Since the end of the large-scale commercial whaling the stocks are slowly recovering. The Bering-Chukchi-Beaufort Seas (BCB) stock is thought to be close to pre-whaling levels, but the Atlantic stocks recover more slowly and are still at relatively low levels (Fauchald et al. 2017).
Effects of climate change on the bowhead whale
As bowhead whales are a typical ice-associated migratory species, climate change could have a direct effect on them. The bowhead’s food, zooplankton, is closely coupled to the primary production, which in turn is directly influenced by climate change (see also the sub-challenge ‘phytoplankton’) (George et al. 2015). However, bowhead whales are not directly dependent on the presence of sea-ice but more on the presence of zooplankton, which may also be present in open water. The reduction of sea-ice could even have a positive influence on the amount of available prey for the bowhead whale through an increase in primary production (George et al. 2015; Moore & Huntington, 2008; Moore & Laidre, 2006).
Influence of climate change on the behaviour of bowhead whales and the traditional way of life
Bowhead whales have been part of subsistence hunting for thousands of years (Ashjian et al. 2010; Seersholm et al. 2016; Suydam & George, 2004). Current subsistence hunting on bowhead whales is regulated through strict quotas to not impede further stock recovery (Fauchald et al. 2017).
Subsistence whaling in the BCB stock (Alaska) can be taken as an example. The (rough) migratory pattern of this stock is depicted in Figure 6 (George et al. 2015). During the spring and fall migrations the local communities of Northern Alaska hunt the bowhead whales to provide subsistence food (Ashjian et al. 2010). The presence of bowhead whales is mostly dependent on readily available food sources (zooplankton) which can be directly seen in its distribution.
Figure 6: Seasonal range map of the Bering–Chukchi–Beaufort bowhead whales based on satellite telemetry data (Quakenbush et al., 2012). Bowheads are also known to occur in regions outside these general boundaries. Source: George et al. 2015.
Four factors influence the availability of euphausiids (krill) as food source for bowhead whales near Barrow (at the most northern tip of Alaska) during the migration seasons (Ashjian et al., 2010):
the northwards transport of Pacific Water during spring;
- the quantity of euphausiids in the Pacific Water and their growth and survivorship during their transit across the Chukchi Sea to the Barrow region;
- the transit time of Pacific Water and plankton from the Bering Strait to Barrow;
- the existence of mechanisms that aggregate euphausiids into dense prey patches.
All the factors link to each other and are affected by climate change effects. Certain wind conditions have influence on the upwelling and aggregation of euphausiids. This creates favourable conditions for bowhead whales and consequently for subsistence hunters. When weather and wind patterns change due to climate change, migration patterns could be altered and subsistence hunting could be affected (Ashjian et al. 2010). Considerable inter annual variation is seen in migration and summer locations of bowheads, possibly due to shifting environmental conditions (Fauchald et al. 2017). Bowhead whales arrive earlier and hunting starts earlier in spring and later in autumn (Huntington et al. 2016). Less multiyear sea-ice and thinner land-ice has made it harder to find ice floats for hauling out whales for butchering in spring. Whales no longer appear to feed along the edge of the land-ice southwest of Barrow in spring (Huntington et al. 2016). The latter seems to pose a bigger problem for the native subsistence hunters than the changing migratory patterns, as the traditional bowhead hunts rely on the presence of sea-ice (Sakakibara, 2017).
In conclusion, climate change has an effect on Bowhead whales’ migration behaviour which in turn influences the traditional way of life. However, as the bowhead whale hunt is influenced by other factors as well, some of them also dependent on climate change, there is not always a direct relationship.
Data use, availability and gaps
To provide a more in depth answer on the availability and quality of data, a more narrow and specified question is needed. For now, two species were chosen to illustrate the effects of climate change on animal behaviour and the traditional way of life. On the (migratory)behaviour of caribou and bowhead whales information can be found mainly in scientific papers published in peer-reviewed journals. Because climate change can have effects on species’ behaviour in various ways with various outcomes it was difficult to build databases for this topic. However, information on the (migratory) behaviour of specific populations or stocks of animals used for the traditional way of life and the influence of climate change on this can’t be found in a single database or data source. While it is complicated to monitor the effects of climate change on the traditional way of life, it is possible to monitor species’ migrations and/or behaviour in areas in which climate change is visible.
Conclusion and lessons learned
Climate change impacts the traditional way of life. This may be a consequence of the effect of climate change on animal behaviour such as migration routes. However, people still actively pursuing the traditional way of life in the Arctic seem to be very adaptive to changing conditions. For example, Inuit in the Canadian Arctic are very flexible, showing responses to varying climatic conditions (Figure 7, Pearce et al. (2015).
Figure 7: Photographs of Inuit in the Canadian Arctic illustrating responses to changing climatic conditions that affect subsistence. (Left): Flexibility – Iqaluit hunters improvise, using boats to maintain access to seal hunting areas in late fall. (Centre): Hazard avoidance – Ulukhaktok hunters make extra efforts to read weather and ice conditions before and during travel. (Right): Emergency preparedness – Knowledge of how to build an emergency snow house enables hunters to wait out storm events. Source: Pearce et al. 2015.
A similar optimism can be found for sustaining subsistence systems, pointing at the long history of subsistence systems and its apparent resilience (Kofinas et al., 2010). However, changing climatic conditions may prove to be too problematic for certain types of traditional hunting as simple things like access to the food source may cause a significant reduction in the availability of subsistence resources in the future (Brinkman et al. 2016).
Lessons learned during the answering of this sub-challenge:
- There are many types of traditional life, with communities varying in traditions, size, etc., and information is not always available;
- Information on animal migration and the influence of climate change on migration behaviour is available for some species such as caribou and bowhead whales;
- The available information is usually in text-form as scientific published peer-reviewed papers;
- Behavioural changes and effects of climate change will not always be directly related, as complex interactions and relations can alter parts of the system or combinations of different systems;
- Databases with direct numbers are not always available;
- Climate change is not the only thing affecting the traditional way of life: globalization, westernization and modernization are only some of the other factors influencing the traditional way of life.
To know the needs of the people using the traditional ways of life and the influence of climate change on animal behaviour linked to this, long term and consistent research is needed. Examples of monitoring are:
- Per traditional community the most used wild species for subsistence reasons;
- Per traditional community the direct effects of climate change on the traditional way of life through subsistence hunting and fishing such as ice decline or weather changes;
- Specific species populations or stocks used for subsistence reasons;
- (Migratory) behaviour of the specific populations or stocks used for subsistence reasons;
- Effects of climate change on the habitat and (migratory) behaviour of specific populations or stocks used for subsistence reasons.
The results of the monitoring should be openly available in a public database.
- Ashjian, C. J., Braund, S. R., Campbell, R. G., GEORGE, J. C., Kruse, J., Maslowski, W., ... & Sherr, E. B. (2010). Climate variability, oceanography, bowhead whale distribution, and Iñupiat subsistence whaling near Barrow, Alaska. Arctic, 179-194. http://darchive.mblwhoilibrary.org/bitstream/handle/1912/5127/973-2855-1-PB.pdf?sequence=1
- Berkes, F., & Jolly, D. (2001). Adapting to climate change: Social-ecological resilience in a Canadian western arctic community. Conservation Ecology, 5(2), 18.
- Brinkman, T. J., Hansen, W. D., Chapin, F. S., Kofinas, G., BurnSilver, S., & Rupp, T. S. (2016). Arctic communities perceive climate impacts on access as a critical challenge to availability of subsistence resources. Climatic Change, 139(3-4), 413-427. https://static1.squarespace.com/static/542db5eae4b03f0fd61b3bb5/t/58389c79579fb36e9c8334d3/1480105095696/
- COSEWIC. 2009. COSEWIC assessment and update status report on the Bowhead Whale Balaena mysticetus, Bering–Chukchi–Beaufort population and Eastern Canada–West Greenland population in Canada. Committee on the Status of Endangered Wildlife in Canada. Ottawa. vii + 49 pp. http://www.sararegistry.gc.ca/default.asp?lang=En&n=082503B1-1
- Curtis, T., Kvernmo, S., & Bjerregaard, P. (2005). Changing Living Conditions. International Journal Of Circumpolar Health, 64(5), 442–450. Retrieved from http://scholar.google.nl/scholar_url?url=http://journals.co-action.net/index.php/ijch/article/download/18025/20515&hl=nl&sa=T&oi=gga&ct=gga&cd=28& ei=qLMEV6esCYGTmgHoyKeQDg&scisig=AAGBfm2dQXvSs6B7HVtOYa8irnMMkP2xxw&nossl=1&ws=1280x843
- Fauchald, P., Hausner, V., Schmidt, J., & Clark, D. (2017). Transitions of social-ecological subsistence systems in the Arctic. International Journal of the Commons, 11(1). https://www.thecommonsjournal.org/articles/10.18352/ijc.698/
- George, J. C., Druckenmiller, M. L., Laidre, K. L., Suydam, R., & Person, B. (2015). Bowhead whale body condition and links to summer sea ice and upwelling in the Beaufort Sea. Progress in Oceanography, 136, 250-262. http://faculty.washington.edu/klaidre/docs/George%20et%20al.%202015.pdf
- Hauser, D. D., Laidre, K. L., Stafford, K. M., Stern, H. L., Suydam, R. S., & Richard, P. R. (2017). Decadal shifts in autumn migration timing by Pacific Arctic beluga whales are related to delayed annual sea ice formation. Global change biology, 23(6), 2206-2217.
- Hendriksen, K., & Jørgensen, U. (2015). Hunting and fishing settlements in Upernavik district of Northern Greenland – challenged by climate, centralization, and globalization. Polar Geography, 38(2), 123–145. http://doi.org/10.1080/1088937X.2015.1034222
- Hobbie, J.E., Shaver, G.R., Rastetter, E.B., Cherry, J.E., Goetz, S.J., Guay, K.C, Gould, W.A. & Kling, G.W. (2017). Ambio 46 (Suppl 1): 160. https://doi.org/10.1007/s13280-016-0870-x
- Huntington, H. P., Quakenbush, L. T., & Nelson, M. (2016). Effects of changing sea ice on marine mammals and subsistence hunters in northern Alaska from traditional knowledge interviews. Biology Letters, 12(8), 20160198. http://rsbl.royalsocietypublishing.org/content/roybiolett/12/8/20160198.full.pdf
- Kofinas, G. P., Chapin, F. S., BurnSilver, S., Schmidt, J. I., Fresco, N. L., Kielland, K., ... & Rupp, T. S. (2010). Resilience of Athabascan subsistence systems to interior Alaska’s changing climate This article is one of a selection of papers from The Dynamics of Change in Alaska’s Boreal Forests: Resilience and Vulnerability in Response to Climate Warming. Canadian Journal of Forest Research, 40(7), 1347-1359. https://www.fs.fed.us/pnw/pubs/journals/pnw_2010_kofinas001.pdf
- Koptseva, N. P., & Kirko, V. I. (2014). Ethic identification of indigenous people of the Siberian Arctic. American Journal of Applied Sciences, 11(9), 1573-1577.
- Lougheed, T. (2010). The Changing Landscape of Arctic Traditional Food. Environmental Health Perspectives, 118(9), a386–a393. https://ehp.niehs.nih.gov/118-a386/
- Markus, T., Stroeve, J. C., & Miller, J. (2009). Recent changes in Arctic sea ice melt onset, freezeup, and melt season length. Journal of Geophysical Research: Oceans, 114(C12). http://onlinelibrary.wiley.com/doi/10.1029/2009JC005436/epdf
- Moerlein, K. J., & Carothers, C. (2012). Total Environment of Change: Impacts of Climate Change and Social Transistions on Subsistence Fisheries in Northwest Alaska. Ecology and Society, 17(1), 10. https://www.ecologyandsociety.org/vol17/iss1/art10/
- Moore, S. E., & Huntington, H. P. (2008). Arctic marine mammals and climate change: impacts and resilience. Ecological Applications, 18(sp2). http://www.westcoast.fisheries.noaa.gov/publications/protected_species/marine_mammals/cetaceans/gray_whales/ studies_under_review/moore_and_huntington_2008.pdf
- Moore, S. E., & Laidre, K. L. (2006). Trends in sea ice cover within habitats used by bowhead whales in the western Arctic. Ecological Applications, 16(3), 932-944. https://staff.washington.edu/klaidre/docs/MooreandLaidre_2006.pdf
- Nicholson KL, Arthur SM, Horne JS, Garton EO, Del Vecchio PA (2016). Modeling Caribou Movements: Seasonal Ranges and Migration Routes of the Central Arctic Herd. Welker JM, ed. PLoS ONE. 2016;11(4):e0150333. http://journals.plos.org/plosone/article?id=10.1371/journal.pone.0150333
- Nickels, S., Furgal, C., Buell, M.& Moquin, H. (2005). Unikkaaqatigiit – Putting the Human Face on Climate Change: Perspectives from Inuit in Canada. Ottawa: Joint publication of Inuit Tapiriit Kanatami, Nasivvik Centre for Inuit Health and Changing Environments at Université Laval and the Ajunnginiq Centre at the National Aboriginal Health Organization. 129p. https://www.itk.ca/wp-content/uploads/2016/07/unikkaaqatigiit01-1.pdf
- Nuttall, M., Berkes, F., Forbes, B., Kofinas, G., Vlassova, T., & Wenzel, G. W. (2005). Hunting, herding, fishing, and gathering: Indigenous peoples and renewable resource use in the Arctic. In Arctic Climate Impact Assessment (pp. 649–690). New York, NY, USA: Cambridge University Press. Retrieved from http://www.acia.uaf.edu/PDFs/ACIA_Science_Chapters_Final/ACIA_Ch12_Final.pdf
- Parker, K. L., Barboza, P. S., & Stephenson, T. R. (2005). Protein conservation in female caribou (Rangifer tarandus): effects of decreasing diet quality during winter. Journal of Mammalogy, 86(3), 610-622. http://web.unbc.ca/~parker/Pubs/ParkerBarbozaStephenson%202005JMamm.pdf
- Pearce, T., Ford, J., Willox, A. C., & Smit, B. (2015). Inuit traditional ecological knowledge (TEK), subsistence hunting and adaptation to climate change in the Canadian Arctic. Arctic, 233-245. http://arctic.journalhosting.ucalgary.ca/arctic/index.php/arctic/article/download/4475/4592
- Quakenbush, L., Citta, J., George, J. C., Heide-Jørgensen, M. P., Small, R., Brower, H., ... & Pokiak, C. (2012). Seasonal movements of the Bering-Chukchi-Beaufort stock of bowhead whales: 2006–2011 satellite telemetry results. Int Whal Comm Sci Report SC/64/BRG1. http://www.north-slope.org/assets/images/uploads/SC-64-BRG1.quakenbush_et_al.2012.pdf
- Reilly, S.B., Bannister, J.L., Best, P.B., Brown, M., Brownell Jr., R.L., Butterworth, D.S., Clapham, P.J., Cooke, J., Donovan, G., Urbán, J. & Zerbini, A.N. 2012. Balaena mysticetus. The IUCN Red List of Threatened Species 2012: e.T2467A17879018. http://dx.doi.org/10.2305/IUCN.UK.2012.RLTS.T2467A17879018.en. Downloaded on 11 April 2017.
- Sakakibara, C. (2017). People of the Whales: Climate Change and Cultural Resilience Among Iñupiat of Arctic Alaska. Geographical Review, 107(1), 159-184. http://onlinelibrary.wiley.com/doi/10.1111/j.1931-0846.2016.12219.x/epdf
- Searles, E. N. (2008). Inuit identity in the Canadian Arctic. Ethnology, 47(4), 239–255. http://220.127.116.11/Documents/SociologyAnthropology/Inuit%20Identity%20in%20the%20Canadian%20Arctic.pdf
- Seersholm, F. V., Pedersen, M. W., Søe, M. J., Shokry, H., Mak, S. S. T., Ruter, A., ... & Meldgaard, M. (2016). DNA evidence of bowhead whale exploitation by Greenlandic Paleo-Inuit 4,000 years ago. Nature Communications, 7. https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5105157/
- Sharma, S., S. Couturier & S.D. Côté, 2009. Impacts of climate change on the seasonal distribution of migratory caribou. Global Change Biology 15(10): 2549-2562. http://onlinelibrary.wiley.com/doi/10.1111/j.1365-2486.2009.01945.x/abstract
- Stroeve, J. C., Markus, T., Boisvert, L., Miller, J., & Barrett, A. (2014). Changes in Arctic melt season and implications for sea ice loss. Geophysical Research Letters, 41(4), 1216-1225. http://onlinelibrary.wiley.com/doi/10.1002/2013GL058951/full
- Suydam, R. S., & George, J. C. (2004). Subsistence harvest of bowhead whales (Balaena mysticetus) by Alaskan Eskimos, 1974 to 2003. Unpublished Report SC/56/BRG12. Cambridge, UK: IWC. http://www.north-slope.org/assets/images/uploads/1974-2003%20Village_harv%20BRG12.pdf
- Thomson, J., Fan, Y., Stammerjohn, S., Stopa, J., Rogers, W. E., Girard-Ardhuin, F., ... & Ackley, S. (2016). Emerging trends in the sea state of the Beaufort and Chukchi seas. Ocean Modelling, 105, 1-12. http://www.sciencedirect.com/science/article/pii/S1463500316300622
- Thompson, D. W., & Wallace, J. M. (1998). The Arctic Oscillation signature in the wintertime geopotential height and temperature fields. Geophysical research letters, 25(9), 1297-1300. http://onlinelibrary.wiley.com/doi/10.1029/98GL00950/pdf
- Wiig, Ø., Bachmann, L., Heide-Jørgensen, M. P., Laidre, K. L., Postma, L. D., Dueck, L., & Palsbøll, P. J. (2010). Within and between stock re-identifications of bowhead whales in Eastern Canada and West Greenland. Rep Int Whal Comm SC62/BRG65. https://www.researchgate.net/profile/Mads_Peter_Heide-Jorgensen/publication/242554307_Within_and_between_stock_re-identifications_of_bowhead_whales_in_Eastern_Canada_and_West_Greenland/links/0a85e52de97bf8f101000000.pdf
- Yannic, G., Pellissier, L., Ortego, J., Lecomte, N., Couturier, S., Cuyler, C., ... & Kolpashikov, L. (2014). Genetic diversity in caribou linked to past and future climate change. Nature Climate Change, 4(2), 132-137.