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See all EU institutions and bodiesHuman settlements at risk of permafrost thaw by 2060
Source: Ramage et al., 2021
The map shows current (2017) settlements on permafrost (i) threatened by permafrost thaw where people will have to adapt to changes related to permafrost loss by 2060 (brown dots), and (ii) those that will remain permafrost settlements in 2060 (green dots). Of all European permafrost settlements, only 2 settlements in Norway and less than half of the currently existing settlements in Greenland will still be located on permafrost by 2060.
Health issues
Permafrost is the year-round frozen layer of soil and rock, which covers one quarter of the earth’s northern hemisphere. It is overlaid by an ‘active layer’ of soil that thaws and freezes seasonally, can support plant growth, and at the same time serves as insolation keeping the permafrost temperature below 0°C. In Europe, permafrost is found in the polar regions of the high arctic of Svalbard and in northern parts of the Nordic countries, as well as in the high-altitude mountains of the Nordics and the Alps. Global warming is causing permafrost to thaw, which can adversely affect human health via several pathways including water quality, physical hazards, infrastructure damage, hazardous waste release, agriculture, food security and safety, and exposure to pathogens.
Water quality
Permafrost thaw releases groundwater from frozen soils, changing hydrological pathways, creating more run-off and affecting the groundwater recharge processes. Permafrost thaw also releases naturally stored trace elements (including mercury) and major ions into waterways (Colombo et al., 2018; Lamontagne-Hallé et al., 2018). This deteriorates the drinking water quality, which if consumed in high quantities, can lead to developmental, immune-and reproductive disorders, neurotoxicity, cancer and other health impacts (WHO, 2022).
Physical hazards, infrastructure damage and release of hazardous waste
Permafrost degradation and thaw can cause movement of frozen debris and landslides, posing a direct threat to people. It also reduces the stability of infrastructure (including buildings, roads, railway lines), which may result in reduced access to essential services for already remote communities. This can severely impact the livelihoods of local communities, leading to mental (Bell et al., 2010) and physical health impacts, including injuries and fatalities (IPCC, 2022). Permafrost thaw can also destabilise industrial sites (including waste storage and disposal infrastructure) and cause damage to landfills, drilling sites, storage tanks and pipelines, thereby posing health threats to people. Moreover, hazardous substances, including chemical and radioactive waste, previously stored in permafrost may also be released (Langer et al., 2023). Contact with these hazardous materials can lead to a number of health risks, including radiation sickness, cancer and physiological impairments (Miner et al., 2021).
Agriculture, food security and safety
Changes to permafrost affects agriculture and reindeer-husbandry, which directly impacts the livelihoods of local communities reliant on these practices, leading to high stress levels and poor mental health, as well as poor physical health from reduced water and food availability (Jungsberg et al., 2022). Permafrost thaw can also lead to food contamination and associated food-borne diseases in local communities due to the lower effectiveness of permafrost for natural food refrigeration (Parkinson and Evengård, 2009).
Mercury released by permafrost thaw can also pose health risks via the food chain as the highly potent neurotoxin methyl mercury accumulates in fish and artic mammals such as seals (WHO, 2017). People living in the Artic are particularly at risk of mercury poisoning and associated developmental and neurological diseases (such as the Minamata disease) as fish and artic mammals constitutes a large proportion of the diet (Nedkvitne et al., 2021).
Increased exposure to pathogens
Permafrost thaw may also lead to increased exposure to pathogens, both directly through the release of pathogens previously frozen in permafrost (Miner et al., 2021), and indirectly through improved conditions for disease transmission (e.g., wet or bog-like soils favour mosquito breeding conditions and the expansion of vector-borne diseases; nutrient-richer water due to thawing permafrost increases pathogen virulence in fish and increases the risk for food-borne diseases) (Wu et al., 2022; Wedekind et al., 2010). Particularly warm years have been associated with increased risks of the release of previously frozen anthrax bacteria and anthrax outbreaks, a serious threat to both human health and the livestock (i.e., their source of income) of Arctic herding communities (Stella et al., 2020).
Observed effects
Permafrost temperatures have increased in most areas since the early 1980s due to increased air temperature and changes in snow cover (IPCC, 2022). Widespread permafrost degradation has been observed in the southern Arctic especially, in the Nordics. Yet, a systematic European-wide assessment of impacts of permafrost thaw for people in Europe is lacking and instead mostly sporadic evidence exists. In the high arctic region of Europe, permafrost thaw mostly affects human health through community and livelihood impacts, via physical and mental impacts of compromised water quality, pathogen exposure, threats to food safety and security, and infrastructural damage, but limited recorded evidence of these impacts exists. In high-altitude regions in the Nordics and the Alps, observed health impacts of permafrost thaw relate mostly to infrastructure damage, including avalanche defence structures, and rockfall (Fischer et al., 2012; Ravanel et al., 2017) as the affected areas are often recreational zones rather than community settlements. In July 2022, high mountain permafrost thaw led to the collaps of the Marmolada glacier in the northern Italian Alps, killing 11 people and injuring 8 (Bondesan and Francese, 2023).
Projected effects
Due to global warming, around 70-75% of people and infrastructure currently in permafrost area is likely to be affected by near-surface permafrost thaw by 2050 (Hjort et al., 2018). Quantitative assessments of future permafrost thaw impacts are rare, but studies that do exist mention impacts such as changed river flow paths and runoff (Rogger et al., 2017), rockfall in mountainous areas (Mourey and Ravanel, 2017), water quality deterioration from industrial contamination (Langer et al., 2023), and increased mercury release from Northern Hemisphere permafrost, i.e., the world’s largest mercury reservoir (Schuster et al., 2018). Permafrost thaw is also expected to exacerbate disease outbreaks, which will affect human and animal health and livelihoods and wellbeing of populations in Europe’s north (Stella et al., 2020).
Policy responses
Current policy responses in the EU mostly address the permafrost thaw phenomenon rather than its health impacts specifically. Commitments to mitigating permafrost thaw and its environmental, climatic and social impacts are included in the EU Green Deal and through the EU’s Arctic policy. The EU-funded NUNATARYUK project addresses these commitments by investigating how thawing permafrost on land, along the coast, and below the sea changes the global climate and life for people in the Arctic. To effectively address the health impacts of permafrost thaw at EU or national level with adaptive actions, it would be valuable to acquire more (quantitative) knowledge on at-risk communities and their exposure pathways to permafrost thaw.
Further information
- Items in the Resource Catalogue
References
Bell, J., et al., 2010, Climate Change and Mental Health: Uncertainty and Vulnerability for Alaska Natives, Center for Climate and Health Bulletin, Alaska Native Tribal Health Consortium. Available at https://anthc.org/wp-content/uploads/2016/01/CCH-Bulletin-No-3-Mental-Health.pdf
Bondesan, A. and Francese, R. G., 2023, The climate-driven disaster of the Marmolada Glacier (Italy), Geomorphology 431, 108687. https://doi.org/10.1016/j.geomorph.2023.108687
Colombo, N., et al., 2018, Review: Impacts of permafrost degradation on inorganic chemistry of surface fresh water, Global and Planetary Change 162, 69-83. https://doi.org/10.1016/j.gloplacha.2017.11.017
Fischer, L., et al., 2012, On the influence of topographic, geological and cryospheric factors on rock avalanches and rockfalls in high-mountain areas, Natural Hazards and Earth System Sciences 12(1), 241-254. https://doi.org/10.5194/nhess-12-241-2012
Hjort, J., et al., 2018, Degrading permafrost puts Arctic infrastructure at risk by mid-century, Nature Communications 9(1), 5147. https://doi.org/10.1038/s41467-018-07557-4
IPCC, 2022, The Ocean and Cryosphere in a Changing Climate: Special Report of the Intergovernmental Panel on Climate Change, Pörtner, H.-O. et al. (eds), Cambridge University Press, Cambridge, UK and New York, USA, 755 pp. https://doi.org/10.1017/9781009157964
Jungsberg, L., et al., 2022, Adaptive capacity to manage permafrost degradation in Northwest Greenland, Polar Geography 45(1), 58-76. https://doi.org/10.1080/1088937X.2021.199506
Lamontagne-Hallé, P., et al., 2018, Changing groundwater discharge dynamics in permafrost regions, Environmental Research Letters 13(8), 084017. https://doi.org/10.1088/1748-9326/aad404
Langer, M., et al., 2023, Thawing permafrost poses environmental threat to thousands of sites with legacy industrial contamination, Nature Communications 14(1), 1721. https://doi.org/10.1038/s41467-023-37276-4
Miner, K. R., et al., 2021, Emergent biogeochemical risks from Arctic permafrost degradation, Nature Climate Change 11(10), 809-819. https://doi.org/10.1038/s41558-021-01162-y
Mourey, J. and Ravanel, L., 2017, Evolution of Access Routes to High Mountain Refuges of the Mer de Glace Basin (Mont Blanc Massif, France), Journal of Alpine Research | Revue de géographie alpine, 105-4. https://doi.org/10.4000/rga.3790
Nedkvitne, N., et al., 2021, Mercury in permafrost landscapes in the Norwegian Subarctic - current status and potential for increased release and methylation by permafrost thaw, in: EGU General Assembly 2021 (vEGU21) Conference Proceedings, April 2021. https://doi.org/10.5194/egusphere-egu21-11126
Parkinson, A. J. and Evengård, B., 2009, Climate change, its impact on human health in the Arctic and the public health response to threats of emerging infectious diseases, Global Health Action 2(1), 2075. https://doi.org/10.3402/gha.v2i0.2075
Ramage, J., et al., 2021, Population living on permafrost in the Arctic’, Population and Environment 43(1), 22-38. https://doi.org10.1007/s11111-020-00370-6
Ravanel, L., et al., 2017, Impacts of the 2003 and 2015 summer heatwaves on permafrost-affected rock-walls in the Mont Blanc massif, Science of The Total Environment 609, 132-143. https://doi.org/10.1016/j.scitotenv.2017.07.055
Rogger, M., et al., 2017, Impact of mountain permafrost on flow path and runoff response in a high alpine catchment, Water Resources Research 53(2), 1288-1308. https://doi.org/10.1002/2016WR019341
Schuster, P. F., et al., 2018, Permafrost Stores a Globally Significant Amount of Mercury, Geophysical Research Letters 45(3), 1463-1471. https://doi.org/10.1002/2017GL075571
Stella, E., et al., 2020, Permafrost dynamics and the risk of anthrax transmission: a modelling study, Scientific Reports 10(1), 16460. https://doi.org/10.1038/s41598-020-72440-6
Wedekind, C., et al., 2010, Elevated resource availability sufficient to turn opportunistic into virulent fish pathogens, Ecology 91(5), 1251-1256. https://doi.org/10.1890/09-1067.1
WHO, 2017, Mercury and health fact sheet. Available at https://www.who.int/news-room/fact-sheets/detail/mercury-and-health
WHO, 2022, Guidelines for drinking-water quality, 4th edition, WHO, Geneva. Available at https://iris.who.int/bitstream/handle/10665/352532/9789240045064-eng.pdf?sequence=1
Wu, R., et al., 2022, Permafrost as a potential pathogen reservoir’, One Earth 5(4), 351-360. https://doi.org/10.1016/j.oneear.2022.03.010
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