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The global population and status of Snowy Owls Bubo scandiacus are particularly challenging to assess because individuals are irruptive and nomadic, and the breeding range is restricted to the remote circumpolar Arctic tundra. The International Union for Conservation of Nature (IUCN) uplisted the Snowy Owl to “Vulnerable” in 2017 because the suggested population estimates appeared considerably lower than historical estimates, and it recommended actions to clarify the population size, structure, and trends. Here we present a broad review and status assessment, an effort led by the International Snowy Owl Working Group (ISOWG) and researchers from around the world, to estimate population trends and the current global status of the Snowy Owl. We use long-term breeding data, genetic studies, satellite-GPS tracking, and survival estimates to assess current population trends at several monitoring sites in the Arctic and we review the ecology and threats throughout the Snowy Owl range. An assessment of the available data suggests that current estimates of a worldwide population of 14,000–28,000 breeding adults are plausible. Our assessment of population trends at five long-term monitoring sites suggests that breeding populations of Snowy Owls in the Arctic have decreased by more than 30% over the past three generations and the species should continue to be categorised as Vulnerable under the IUCN Red List Criterion A2. We offer research recommendations to improve our understanding of Snowy Owl biology and future population assessments in a changing world.
Hunting pits are common archaeological features in northern landscapes, mainly researched from a morphological perspective, as dateable material is scarce. This has resulted in a limited and generalized understanding of hunting pits. While human land use in non-agrarian settings is often subtle, it can still be understood in terms of distribution and management by using relational approaches that address spatial organization and the nature of land use. This study, based on extensive field surveys and GIS analyses and guided by the concept of landscape domestication, has identified the characteristics of approximately 1500 previously unrecorded hunting pits in the Arctic region of Sweden. It examines how hunting pit systems, their selective spatial distribution, and strategic arrangement can be seen as expressions of landscape domestication. The author concludes that, through profound knowledge and deliberate resource management, communities invested in the landscape, generating dense spatial and temporal manifestations in the form of hunting pits. These systems reflect an elaborate hunting technique involving the whole landscape.
Edited by
Ottavio Quirico, University of New England, University for Foreigners of Perugia and Australian National University, Canberra,Walter Baber, California State University, Long Beach
Links between the Arctic and the Earth’s climate system generate several paradoxes. Despite the low level of anthropogenic emissions of GHGs from the Arctic, it plays a critical role in the dynamics of the Earth’s climate system. The principal drivers of climate change are non-Arctic, but climate change impacts show up sooner and more dramatically in the Arctic, making it ground zero in efforts to address the challenge of climate adaptation. Ironically, these changes have also increased the accessibility of the massive reserves of hydrocarbons located in the circumpolar north. The Arctic Council has sought to address these concerns by monitoring the course of climate change in the Arctic and bringing together representatives of major GHG emitters to consider options for addressing climate change, but the council is limited in terms of authority and resources; Russia’s war in Ukraine has disrupted its activities. The paradoxical links arising in this case are characteristic of complex systems more generally and highlight the importance of developing the ability to respond agilely when needs and opportunities to deal effectively with rapidly changing conditions arise.
Bortolanite, a rare mineral of the rinkite group, seidozerite supergroup occurs in two different associations in the Lovozero massif in the Kola Peninsula, Russia: (1) together with ferri-katophorite and phlogopite, it forms porous or mesh aggregates (symplectitic accretions) with euhedral contours in the contact zone of a volcano–sedimentary xenolith and eudialyte lujavrite at Kuamdespakhk Mt and (2) in intergrowths with titanite and fluorcaphite in the poikilitic feldspathoid syenites at Sengischorr Mt. In both cases, bortolanite was found in association with rosenbuschite that is close to it in chemical composition, but unlike bortolanite, it contains no REEs. The mineral is triclinic, space group P$\bar{1}$, a = 9.5807(5), b = 5.6943(4), c = 7.2813(4) Å, α = 89.891(5)°, β = 100.959(4)°, γ = 101.241(5)°, V = 382.25(4) Å3 and Z = 1.
The Lovozero bortolanite differs from the Brazilian holotype sample from de Caldas alkaline massif, Minas Gerais, due to the presence of (OH)-groups in its composition, which is indicated by Raman data. A combination of single-crystal X-ray diffraction data and electron microprobe data provides the following crystal-chemical formula: (Ca1.97Ce0.01Nd0.01Th0.01)Σ2(Ca1.39Zr0.61)Σ2(Na0.72Ca0.28)Σ1(Na1.36Ca0.56Mn0.03Zn0.01)Σ1.96(Ti0.78Zr0.08Nb0.05Mg0.05Fe0.04)Σ1Si4O14((OH)0.92O0.87F0.21)Σ2F2.
As a result of anthropogenic climate change, Inuit in the Arctic and island inhabitants in the Pacific Ocean both experience interrelated changes in their maritime environments. Global warming causes Arctic ice to melt, which leads to rising sea levels. As a result, local inhabitants in both regions experience the disappearance of their space (land and ice), paired with the arrival of new stakeholders with a diverse range of interests in the areas. As the inhabitants of the regions most vulnerable to the effects of climate change, Inuit and Pacific Islanders have engaged in counter-mapping and counter-narrating their space that colonial powers have previously conceptualized as isolated, remote, and peripheral. In contrast, the maps of Inuit Nunangat and the Blue Pacific illustrate and tell the stories of transnational spaces that have been collectively shared and used since time immemorial. These counter-mapping and counter-narrative approaches shape a new perception of the regions. This chapter contributes to conceptual development of environmental violence by discussing case studies of counter-mapping and counter-narration in the Arctic and the Pacific Ocean – as locals’ responses to experiences of structural and cultural violence to overcome their vulnerability, challenge power differentials, and satisfy their human needs.
While much work on expertise has explored the mobilisation and production of knowledge, the development of epistemic communities, and the mechanisms through which expertise operates – little work has been done exploring how expertise is understood across academic literature on particular regional cases such as the Arctic. In this article, I scope a broad literature review of the Arctic, seeking out how expertise has been depicted and framed in academic and theoretical literature. The results are framed around five different themes: (1) expertise serving the interests of great powers, (2) recognition of the overall importance of expertise in Arctic governance, (3) the purpose of experts, (4) science diplomacy and expertise: a murky barrier, and (5) how to study experts, but also find that Indigenous knowledge is often left out of literature that relies upon Western frameworks of expertise. This incongruity suggests that there are two competing conceptualizations of Arctic expertise, one in theory and another in practice – which has consequences for how the region and its expertise are narrated.
This study investigates the impacts of the timing of an extreme cyclone that occurred in August 2012 on the sea-ice volume evolution based on the Arctic Ice Ocean Prediction System (ArcIOPS). By applying a novel cyclone removal algorithm to the atmospheric forcing during 4–12 August 2012, we superimpose the derived cyclone component onto the atmospheric forcing one month later or earlier. This study finds that although the extreme cyclone leads to strong sea-ice volume loss in all runs, large divergence occurs in sea-ice melting mechanism in response to various timing of the cyclone. The extreme cyclone occurred in August, when enhanced ice volume loss is attributed to ice bottom melt primarily and ice surface melt secondarily. If the cyclone occurs one month earlier, ice surface melt dominates ice volume loss, and earlier appearance of open water within the ice zone initiates positive ice-albedo feedback, leading to a long lasting of the cyclone-induced impacts for approximately one month, and eventually a lower September ice volume. In contrast, if the cyclone occurs one month later, ice bottom melt entirely dominates ice volume loss, and the air-open water heat flux in the ice zone tends to offset ice volume loss.
Interferometric synthetic aperture radar (InSAR) data suffer from an elevation bias due to signal penetration into the firn and ice surface, rendering the height information unusable for elevation and mass-change detection. This study estimates the penetration bias in X-band InSAR data to quantify its impact on elevation and mass-change detection and to demonstrate the applicability of TanDEM-X digital elevation models (DEMs) for cryosphere research. To achieve this, a multiple linear regression model is applied to a time series of four TanDEM-X DEMs acquired between 2010 and 2018 over the Sverdrup Glacier basin (SGB), Devon Ice Cap, Canada. The resulting penetration corrected TanDEM-X DEMs agreed to within ±14 cm of spatially and temporally coincident precise in situ kinematic dGPS data (±10 cm RMSE). Additionally, multi-year estimations of mass change for the SGB derived from differencing TanDEM-X DEMs over multi-year periods between 2010 and 2018, showed good agreement with mean deviation of 338 ± 166 mm w.e. with independent measurements of mass change derived from annual in situ surface mass balance over the same time periods. The results show that the penetration bias can vary significantly, leading to random under- and overestimations in the detection of elevation and mass changes.
Although “urban” and “fisheries” are not commonly paired in the analyses of either urbanism or fisheries governance, today’s large-scale fisheries are often closely organised in connection with cities. In this paper, I build on a feminist perspective and urban studies to examine the makings of a city through contemporary fisheries. Drawing upon observations and interviews conducted in Tromsø, Norway, which is a key site for Arctic fisheries, I review how fish and fisheries are simultaneously made visible and invisible in urban spheres. By analysing the gendered structures and valuations that organise the city–fisheries relations, I introduce three “fishy” windows to demonstrate the kinds of development and future pathways for fisheries that are considered relevant and rational in and for the city. In particular, I discuss how the historical, techno-masculine narratives of mastering Arctic nature frame and legitimise fisheries practices as they expand throughout Tromsø. The study builds on the emerging research on Arctic urbanism to highlight the need to better integrate gendered analyses of the “urban” into social science research on natural resource extraction.
Much has been written about the so-called Franklin expedition (1845–), but not about the master mariners, who joined as “Greenland pilots,” as experienced whaling masters on Royal Navy expeditions were usually called in the 19th century. Having been on Royal Navy expeditions to the Arctic before, Thomas Blanky, the ice master of HMS Terror, was mentioned here and there in contemporary sources. But who he was and how and why he joined the expedition are still widely unanswered questions, to be dealt with for the first time here.
China’s role in the Arctic regime remains a debatable topic in the expert discourse on the High North. Currently, in view of the aggravated conflicts in other regions that include Russia as the largest Arctic state, and China as its strategic partner, the Arctic regimes are experiencing salient disturbances. Against this backdrop, an understanding of China’s opportunities to affect Arctic affairs is urgently needed. We address this issue by combining political and legal analyses. We used the regime theory approach to outline the Arctic regime complex (ARC), and through this lens, we discuss the recent changes that are being observed. Based on this, we determine China’s actual potential for making amendments to the ARC. We conclude that China has no capacity to make a crucial shift in the ARC, but it is still able to alter particular rules, like those related to Arctic Ocean management and scientific cooperation. The further efficient operation of the Arctic Council will play a decisive role in envisaging China’s behaviour in the region.
Russia’s Arctic policy since 2008 has been influenced by two competing foreign policy lines (discourses): the “Arctic as a resource base” and the “sovereignty discourse”. The “Arctic as a resource base” has been the dominant one since the first Russian Arctic Strategy in 2008. It is primarily about exploiting the vast oil and gas resources estimated to be located there, as well as turn the Northern Sea Route into a “global transport corridor”. In Russia’s Arctic Strategy of 2020, however, there is enhanced emphasis on sovereignty and power balancing in Russian Arctic policy. And the focus on sovereignty was heightened with the amendments to Russia’s Arctic Strategy in March 2023. This increased emphasis on sovereignty, territorial defence and balance of power in Russian Arctic policy is likely to be further reinforced by the growing great-power competition between the USA and Russia, which has gained new momentum following Russia’s invasion of Ukraine in 2022.
In 1866, Charles F. Hall recorded testimony from a Pelly Bay native named Sŭ-pung-er who reported that together with his uncle, they had visited the Northwest coast of King William Island 4 years prior in search of materials abandoned by the Franklin Expedition. Sŭ-pung-er told Hall that he had identified a site which Hall believed was a “vault” which might contain documents and speculated that it could have been a burial site for a high-ranking officer. Sŭ-pung-er’s testimony also included the description of a wooden “pillar, stick or post” which marked the spot of the vault. The location of this site and the pillar have never been found. Yet they remain sought-after for both their significance and the potential bonanza of information about the expedition. Any clue or artefact, which could provide clarity for this site, is therefore of great value. This paper describes a model of the pillar seen on King Williams Island, replicated by Sŭ-pung-er, which Hall brought back from the Arctic and included in his list of Franklin relics. The model, now housed in the Smithsonian Museum of American History, was first featured in a drawing of relics appearing in 1869 in Harper’s Weekly magazine. The fact that this artefact has been in plain sight for so long, but unrecognised for what it is, is significant. The pillar model both provides clarity and continues the mystery surrounding the Franklin Expedition.
The book ends in 1940, on the cusp of change that came with the militarization of the North during the Second World War and the Cold War. This was also when the Canadian government asserted greater control over the North, including over healthcare. Epidemics that arrived with resource workers, military, and state personnel, were interpreted by southern observers as ‘virgin soil epidemics’ in ‘isolated’ populations. These epidemics and their northern setting influenced biomedical research into the nature of immunity that was significant to the history of medicine.
Twentieth-century circumpolar epidemics shaped historical interpretations of disease in European imperialism in the Americas and beyond. In this revisionist history of epidemic disease as experienced by northern peoples, Liza Piper illuminates the ecological, spatial, and colonial relationships that allowed diseases – influenza, measles, and tuberculosis in particular – to flourish between 1860 and 1940 along the Mackenzie and Yukon rivers. Making detailed use of Indigenous oral histories alongside English and French language archives and emphasising environmental alongside social and cultural factors, When Disease Came to this Country shows how colonial ideas about northern Indigenous immunity to disease were rooted in the racialized structures of colonialism that transformed northern Indigenous lives and lands, and shaped mid-twentieth century biomedical research.
‘The Arctic sublime’ was a Romantic subcategory in its own right because of the period’s fascination with Arctic vastness and awe-inspiring icescapes. This chapter examines some of the famous representations of the Arctic sublime, including Mary Shelley’s Frankenstein and Caspar David Friedrich’s painting Das Eismeer, but also lesser-known texts that illustrate the intense contemporary engagement with northern climes. The sources that were available to the public and helped create an image of the Arctic were not only literary or artistic representations but also travel accounts and stories of shipwrecks. The chapter traces the patriotic celebrations of explorers braving the deadly terrors of the Arctic as well the discourse that developed around the optical mirages and illusions in high latitudes. The latter are particularly pertinent as they fitted into a Burkean sense of sublime psychological disruption and disorientation. The chapter shows how the public could – virtually – occupy the Arctic and experience the thrill of its sublime landscapes in books and at exhibitions, while the actual Arctic remained enigmatic and unconquerable.
Recent years have shown that international science dialogue exists at the edge of turbulence and is disturbed by different geopolitical events. The notion of science diplomacy has taken the critical discourse to different levels of actors. Such a discourse exposes the epistemological ambivalence and methodological imbalance of both science and diplomacy in this phenomenon. Current geopolitical conditions have revealed new edges of science diplomacy instruments that spread from “soft” to “hard” practices. Different levels of dialogue and cooperation have shown different examples of resilience and adaptability (or the opposite) to the external turbulence. The phenomenon of regionalisation in science diplomacy is facing criticism from the science community while the current geopolitical situation has dramatically influenced the Arctic science dialogue, as well as governance practices. This commentary discusses particular examples of existing Arctic science diplomacy practices in current geopolitical conditions which are reflected in the Arctic theoretical and practical discourse.
The first part of the chapter examines how the loss of the Christian colony became a prism through which it was possible to reflect on the two globalising European projects of the nineteenth century: colonialism and Christian mission. The ‘lost colony’ in Greenland came to function as a mirror for contemporary anxieties about the danger of settling far from European metropoles. Analysis of available sources shows that this fear was fed by anecdotal evidence that the European Greenlanders had lost their Christian faith and descended into savagery. The second part of the chapter explores a series of significant themes in eighteenth- and early nineteenth-century literary representations of the Christian mission in Greenland. As the old colonists had been Christian and new missions were now making progress, a ‘fall-and-restoration’ structure became embedded in several texts. The most notable example is the British poet James Montgomery’s Greenland (1819), a text neglected in modern criticism despite the fact that it enjoyed significant popularity in the Romantic period.
The chapter examines the rhetoric of imperialism in the period leading up to the Danish recolonisation of Greenland in 1721 (and its immediate aftermath). English privateer Martin Frobisher’s expeditions in the late sixteenth century first gave impetus to the search for riches in the Arctic. The slew of texts published in the wake of Frobisher’s expeditions provided the nation with the image of courageous Englishmen establishing claims to lands in the North Atlantic. The chapter analyses English writings that allude to Greenland in ways that constitute claims to land. However, these claims were not uncontested. The Danish crown sent out expeditions in the early seventeenth century, which were also documented in the medium of print. It is the aim to show how Danish endeavours can be seen partly as a response to English activity. A significant part of the chapter is therefore an inquiry into how Danish writers attempted to ascertain Greenland as a land belonging to the Dano-Norwegian crown.