Benjamin Leigh Smith was born on 12 March 1828 at Whatlington, East Sussex, a son of Benjamin Smith (1783–1860). The family into which he was born carried a strong independent line of thought and adherence to often unpopular views from one generation to the next. William Smith, our subject's grandfather, was a staunch supporter of William Wilberforce and his advocacy of the abolition of slavery. William also supported the views of the American rebels and refused to seek compensation for the loss of family estates in Savannah after the Declaration of Independence. William's son Benjamin, a friend of Thackeray and Member of Parliament for Norwich, 1834–37, was a radical politician and advocate of the repeal of the corn laws. Benjamin senior, a convinced Unitarian, had strong views on the education of his children, and when very young they were taught in what, even now, might be regarded as a progressive manner. A committee, headed by Smith and Lord Brougham, gave funds for the Westminster Infant School which provided elementary education for about 100 poor children in the neighbourhood. Whenever young Benjamin and his brothers and sisters were in London they attended this school which was run by James Buchanan: he had begun life as a weaver in Lanarkshire, and ran the school with the aid of his wife on Swedenborgian principles. There was no corporal punishment; outbreaks of indiscipline were overcome by Buchanan calling all the children to dance together to the sound of his flute. The lack of conventional discipline scandalized the committee and they all withdrew their support leaving Smith to foot the bill. He generously gave £1000 for building baths and a small theatre at the school. Progress was made nonetheless, and Benjamin Senior was sufficiently impressed to invite this unconventional pedagogue to the family estates and continue his children's education during the holidays.

Torngat Mountains National Park (TMNP) is Canada's newest national park, and was established in 2005. The development of the park has mirrored a change in mandate for the agency that manages it, Parks Canada. Since 2005 Parks Canada has sought to focus on ‘proactively facilitate[ing] opportunities for meaningful and memorable visitor experiences’, complimentary to maintaining the protection of ecological integrity and providing education (Parks Canada 2005, no page numbers). Under the auspices of this new multi-faceted mandate, this research note will examine the current state of tourism in TMNP, and will also evaluate some of the opportunities and challenges for the future. Within Parks Canada's Visitor experience vision 2015 statement, understanding tourism delivery in the present and future are important components of its mission, as is engagement with external partners to assist in this process. The analysis of tourism development in TMNP for this note comes from the authors' two week research trips to the park in August 2008 and July 2009, undertaken to assist Parks Canada to evaluate their current visitor experience activities and future options.

Arctic pollution has become a focus of attention as a result of the admission byRussia of former indiscriminate dumping of radioactive waste in the Kara Sea; thus, radionuclides in the Arctic Basin have become a major cause for concern. Evidence for the bioaccumulation of toxic contaminants such as organochlorines, PCBs, and heavy metals in the Arctic food webwould seem to raise questions about this issue, there being little evidence of significant levels of radionuclide contamination in higher orders of the chain. However, there is growing evidence of a major influx of toxic material into the Arctic Basin, from riverine input and atmospheric deposition, which is transported to biologically active melt fronts. This suggests thatthe serious polluting of the Arctic Basin, combined with bioaccumulation processes, particularly for organochlorines and trace metals, is a major cause for concern. There is, then, a requirement for an overview of current information on Arctic pollutants, with a consideration of source, transport, and accumulation processes, in order to be able to apply some perspective to the situation, to quantify and qualify the problems, and to suggest appropriate actions.

Following Cook's historic circumnavigation (1772–75) of the globe in Antarctic waters and his reports of great numbers of seals on South Georgia, considerable numbers of commercial sealing expeditions had made new discoveries of islands in the vicinity of the Antarctic Peninsula. However, not until 1819 was another government-sponsored exploring and scientific expedition organized to continue the search for the then still-unknown southern continent. This time the expedition was a Russian one, and in command of the two-ship squadron was Thaddeus Bellingshausen, then a lieutenant in the Black Sea Fleet; previously he had sailed around the world in an expedition under Kruzenstern in 1803–06. He also gained much experience in coastal surveying and charting in the Black Sea. The two ships in the squadron were Vostok (985 tonne, 117 men) under Bellingshausen's command, and Mirnyy (884 tonne, 73 men) under Lt Mikhail Lazarev, who had served for several years in the British Navy. Bellingshausen, in the opinion of some, merits equal consideration as a navigator and seaman with Cook (Debenham, 1945, p xi, xiii; Barratt, 1981, p 202). He, himself, had a high admiration for Cook and drew heavily upon Cook's narratives for guidance in sailing the. Southern Ocean. The aim of the expedition, according to a letter by the Minister of Marine to Bellingshausen, was ‘to carry out a voyage of discovery in the high southern latitudes, and to circumnavigate the ice-belt of the southern Polar Circle.’ (Debenham, 1945, p 6). The two ships sailed from Kronshtadt on 14 July 1819f and returned to that port on 5 August 1821 having achieved the aim of the expedition, spending two summer seasons in Antarctic waters and one season exploring the South Pacific islands. They called at Rio de Janeiro on the outward and homeward sailings.

A previous article (Polar Record, Vol 16, No 104, p 7243 5) outlined the current results, principally from polar areas, of the Deep Sea Drilling Project (DSDP) obtained during the cruises of the Joint Oceanographic Institutions for Deep Earth Sampling (JOIDES) research vessel Glomar Challenger. An indication was given of the considerable contribution made by DSDP coring to fundamental geoscientific research. At that time only three legs had been completed in high latitudes: leg 12 in the North Atlantic Ocean, leg 18 in the North Pactific Ocean, and leg 19 in the Bering Sea. No drilling had been undertaken in Antarctic waters but the plans for such work were outlined in the article.

The Lambert Glacier system, one of the largest in Antarctica, drains from Princess Elizabeth Land into Prydz Bay, terminating in the Amery Ice Shelf, in about long 70° to 75° E.

Understanding the benefits and outcomes of Canada's public investment in Arctic science and associated community–researcher partnerships represents a significant challenge for government. This paper presents a capital assets-based approach to conceptualising northern research partnership development processes and assessing the potential outcomes. By more explicitly considering the pre- and post-partnership asset levels (that is, social, human, physical, financial and natural assets) for different collaborators, the potential benefits and challenges associated with community–researcher partnerships can be collaboratively assessed. In order to help refine this approach, we conducted a survey of those involved in developing and maintaining community–researcher partnerships across Arctic Canada. Results indicate that the proposed approach could be useful for research funding agencies seeking to better understand partnership outcomes and promote more effective community–researcher interactions. Challenges include adequately capturing the qualitative nature of different capital assets, pointing to future research and policy needs. Better understanding the role of research in northern development has the potential to improve northern research, policy and practice.

Reindeer and caribou, respectively Old World and New World forms of Rangifer tarandus, live in large groups in the boreal forest and on the Arctic tundra. Many stocks of reindeer are herded by pastoralists. This article reviews the ecology, breeding biology and herding behaviour of both forms, as revealed by recent field studies. It identifies breeding synchrony, dominance and leadership as important aspects of their social organization, mediated by a system of signals that keep the herds together, and discusses the significance of pastoral practices that maintain herd organization and make reindeer herding possible.

Recent initiatives in polar research like Women in Polar Science and Women of the Arctic have shone a light on the strengths of female polar researchers and the struggles they have faced in their respective careers. These initiatives have started and contributed to ongoing conversations in the polar research community about increasing diversity and making the field more inclusive. In this commentary, we discuss the need to focus on intersectionality in diversity, equality and inclusion initiatives in polar research, and to address intersecting barriers faced by members and would-be members of our fields. These barriers are varied, often overlapping, and include, but are not limited to: gender identity; sexuality; socio-economic status; language; disability; and race. Polar research is poised to benefit from a tremendous diversity of ideas and approaches if we as a community can fully commit ourselves to understanding and addressing overlapping, interconnected barriers to equality and progress in polar research.

The United States has sometimes been called a reluctant Arctic actor, but during its chairmanship of the Arctic Council (2015–2017) the US engaged as an active proponent of Arctic cooperation, using the region as a showcase for strong global climate policy. This paper places US Arctic policy development during the Obama presidency within a longer time perspective, with a focus on how US interests towards the region have been formulated in policies and policy statements. The paper uses frame analysis to identify overarching discourses and discusses the extent to which certain themes and political logics recur or shift over time. It highlights economic development and national competitiveness as a prominent recurring frame, but also that the policy discourse has moved from nation-building and military security towards a broader security perspective, with attention to energy supply for the US, and more recently also to the implications of climate change. Over time, there is a clear shift from reluctance towards Arctic regional cooperation to embracing it. Moreover, it highlights how different stands in relation to climate change have affected Arctic cooperation in the past and may do so again in the future.

The UN Permanent Forum on Indigenous Issues (PFII) was established on 31 July 2000 and held its first session at UN Headquarters in New York in May 2002. The result of decades of development, the forum signified an official opening of the UN to indigenous peoples' participation alongside that of states. This article analyses the discussions on the establishment of the PFII and the role of indigenous peoples as political actors in those discussions. A focus of particular interest is the contradiction between state sovereignty and indigenous self-determination. In examining the establishment process, the analysis draws on scholarship dealing with norms, institutions, organisation and legitimacy. The themes and frames used by indigenous peoples that are significant in state-indigenous relations and that have had an effect on the forum are indigenousness, self-determination, rights and recognition. These show how the relationship between state sovereignty and indigenous self-determination underlay the establishment discussions and their outcome. The materials for the article comprise the transcripts of the establishment negotiations, interventions of state and indigenous representatives, as well as literature on the political participation of indigenous peoples, international law and the UN system and indigenous peoples. The discussions are analysed textually. The article claims that, although the UN is a state-dominated organisation, indigenous peoples are nevertheless able to affect international cooperation. This is an INDIPO project paper (Tennberg 2006).

Pending land claims by Alaska Natives were extinguished by the Alaska Native Claims Settlement Act of 1971. This act marked the culmination of more than 100 years of expressed Federal concern for protection of land rights of aboriginal peoples within the region, starting with the 1867 Treaty of Cession. The Federal legislation provided both a cash and a land settlement, and mandated creation of corporations to manage the resulting assets. Two amendments, in 1976 and 1980, attempted to alleviate certain problems arising from the original act. Nonetheless, many difficulties with the act itself are becoming more apparent as the 1990s approach, and certain sections of the act such as taxation and stock alienation become activated. This paper discusses the major events leading to passage of the act, key provisions of the act, and the major controversies and conflicts facing Alaska Natives through the next two decades as a result of the legislation.

Details are provided of a sledge, possibly of late nineteenth/early twentieth century provenance, discovered on Byers Peninsula, Livingston Island, South Shetland Islands, in 2007.

US-China relations represent the most central bilateral relationship in the world, but few studies investigate the two countries’ approaches to the Arctic. This article explores the geopolitical shifts in the Arctic, and compares and contrasts American and Chinese policy in the region. The article examines to what extent the two have common or conflicting interests, and discusses the potential for US-China friction and rivalry. Some alarmist writers suggest that the future Arctic is set for confrontation. This article, however, argues that the current stakes in the circumpolar Arctic region are not sufficiently high to warrant confrontation between the two states. Cooperation predominantly guides their policies and activities. While they play different roles and increasingly seek to demonstrate their influence, there are common interests, such as in the freedom of the seas, in resource extraction and in developing infrastructure in the region.

In October 1976 HM nuclear submarine Sovereign was sent into the Arctic Ocean on a voyage to the North Pole. This was the second Royal Naval submarine deployment in the Arctic Ocean, the first being the voyage of the Dreadnought in 1971. Sovereign was accompanied by HM submarine Narwhal as far as 80°N, and within the Arctic Basin the submarine's track was flown over by a Canadian Argus maritime patrol aircraft. The Scott Polar Research Institute carried out a scientific programme from both vessels, with Dr P. Wadhams aboard Sovereign and V. A. Squire aboard Narwhal.

The climatic conditions in the Arctic, and observations of the wind-induced drift of ice made in connexion with Fridtjof Nansen's Fram expedition, led to the discovery 100 years ago by Vilhelm Bjerknes' pupil, V.W. Ekman, of the importance of the Earth's rotation in limiting the depth of the wind-induced shear current in the ocean. This essay commemorates the centenary of Ekman's seminal paper, which was published in 1905. The paper presents a concise summary of Ekman's contributions to physical oceanography and a brief review of their continuing impact. The two key concepts are the Ekman spiral (the helical rotation of the velocity vector, in atmospheric and oceanic boundary layers) and the resultant Ekman pumping (vertical motions in the water column associated with the divergence of the flow in the surface layer in the presence of a rotational wind-stress field). Later work has revealed how the magnitude and direction of the surface current relative to the wind vector is influenced by the presence of surface waves and the behaviour of the turbulent flow in the near-surface layer of the ocean. However, the structure of Ekman's original viscous coupling model remains a permanent legacy to physical oceanographers.

The Arctic and the Antarctic appear to be polar opposites with regard to many matters, including the systems of governance that have evolved in the two regions. Antarctica is demilitarised, closed to economic development, open to a wide range of scientific activities, and subject to strict environmental regulations under the terms of the legally binding Antarctic Treaty of 1959 along with several supplementary measures that together form the Antarctic Treaty System (ATS). The Arctic, by contrast, is a theatre of military operations, a site of largescale industrial activities, a homeland for sizable groups of indigenous peoples, and a focus of growing concern regarding the environmental impacts of human activities. The Arctic Council, the principal international body concerned with governance at the regional level, operates under the terms of a ministerial declaration that is not legally binding; it lacks the authority to make formal decisions about matters of current interest. Digging a little deeper, however, one turns up some illuminating similarities between the governance systems operating in the antipodes. In this article, I pursue this line of thinking, setting forth a range of observations relating to (i) the history of governance in the antipodes, (ii) institutional innovations occurring in these regions, (iii) issues of membership, (iv) jurisdictional concerns, (v) the role of science, (vi) relations with the UN system, (vii) institutional interplay, and (viii) the adaptiveness of governance systems in the face of changing circumstances. The governance systems for the polar regions are not likely to converge anytime soon. Nevertheless, this analysis should be of interest not only to those concerned with the fate of Antarctica and the Arctic but also to those seeking to find effective means of addressing needs for governance in other settings calling for governance without government.

Under the regime established by the Antarctic Treaty of 1959, decision-making remains exclusively with the limited number of states that are entitled to appoint representatives to participate in Antarctic Treaty Consultative Meetings. Whereas the 12 original signatory states have a permanent right to attend these meetings, acceding states may gain consultative status only during the time they carry out substantial scientific research in the Antarctic. This paper addresses three issues: the first relates to the problems arising out of the ‘admission procedure’ adopted by the original signatory states when faced with the first application of an acceding state to become an Antarctic Treaty Consultative Party, a procedure that has been applied ever since to similar cases. The second looks at the forms of scientific research activities an acceding party ought to conduct in Antarctica in order to meet the requirements laid down in the Antarctic Treaty. The third deals more generally with the issue of limited participation in the Antarctic Treaty decision-making process, which has come under severe criticism from non-Consultative Parties and states that have not acceded to the Treaty.

The third-quarter phenomenon is the dominant theoretical model to explain the psychological impacts of deployment in Antarctica on personnel. It posits that detrimental symptoms to functioning, such as negative mood, increase gradually throughout deployment and peak at the third-quarter point, regardless of overall deployment length. However, there is equivocal support for the model. The current meta-analysis included data from 21 studies (involving 1,826 participants) measuring negative mood during deployment to elucidate this discrepancy. Across studies analyses were conducted on three data types: stratified by month using repeated-measured all time points meta-analytic techniques and pre/post-deployment data for summer/winter deployment seasons. Our results did not support the proposed parameters of the third-quarter phenomenon, as negative mood did not peak at the third-quarter point (August/September) of deployment. Overall effect sizes indicated that negative mood was greater at baseline than the end of deployment for summer and winter deployment seasons. These findings have theoretical and practical implications and should be used to guide future research, assisting in the development and modification of pre-existing prevention and intervention programmes to improve well-being and functioning of personnel during Antarctic deployment.