On 18 June 1928, Roald Amundsen and a team of five men (René Guilbaud, Leif Dietrichson, Albert Cavelier de Cuverville, Gilbert Brazy and Emile Valette) flew in a French Latham 47 prototype aeroplane from Tromsø, Norway, to aid in the rescue of survivors of the crashed airship Italia. The party disappeared nearly without trace into the Barents Sea. We shall examine Amundsen's last years, the decision to employ for an Arctic relief mission a prototype aeroplane which had not completed its flight tests, and the evidence that, in deciding to disregard warnings and fly this aeroplane unaccompanied over the Barents Sea, Amundsen took a significant risk that led to his death and those of his crew.

In the summer of 1880, the British explorer Benjamin Leigh Smith made the first reconnaissance of the western reaches of Zemlya Frantsa-Iosifa [Franz Josef Land] in the specially built polar research vessel Eira. This was the first expedition to go ashore in the archipelago after its acknowledged discovery by Weyprecht and Payer in 1873. Combined with his brief reconnaissance in 1881 before Eira sank near Cape Flora, Leigh Smith added a total of 41 place names, 37 of which are still in use, to its geographic nomenclature during his two expeditions, 1880 (39 place names) and 1881–1882 (2). The 1880 names were a post-expedition collaboration, between Leigh Smith and Clements Markham, Secretary of the Royal Geographic Society (RGS). Leigh Smith provided the names of colleagues and scientists who had either been with him in 1880 or on one of his earlier expeditions to Svalbard, or those of favoured relatives, while Markham, along with Sir George Nares as an RGS peer reviewer, added the names of particularly influential individuals in geographical circles as well as a variety of museum curators who identified natural history collections returned by the expedition. Additionally, two place names are connected to the Dutch Willem Barents expedition of 1879.

With the melting of sea ice in the Arctic, the potential for higher shipping access has markedly changed. Shipping activity in the Arctic is increasing, including tourism and exploration activities, underlining the need for reliable communication and monitoring. This article examines the interactions between climate and sea ice change, the patterns of cruise ship tourism through Arctic Canada and the interest of operators to increase their activities in the cruise tourism market in the region. Since 1995, the melting of the summer pack ice in the offers the possibilities of increased shipping in this region while encouraging speculation regarding the potential of the northwest passage (NWP) and the Canadian Arctic to become a major cruise maritime highway. Integrating research from both human and transport geography, this article presents an analysis of vessel movements. It also analyses perceptions of charters and cruise ship operators and of their interests in the cruise tourism market. Discussion is focused on issues associated with the lack of available vessels and maritime infrastructure, regulations in the Canadian arctic waters, security and search and rescue. This research could prove useful for communities, and policy makers, as well as the cruise sector itself, with regard to response to change in these remote locations.

The present study was conducted to measure the elemental concentration and bacterial deposition in the firn-cores at the Midre Lovénbreen glacier, Svalbard. Firn-cores up to 1m deep were collected and divided into three subsections. These were subjected to elemental analysis using inductively coupled plasma mass spectroscopy (ICPMS). In all 20 elements were analysed. The crustal enrichment factors calculated for these elements on the basis of Fe values, demonstrate that the elements have derived from both crustal and anthropogenic sources. For certain elements there also exists a possibility of input from sea salt spray. Total bacterial counts in these firn samples ranged from 1.03 × 105 to 3.67 × 105 per ml of meltwater. Culturability of these bacterial cells, in comparison to the total count was very low. At 4°C the maximum culturability was <1.4% of the total count while at 15°C it was still lower (~1%).

The bronze sculpture variously known as These had most to give, Aspiration and Youth, stands in the forecourt of the Scott Polar Research Institute (SPRI) in Cambridge, and functions as a memorial to the British Antarctic Expedition polar party of 1911–1912. It is one of the most important works by Kathleen Scott, wife of Robert Falcon Scott, and a prominent and prolific sculptor. Originally intended as a war memorial and dating from 1922–1923, it received critical acclaim and was exhibited widely. Ten years later Kathleen Scott offered the sculpture to the SPRI to accompany its new building. The institute's committee of management wished to reject the gift, however, as its members considered it too successful in conveying ‘death and martyrdom and in general the tragic side of Polar work’, as Frank Debenham stated, rather than scientific research and discovery. After prolonged discussions with the institute's architect, Herbert Baker, who admired Kathleen Scott and this work, it was finally accepted and installed as inconspicuously as possible. This article reconstructs the historical background to the sculpture and the controversy that surrounded it, using primary source material. The relevance of the objections to the sculpture, as well as its positive qualities, are also briefly examined from a modern perspective.

Distributions of gymnosomatous pteropods, Spongiobranchaea australis and Clione antarctica, were determined at six sites along a latitudinal gradient in western Antarctica Peninsula shelf waters using vertically stratified trawls. Hydrographic data were collected at the same sites with conductivity-temperature-depth casts, and correlations of explanatory variables to gymnosome distributions were determined using statistical analyses performed in Matlab, a high level programming software to conduct numerical computation and visualisation. Explanatory variables included sampling site, latitude, longitude and depth, seawater temperature, salinity and density, Southern Ocean Antarctic Surface Water, Winter Water, Upper Circumpolar Deep Water and warm transitional waters, as well as oceanographic remote sensing data for coloured dissolved organic matter, chlorophyll a concentration, normalised fluorescence line height, nighttime sea surface temperature, photosynthetically active radiation, particulate inorganic carbon, particulate organic carbon, daytime sea surface temperature and daily sea ice concentration. Hydrographic data revealed that warmer water masses were prevalent along the western Antarctic Peninsula, and the distributions of both gymnosome species were primarily influenced by water masses, temperature, sampling site and latitude. As a consequence, distributional shifts of gymnosomes are predicted in response to the current warming trends.

Sir John Franklin's widow, Jane Franklin, planned a biography of her husband in the years following the disappearance of his expedition. In this project she was directly assisted by her niece and amanuensis Sophia Cracroft. This biography never came to fruition, but it did result in an unpublished manuscript history of the Franklin family, dated 1853, which Cracroft shared with Franklin's early biographers. The manuscript provides an interesting account of the Franklin family, including the detailed circumstances of the failure of the Boston and Spilsby Bank in 1804, which caused great financial and emotional stress. The final section of the manuscript provides an account of John Franklin's early naval career and Arctic expeditions.

The aim of this study is to investigate how reduction in the sea ice cover may affect oil activity in the Arctic during the next 30 years. The Arctic is divided into 21 oil provinces. A multidisciplinary approach is applied drawing on both the comparative cost techniques as developed in location theory and sea ice cover projections. The comparative cost technique implies a systematic listing of cost differentials by oil provinces. The sea ice projections are based on the NCAR CCSM3 global climate model under the A1B and A2 emission scenarios. The article concludes that the north Norwegian Sea, and south and west Barents Sea will remain the most attractive areas for oil exploration in the coming 30 years. Furthermore, due to sea ice decline, the north and east Barents Sea and north and west Kara Sea will become more attractive. However, most Arctic provinces will remain high cost regions.

In the summer of 2014 a major search was mounted in the Canadian Arctic for H.M.S. Erebus and Terror, the ships of Sir John Franklin's expedition, the aim of which was to make a transit of the northwest passage. Beset in the ice to the northwest of King William Island in the summer of 1846, they were abandoned there by the 105 surviving members of their crews in the summer of 1848. The officers and men hoped to walk south to the mouth of the Back River, presumably to ascend that river in the hope of reaching the nearest Hudson's Bay Company's post at Fort Resolution on Great Slave Lake. None of them survived. The 2014 expedition, the Victoria Strait Expedition, mounted by a consortium which included Parks Canada, the Canadian Coast Guard, the Canadian Navy, the Royal Canadian Geographical Society, the Arctic Research Foundation, and One Ocean Adventure, had four ships at its disposal including the Canadian Coast Guard's icebreaker Sir Wilfrid Laurier (Captain Bill Noon) and the Navy's HMCS Kingston.

This note considers the latest iterations to the Arctic Council following the May 2013 ministerial meeting in Kiruna, Sweden. While new state observers including China and Japan were admitted, the European Union's application was deferred and the entire list of non-governmental and intergovernmental organisation applicants was rejected without consideration. Although time-based pressures may have been a factor, the failure to consider the non-state entities’ applications has the effect of reinforcing the impression that the Arctic Council is and will remain a state-centric body.

Each year Polar Record calls upon numerous scholars to assist in the demanding and intensive refereeing and peer-review procedures for manuscripts submitted for publication. These individuals give generously of their time and expertise to help ensure that a high academic quality is maintained in Polar Record. During the preparation of the four issues for 2014, the following individuals participated in the review and refereeing process. Our deep appreciation for their assistance is offered to all.