Commander John P. Cheyne, R.N. (1826–1902) is a forgotten figure in the history of nineteenth-century polar exploration. A veteran of three expeditions in search of the missing Franklin expedition, his retirement was atypical of the many naval officers who had served in the Arctic. Late in 1876, after the disappointing return of the British Arctic expedition under George Strong Nares, Cheyne first announced his grand plans to reach the North Pole by balloon. He embarked on a transatlantic lecture tour in an effort to raise funds. It was a novel proposal that captured public imagination, but also drew wide criticism, and sometimes ridicule. This paper draws upon a study of primary and secondary materials: original manuscripts and correspondence, British and American newspapers and the illustrated press, souvenirs, pamphlets, and periodical reviews. This is a neglected episode in the history of polar exploration and in the history of aeronautics more generally, and it is a story of naivety and optimism, bravado and speculation. This paper examines the prevailing currents of public opinion of the value of exploration in this period, the debates surrounding new techniques of polar travel, and the changing image of the explorer. Both aeronautical pioneer and itinerant showman, Cheyne was increasingly maligned as a charlatan and lunatic. He proved unable to realise his dream of polar flight.

In the century since Roald Amundsen and Robert F. Scott led the first and second expeditions to reach the South Pole, commentators have frequently passed judgement on the different means of transport that the two explorers employed. In hindsight, and since he ‘won,’ they have consistently praised Amundsen for using dogs exclusively and criticised Scott for not doing the same. Surprisingly, however, almost no attention has been given to the experience of Amundsen's dogs, whose extreme suffering seems to have vanished into a collective blind spot. Here, with the aim of restoring balance to one part of the vexed historiography of the two explorers, that record is set straight. Amundsen's troubled and contradictory attitude towards his animals is also explored and common misconceptions about Scott's views on the use of dogs for transport are confuted.

This paper lists accounts of whaling voyages to the Arctic from British ports, dating from the early 17th to early 20th centuries, that are available as logbooks, journals or publications for study in British, Canadian or United States public institutions. Included are all original whaling logbooks and journals located by the authors, mainly but not exclusively from previous listings, plus early publications by whaling masters, mates, surgeons and others in the trade containing details of particular voyages, and later accounts based on edited versions of holograph manuscripts. Records of whaling voyages are of intrinsic historical and sociological value, and many include data on weather and sea ice conditions that are of particular relevance to current studies of climatic variation.

As the fourth International Polar Year (IPY) 2007–2008, gets into full swing it is timely to reflect on the history of development of international scientific collaboration in the IPYs since the first one in 1882–1883, including the third, which evolved into the International Geophysical Year (IGY) of 1957–1958. The success of international scientific collaboration in the IGY led the International Council for Science (ICSU), the body that managed the IGY, to create the Scientific Committee on Antarctic Research (SCAR) to carry forward the collaboration in Antarctic science that had begun during the IGY. This year, 2008, seems an appropriate time to undertake such an historical review, given that we are not only midway through the fourth IPY, but also that it is SCAR's 50th anniversary; the first SCAR meeting having been held in The Hague on 3–5 February 1958. Since SCAR's membership began with 12 member countries and 4 ICSU unions, membership has grown to 34 countries and 8 ICSU unions, with more expected to join at the 30th meeting of SCAR in Moscow in July 2008. Both SCAR's activities and those of the fourth IPY benefit from international collaboration not only between scientists, but also between the national Antarctic operations managers, working together through the Council of Managers of National Antarctic Programmes (COMNAP), and national policy makers working together through the Antarctic Treaty mechanisms. Thanks to all their efforts, the IPY of 2007–2009 will leave behind a legacy of enhanced observing systems for documenting the status and change of all aspects of the Antarctic environment as the basis for improved forecasting of its future condition. SCAR expects to play a major role in the design of those systems and their use to improve scientific understanding of the place of the Antarctic in the global environmental system, and the pace and direction of change within that system.

Sea ice has been, and continues to be, an integral component of life in the Inuit community of Pangnirtung, Nunavut. Located in a fiord of the same name off the northeastern end of Cumberland Sound, extensive ice formation occurs within the fiord and the sound. This creates an important travel and hunting platform, and enables access to the coastlines of Cumberland Sound, hunting and fishing grounds, and nearby communities. With the combined importance, dynamism, and continuous use of this frozen ocean environment, local Inuit elders and hunters have developed a detailed and nuanced understanding of sea ice conditions, freeze/thaw processes, and the influences of winds and currents on ice conditions. Working collaboratively with the community of Pangnirtung since September 2003, we present the results of 30 semi-directed interviews, 5 sea ice trips, and 2 focus groups to provide a baseline understanding of local freezing processes (near-shore, open water, sea ice thickening, landfast ice, tidal cracks, and the floe edge), melting processes (snow melt, water accumulation and drainage, and break-up), wind influences on sea ice (wind direction and strength affecting sea ice formation and movement), and, current influences on sea ice (tidal variations and current strength affecting sea ice formation, movement, and polynya size/location). Strong emphasis is placed on Inuktitut terminology and spatial delineations of localised ice conditions and features. Therefore, this paper provides insights into local scale ice conditions and dynamics around Pangnirtung that are not captured in regional scale studies of Cumberland Sound and/or Davis Strait. As the third in a series of three papers on the same subject, but from different communities in the Qikiqtaaluk (Baffin) Region of Nunavut, this paper also provides a comparative summary of Inuktitut and scientific sea ice terminology along with an overview of the broader implications of results for collaborative science, education, and heritage initiatives.

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.

A newly discovered Antarctic poem, probably by Raymond Priestley, is presented.