Aurora and the Otago Museum: the boundary between Antarctic science and seamanship

Polar Record ◽  
2017 ◽  
Vol 53 (2) ◽  
pp. 192-198 ◽  
Author(s):  
Moira White
Keyword(s):  
World War I ◽  
British Empire ◽  
Ross Sea ◽  
Weddell Sea ◽  
World War ◽  
Pack Ice ◽  
Antarctic Expedition ◽  
Antarctic Continent ◽  
Museum Staff ◽  
The Antarctic

ABSTRACTSir Ernest Shackleton's Imperial Trans-Antarctic Expedition famously did not succeed in traversing the Antarctic continent from the Weddell Sea to the Ross Sea. It was, nevertheless, an enterprise that engaged the interest of New Zealanders and the rest of the British Empire even as World War I was being fought. When one of the expedition ships, Aurora, broke from her moorings soon after arrival in McMurdo Sound and drifted trapped in pack ice for months, the construction of a temporary jury rudder while still at sea enabled her crew to make their way to Port Chalmers, Dunedin for more extensive repairs in 1916. This paper discusses interactions between the Otago Museum staff and the crew of Aurora while she was in port, the offer of the replaced jury rudder to the museum, and reflects on the concerns and interests that might have contributed to the offer and its rejection.

Bird and mammal life recorded during the Antarctic drift of SY Aurora, 1915–16

Polar Record ◽  
1990 ◽  
Vol 26 (159) ◽  
pp. 277-288 ◽  
Author(s):  
P. D. Shaughnessy
Keyword(s):  
Southern Ocean ◽  
Ross Sea ◽  
Killer Whales ◽  
Food Items ◽  
Emperor Penguins ◽  
Sea Birds ◽  
Pack Ice ◽  
Antarctic Expedition ◽  
The Antarctic ◽  
Blue Whales

AbstractAfter landing the Ross Sea shore party of Shackleton's Imperial Trans-Antarctic Expedition at Cape Evans, McMurdo Sound, SY Aurora drifted for 313 days between May 1915 and March 1916 in the pack iceof the Ross Sea and Southern Ocean. During the drift A. H. Ninnis maintained observations of the fauna. He was out hunting on the pack ice on at least 86 days to augment the ship's slender provisions, taking 289 penguins, 10 other sea birds and 20 seals. He sighted whales on at least 15 days, including killer whales in July and August and four large whales, possibly blue whales, in November. He also noted birds returning south for the breeding season in spring, progress of moult in emperor penguins, pupping of crabeater and leopard seals, and food items of several seals and seabirds. Most of his report is presented here, edited to improve its readability and remove abbreviations; the text is preceded by a brief summary of the fauna seen and followed by footnotes on some of his observations.

Against all odds: the birth of the Commonwealth Trans-Antarctic Expedition, 1955–1958

Polar Record ◽  
2011 ◽  
Vol 49 (1) ◽  
pp. 50-61
Author(s):  
Stephen Hicks ◽  
Bryan Storey ◽  
Philippa Mein Smith
Keyword(s):  
New Zealand ◽  
The United States ◽  
Weddell Sea ◽  
Antarctic Expedition ◽  
Foreign Office ◽  
Polar Research Institute ◽  
Antarctic Continent ◽  
British Foreign Office ◽  
The Many ◽  
The Antarctic

ABSTRACTWhen the Commonwealth Trans-Antarctic Expedition 1955–1958 advance party sailed from the Millwall Docks in November 1955, bound for the Weddell Sea, their departure was the product of five years of intensive effort on the part of Vivian Fuchs to achieve the first overland crossing of the Antarctic continent. This paper investigates the many obstacles that had to be overcome leading up to Theron sailing and explains the manner in which they were overcome by the Fuchs-Wordie-Clifford triumvirate. The British Foreign Office was particularly opposed to the expedition with the office's focus on sovereignty rather than science while an alternative proposal from Duncan Carse raised a unique set of difficulties. The withdrawal from involvement by the Scott Polar Research Institute Director, Colin Bertram, indicated further disaffection. Most important, if political and financial goals were to be met, was the need for participation by several Commonwealth countries of which New Zealand was the essential partner. Fortunately, the vigorous efforts of a few Antarctic enthusiasts in New Zealand were successful in moving their government to assert its long dormant position in the Ross Dependency. New Zealand's commitment turned the tide of commonwealth apathy towards the TAE. Although the TAE preceded the IGY, events, including the dominating IGY presence of the United States, caused the two projects to become tightly interwoven. For these reasons the years leading up to the departure of Theron were as intriguing as the crossing journey itself.

Henrik Bull, the Antarctic Exploration Committee and the first confirmed landing on the Antarctic continent

Polar Record ◽  
2007 ◽  
Vol 43 (2) ◽  
pp. 143-153 ◽  
Author(s):  
Andrew McConville
Keyword(s):  
Ross Sea ◽  
Learned Societies ◽  
Antarctic Expedition ◽  
Antarctic Continent ◽  
The Antarctic

The Norwegian Henrik Johan Bull managed the Antarctic expedition that penetrated the Ross Sea in 1895 and made a landing at Cape Adare, the first confirmed landing on the Antarctic mainland. Bull had attempted to fund the voyage in Melbourne where he had lived since the late 1880s. At that time, Melbourne's learned societies, through their Antarctic Exploration Committee (AEC), were also making strenuous attempts to launch an expedition. The two parties had contact but the differences in their aims resulted in little cooperation. The AEC plans of a joint commercial/scientific expedition with Dundee or Norwegian whalers, and then a joint scientific expedition under Adolf Erik Nordenskiöld, foundered due to lack of funds. The plans to include a scientist, nominated by the learned societies, in Bull's expedition also failed. Instead, Carsten Egeberg Borchgrevink joined Bull's expedition as an ordinary seaman and an occasional scientist. He used this experience to realise his plans to winter on Antarctica. Both Bull and the AEC were important in developing interest in Antarctic exploration and commerce.

British Antarctic Policy in the Early 20th Century

Polar Record ◽  
1983 ◽  
Vol 21 (134) ◽  
pp. 475-483 ◽  
Author(s):  
Peter J. Beck
Keyword(s):  
World War I ◽  
British Empire ◽  
Land Surface ◽  
World War ◽  
Major Powers ◽  
The Pacific ◽  
Mother Country ◽  
Post War ◽  
The Antarctic ◽  
Colonial Office

World War I has often been said to mark the end of the ‘Age of Imperialism’—the close of ‘that final surge of land hunger’ (Landes 1969) from 1880 to 1914 when much of the world's land surface, especially in Africa and the Pacific, was acquired by the major powers. Britain's large share was demonstrated by the predominance of red on pre-1914 maps, though in fact the British Empire achieved its greatest area after 1918; ‘… including India’, reported the 1920 Colonial Office List, ‘the Empire now extends over 11 million of square miles, or 91 times the area of the Mother Country’ (Mercer 1920). This study examines one specific part of British imperial policy in the immediate post-war years—one which, had it been fully implemented, would have increased the area by a further 40 per cent. In the view of L. S. Amery, Under-Secretary of State at the Colonial Office and one of Britain's leading politicians of the time, it was desirable that:… the whole of the Antarctic should ultimately be included within the British Empire, and that, while the time has not yet arrived that a claim to all the continental territories should be put forward publicly, a definite and consistent policy should be followed of extending and asserting British control with the object of ultimately making it complete.

scholarly journals XXXI.—Shackleton Antarctic Expedition, 1914–1917: The Natural History of Pack-Ice as observed in the Weddell Sea

1921 ◽  
Vol 52 (4) ◽  
pp. 795-829 ◽  
Author(s):  
J. M. Wordie
Keyword(s):  
Natural History ◽  
Weddell Sea ◽  
The West ◽  
Pack Ice ◽  
Antarctic Expedition ◽  
History Of ◽  
The Antarctic ◽  
Land Water

The opportunities for observation were afforded by the voyage and subsequent drift of the S.Y. Endurance. During December 1914 and January 1915 for a period of six weeks she successfully bored her way through pack-ice of every description—drift-ice, open-pack, and very frequently even close-pack. Continually fighting, she penetrated from 59° to 72° S. lat., and finally reached the land water off Coats Land on the latter parallel. As the crow flies, therefore, she was navigated through ice for nearly 800 geographical miles on this voyage; her actual course among the ice-fields and floes was computed to exceed 2000 miles, an achievement without parallel in the Antarctic. The principle adopted was to keep to the east, where presumably there is less pack than in the west; if the Endurance experience is a normal one, however, the meridian of 20° W. long., which was followed, is certainly not far enough east.

The polar ship Scotia

Polar Record ◽  
2005 ◽  
Vol 41 (2) ◽  
pp. 131-140 ◽  
Author(s):  
Angus B. Erskine ◽  
Kjell-G. Kjær
Keyword(s):  
North Atlantic ◽  
Weddell Sea ◽  
Biological Research ◽  
Orkney Islands ◽  
Antarctic Expedition ◽  
South Orkney Islands ◽  
Antarctic Continent ◽  
The Uk ◽  
The Antarctic ◽  
The Great War

The ship that the oceanographer Dr William Speirs Bruce used on the Scottish National Antarctic Expedition, 1902–04, was originally a sealer named Hekla, built in Norway in 1872. In 1889 the Norwegian skipper Ragnvald Knudsen explored the northeast coast of Greenland between latitudes 74° and 75°, and in 1891–92 the ship was used by the Danish naval officer, Lieutenant C. Ryder, to explore the inner recesses of Scoresby Sund, finally visiting Angmagssalik. In 1902, re-named Scotia and captained by Tam Robertson from Peterhead, she sailed to the Weddell Sea under the leadership of Bruce. The southern winter of 1903 was spent at Laurie Island in the South Orkney Islands, and in March–April 1904 the party discovered 150 miles of previously unknown coastline of the Antarctic continent, reaching a farthest south of 74°01′S, 22°00′W. An extensive programme of marine survey and biological research was carried out. Back in the UK, Bruce sold the ship, and she returned to sealing, based in Dundee until appointed to be the first international North Atlantic Ice Patrol ship after the tragedy of Titanic. The Great War caused her to become a freighter in the English Channel area until she caught fire and was burnt out on a sandbank in the Bristol Channel on 18 January 1916.

scholarly journals II.—Shackleton Antarctic Expedition, 1914–1917 : Geological Observations in the Weddell Sea Area

1922 ◽  
Vol 53 (1) ◽  
pp. 17-27 ◽  
Author(s):  
J. M. Wordie
Keyword(s):  
Weddell Sea ◽  
Original Plan ◽  
Antarctic Expedition ◽  
Southern Side ◽  
Antarctic Continent ◽  
Sea Area ◽  
Relationship Of ◽  
The Antarctic ◽  
The Relationship

The original, plan of the Shackleton Expedition, had it been realised, would have yielded geological results of no little value. The base would have been on Coats Land, and next in importance to crossing the Antarctic continent was the projected geological sledging trip across the Wilhelm Barrier, westwards from the head of the Weddell Sea to the southern. continuation of Graham Land. Had it been carried out, it would of course have settled finally the relationship of Graham Land to the rest of Antarctica. The besetment and destruction of the Endurance, however, put an end to the original plan, and no landing was ever made either on the eastern or on the southern side of the Weddell Sea.

Pathways and timescales of connectivity around the Antarctic continental shelf 

2021 ◽  
Author(s):  
Hannah Dawson ◽  
Adele Morrison ◽  
Veronica Tamsitt ◽  
Matthew England
Keyword(s):  
Continental Shelf ◽  
Ross Sea ◽  
Coastal Current ◽  
West Antarctica ◽  
Source Regions ◽  
Freshwater Forcing ◽  
Antarctic Continental Shelf ◽  
Antarctic Continent ◽  
Antarctic Slope Current ◽  
The Antarctic

<p><span xml:lang="EN-US" data-contrast="auto"><span>The Antarctic margin is surrounded by two westward flowing currents: the Antarctic Slope Current and the Antarctic Coastal Current. The former influences key processes near the Antarctic margin by regulating the flow of heat and nutrients onto and off the continental shelf, while together they </span></span><span xml:lang="EN-US" data-contrast="auto"><span>advect</span></span><span xml:lang="EN-US" data-contrast="auto"><span> nutrients, biological organisms, and temperature and salinity anomalies around the coastline, providing a connective link between different shelf regions. However, the extent to which these currents transport water from one sector of the continental shelf to another, and the timescales over which this occurs, remain poorly understood. Concern that crucial water formation sites around the Antarctic coastline could respond to non-local freshwater forcing </span></span><span><span xml:lang="EN-US" data-contrast="auto"><span>from ice shel</span></span></span><span><span xml:lang="EN-US" data-contrast="auto"><span>f meltwater</span></span></span> <span xml:lang="EN-US" data-contrast="auto"><span>motivates a more thorough understanding of zonal connectivity around Antarctica. In this study, we use daily velocity fields from a global high-resolution ocean-sea ice model, combined with the <span>Lagrangian</span> tracking software Parcels, to investigate the pathways and timescales connecting different regions of the Antarctic continental shelf<span> with a view to understanding</span><span> the timescales of meltwater transport around the continent</span>. Virtual particles are released over the continental shelf, poleward of the 1000 <span>metre</span> isobath, and are tracked for 20 years. Our results show a strong seasonal cycle connecting different sectors of the Antarctic continent, with more particles arriving further downstream during winter than during summer months. Strong advective links exist between West Antarctica and the Ross Sea while shelf geometry in some other regions acts as barriers to transport. We also highlight the varying importance of the Antarctic Slope Current and Antarctic Coastal Current in connecting different sectors of the coastline. Our results help to improve our understanding of circum-Antarctic connectivity <span>and the timescales </span><span>of meltwater transport from source regions to downstream </span><span>shelf locations. </span><span>Further</span><span>more, t</span><span>he timescales and pathways we </span><span>present </span><span>p</span>rovide a baseline from which to assess long-term changes in Antarctic coastal circulation due to local and remote forcing.<br></span></span></p>

Englishness, Empire and Nostalgia: A Heterodox Religious Community's Appeal in the Inter-War Years

2018 ◽  
Vol 54 ◽  
pp. 374-392
Author(s):  
Jane Shaw
Keyword(s):  
Twentieth Century ◽  
World War I ◽  
British Empire ◽  
Belief Networks ◽  
Healing Ministry ◽  
World War ◽  
Early Twentieth Century ◽  
The World ◽  
Sense Of Identity ◽  
The Rich

This article looks at the ways in which the Panacea Society – a heterodox, millenarian group based in Bedford during the inter-war years – spread its ideas: through personal, familial and shared belief networks across the British empire; by building new modes of attracting adherents, in particular a global healing ministry; and by shipping its publications widely. It then examines how the society appealed to its (white) members in the empire in three ways: through its theology, which put Britain at the centre of the world; by presuming the necessity and existence of a ‘Greater Britain’ and the British empire, while in so many other quarters these entities were being questioned in the wake of World War I; and by a deliberately cultivated and nostalgic notion of ‘Englishness’. The Panacea Society continued and developed the idea of the British empire as providential at a time when the idea no longer held currency in most circles. The article draws on the rich resource of letters in the Panacea Society archive to contribute to an emerging area of scholarship on migrants’ experience in the early twentieth-century British empire (especially the dominions) and their sense of identity, in this case both religious and British.

scholarly journals Albedo of the ice covered Weddell and Bellingshausen Seas

2012 ◽  
Vol 6 (2) ◽  
pp. 479-491 ◽  
Author(s):  
A. I. Weiss ◽  
J. C. King ◽  
T. A. Lachlan-Cope ◽  
R. S. Ladkin
Keyword(s):  
Sea Ice ◽  
Surface Albedo ◽  
Austral Summer ◽  
Open Water ◽  
Weddell Sea ◽  
First Year ◽  
Pack Ice ◽  
Bellingshausen Sea ◽  
The Mean ◽  
The Antarctic

Abstract. This study investigates the surface albedo of the sea ice areas adjacent to the Antarctic Peninsula during the austral summer. Aircraft measurements of the surface albedo, which were conducted in the sea ice areas of the Weddell and Bellingshausen Seas show significant differences between these two regions. The averaged surface albedo varied between 0.13 and 0.81. The ice cover of the Bellingshausen Sea consisted mainly of first year ice and the sea surface showed an averaged sea ice albedo of αi = 0.64 ± 0.2 (± standard deviation). The mean sea ice albedo of the pack ice area in the western Weddell Sea was αi = 0.75 ± 0.05. In the southern Weddell Sea, where new, young sea ice prevailed, a mean albedo value of αi = 0.38 ± 0.08 was observed. Relatively warm open water and thin, newly formed ice had the lowest albedo values, whereas relatively cold and snow covered pack ice had the highest albedo values. All sea ice areas consisted of a mixture of a large range of different sea ice types. An investigation of commonly used parameterizations of albedo as a function of surface temperature in the Weddell and Bellingshausen Sea ice areas showed that the albedo parameterizations do not work well for areas with new, young ice.

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