Benjamin Leigh Smith's second Arctic expedition: Svalbard and Jan Mayen, 1872

Polar Record ◽  
2008 ◽  
Vol 44 (3) ◽  
pp. 255-264 ◽  
Author(s):  
P.J. Capelotti
Keyword(s):  
The Arctic ◽  
Research Vessel ◽  
North Coast ◽  
Primary Research ◽  
The North ◽  
Arctic Exploration ◽  
Ice Conditions

ABSTRACTIn 1872, the British yachtsman and explorer Benjamin Leigh Smith led his second expedition to the Arctic. Seeking to further the impressive oceanographic and geographic research of his first expedition in the summer of the previous year, Leigh Smith first explored Jan Mayen and then sailed to Svalbard. There, after investigating Moffen, adverse ice conditions precluded effective continuation of the voyage and almost wrecked his research vessel,Sampson. During a brief meeting with Adolf Erik Nordenskiöld's Swedish polar expedition, a bond was formed between the two explorers with fortuitous benefits for the Swedish expedition the following year as it struggled to escape from the north coast of Svalbard. Leigh Smith was forced to make for England in September 1872, without sailing nearly as far to the north or east as during his first expedition. His 1872 experiences led him to reconsider his method for Arctic exploration, and consequently, for his third expedition in 1873, he decided to include a chartered steamer as his primary research vessel withSampsonrelegated to the role of support vessel.

scholarly journals The role of tropopause polar vortices in the intensification of summer Arctic cyclones

2021 ◽  
Author(s):  
Suzanne Louise Gray ◽  
Kevin Ivan Hodges ◽  
Jonathan Luke Vautrey ◽  
John Methven
Keyword(s):  
Three Dimensional ◽  
Relative Vorticity ◽  
The Arctic ◽  
North Coast ◽  
Polar Regions ◽  
The North ◽  
Observation Network ◽  
Long Lifetime ◽  
Cyclone Genesis

Abstract. Human activity in the Arctic is increasing as new regions become accessible, with a consequent need for improved understanding of hazardous weather there. Arctic cyclones are the major weather systems affecting the Arctic environment during summer, including the sea ice distribution. Meso- to synoptic-scale tropopause polar vortices (TPVs) frequently occur in polar regions and are a proposed mechanism for Arctic cyclone genesis and intensification. However, while the importance of pre-existing tropopause-level features for cyclone development, and their existence as part of the three-dimensional mature cyclone structure, is well established in the mid-latitudes, evidence of the importance of pre-existing TPVs for Arctic cyclone development is mainly limited to a few case studies. Here we examine the extent to which Arctic cyclone growth is coupled to TPVs by analysing a climatology of summer Arctic cyclones and TPV characteristics produced by tracking both features in the latest ECMWF reanalysis (ERA5). The annual counts of Arctic cyclones and TPVs are significantly correlated for features with genesis either within or outside the Arctic, implying that TPVs have a role in the development of Arctic cyclones. However, from their proximity, only about one third of Arctic cyclones intensify while influenced by a TPV and a maximum of 10 % have a nearby TPV at their genesis time. Consistent with the track densities of the full sets of Arctic cyclones and TPVs, cyclones associated with TPVs during their intensification phase (matched cyclones) track preferentially over the Arctic Ocean along the North American coastline and Canadian Archipelago. In contrast, cyclones intensifying distant from any TPV (unmatched cyclones) track preferentially along the north coast of Eurasia. Composite analysis reveals the presence of a distinct relative vorticity maximum at and above the tropopause level associated with the TPV throughout the intensification period for matched cyclones and that these cyclones have a reduced upstream tilt compared to unmatched cyclones. Interaction of cyclones with TPVs has implications for the predictability of Arctic weather, given the long lifetime, but relatively small spatial scale of TPVs compared with the density of the polar observation network.

The system-forming role of the Arctic cluster in the development of the economy of the North of Russia (on the example of the Murmansk region)

2020 ◽  
pp. 96-104
Author(s):  
Е.С. Хаценко ◽  
Л.С. Лычкина
Keyword(s):  
Economic Policy ◽  
Legal Aspects ◽  
The Arctic ◽  
Russian Arctic ◽  
The North ◽  
Murmansk Region ◽  
The Creation

Представленная статья посвящена теоретико-правовым аспектам формирования экономической политики Российской Арктики, создание и регулирование Арктического экономического кластера. The presented article is devoted to the theoretical and legal aspects of the formation of the economic policy of the Russian Arctic, the creation and regulation of the Arctic economic cluster.

scholarly journals The Role of the Disaster Preparedness Group in Adapting Abrasion to Communities Affected by Abrasion on the North Coast of Rembang, Central Java

2021 ◽  
Author(s):  
Dewi Liesnoor Setyowati ◽  
Puji Hardati ◽  
Andi Irwan Benardi ◽  
Nur Hamid ◽  
Yohanes Dwi Anugrahanto
Keyword(s):  
Disaster Preparedness ◽  
North Coast ◽  
The North ◽  
Central Java

Chapter 20 Paleogene history

1997 ◽  
Vol 17 (1) ◽  
pp. 388-417
Keyword(s):  
Early Cretaceous ◽  
The Arctic ◽  
North Coast ◽  
Western Coast ◽  
Central Basin ◽  
Oblique Collision ◽  
The North ◽  
Western Border ◽  
Paleozoic Rocks ◽  
West Spitsbergen

The Paleogene chapter of Svalbard history is a quite distinct one. It begins with an unconformity, albeit a sub-parallel one representing a late Cretaceous hiatus. Resting on Albian and older strata, the Van Mijenfjorden Group of six formations totals a thickness of about 2500 m in the Central Basin of Spitsbergen. The outcrop is ringed by Early Cretaceous strata in a broad syncline (Fig. 20.1). The strata are largely non-marine, coal-bearing sandstones, with interbedded marine shales and they range in age through Paleocene and Eocene.From latest Paleocene through Eocene time the West Spitsbergen Orogeny caused (Spitsbergian) deformation along the western border of the Central Basin, but it is most conspicuous in the folding and thrusting of Carboniferous through Early Cretaceous rocks. The orogen extended westwards to and beyond the western coast of central and southern Spitsbergen including Precambrian and Early Paleozoic rocks, which had already been involved in earlier tectogenesis. The eastward-verging thrusting extended beneath the Tertiary basin and reactivated older faults to the east.In the wider context Svalbard, adjacent to the north coast of Greenland, had been an integral part of Pangea from Carboniferous through Cretaceous time. The northward extension of the Atlantic opening reached and initiated the spreading of the Arctic Eurasia Basin at the beginning of the Paleogene Period. This led to the separation of Svalbard together with the Barents Shelf and northern Europe from Greenland by dextral strike-slip transform faulting. In the course of this progression, oblique collision between northeast Greenland and Svalbard caused

A levee breach induced by internal erosion in Western Australia.

2021 ◽  
pp. qjegh2021-037
Author(s):  
Scott Davidson ◽  
Paul Baker
Keyword(s):  
Western Australia ◽  
Internal Erosion ◽  
North Coast ◽  
Sandy Gravel ◽  
Content Type ◽  
The North ◽  
Levee Breach ◽  
Piping Erosion ◽  
A Site

This case study presents a levee breach induced by piping erosion under cyclonic conditions in 2019. The levee is a 2.5 m high, 500 m long, mass earth fill embankment; with no cut-off trench, core, or ancillary structures. Located near Port Hedland on the north coast of Western Australia; its purpose is diversionary, to redirect cyclonic surface water away from the nearby Great Northern Highway. The levee was founded directly on Alluvium in 1987; and formed of locally sourced clayey sandy gravel. In 2003, the levee was partially excavated to enable the placement of a buried pipeline through the levee.Following a cyclonic event in 2019, a 27 m length of the levee breached, resulting in significant scour of the foundation and downstream soil. A site visit and investigation were conducted shortly thereafter, where in situ testing and laboratory soil tests on the levee and foundation materials were conducted.Analysis of the site observations and laboratory testing data led to the probable failure mechanism being theorised as having been initiated within the foundation by piping erosion within sand-rich beds of Alluvium. The large quantity of water ponding upstream of the levee then caused a progressive washout and breach of the levee.Thematic collection: This article is part of the Role of water in destabilizing slopes collection available at: https://www.lyellcollection.org/cc/Role-of-water-in-destabilizing-slopes

scholarly journals Aspects of the Glaciology of Meighen Island, Northwest Territories, Canada

1965 ◽  
Vol 5 (40) ◽  
pp. 399-410 ◽  
Author(s):  
K. C. Arnold
Keyword(s):  
Snow Accumulation ◽  
The Arctic ◽  
North Coast ◽  
Ice Cap ◽  
The North ◽  
Four Seasons ◽  
Northern Half ◽  
Northern Edge ◽  
Summer Temperatures ◽  
Made In

Abstract Meighen Island lies in the centre of the north coast of the Queen Elizabeth Islands and fronts on the Arctic Ocean. An ice cap of about 76 km.2 covers about one-tenth of the island. Its greatest thickness of 150 m. occurs under the summit, near the south end, which was 268 m. above sea-level in 1960. The northern half of the ice cap is less than 30 m. thick; and the total volume is of the order of 2,000 × 106 m.3. Precipitation is low in the northern Queen Elizabeth Islands, and Meighen Island lies in an area where summer temperatures are lowest. In the winters of 1959–60, 1960–61 and 1961–62, the snow accumulation was 12.6, 18.2 and 14.1 cm. of water equivalent. Some snowfall remained on the higher part of the ice cap in the cold summer of 1961; but the ice cap diminished in volume in each year; by 36 × 106, 72 × 106, 22 × 106 and 91 × 106 m.3 in the 1959, 1960, 1961 and 1962 ablation seasons. If the conditions of these four seasons were maintained the ice cap would disappear in about 100 yr. However, a radio-carbon dating of a saxifrage exposed by the retreat of the ice from a small nunatak near the northern edge gave a date of less than 100 yr., and it appears that the existence of the ice cap might be sensitively related to recent climatic change. Careful surveys were made in 1959, 1960 and 1961 in an attempt to detect movement in the ice cap. Unequivocal evidence is not available from these surveys; but the stake network has been maintained and another survey has recently been completed.

scholarly journals Ice Conditions of an Arctic Polynya: North Water in Winter

1986 ◽  
Vol 32 (112) ◽  
pp. 383-390 ◽  
Author(s):  
Konrad Steffen
Keyword(s):  
Sea Water ◽  
Surface Condition ◽  
Open Water ◽  
Sea Surface ◽  
Aerial Images ◽  
The Arctic ◽  
The North ◽  
North Water ◽  
Ice Conditions ◽  
Fast Ice

AbstractThe surface condition of the North Water was investigated during two winters (i.e. the three polynyas: Smith Sound polynya, Lady Ann Strait polynya, and Barrow Strait polynya). Since no detailed information was available on ice conditions and the extent of open water during winter, radiometric temperature measurements of the sea surface had to be taken along a flight line of 2650 km from an altitude of 300 m. From November to March 1978-79 and 1980-81, 14 remote-sensing flights were carried out. On the basis of the radiometric measurements, the following ice types were identified: ice-free, dark nilas, light nilas, grey ice, grey-white ice, and white ice. A comparison between the thermal and the visual ice classification (the latter being based on grey tones of the aerial images) showed a deviation of 3%. The analysis showed that in November, December, and January more than 50% of the Smith Sound polynya was covered by young ice, nilas, and ice-free, whereas in February and March white ice was dominant. Moreover, it was found that the two polynyas in Smith Sound and Lady Ann Strait were much smaller than previously believed. In Barrow Strait, a semi-permanent polynya was observed in the winter of 1980-81. The occurrence of polynyas in Barrow Strait seems to be connected with the location of the fast-ice edge. On the basis of the calculated ice-type distribution and heat-flux rates for different ice types, an energy loss of 178 W m-2was found on the surface of the Smith Sound polynya due to open water and thin ice for the winter months November to March. Compared with other ice-covered sea surfaces in the Arctic, the heat release by the sea-water in the Smith Sound polynya is about 100 W m-2larger.

scholarly journals Irrigation and the Origins of the Southern Moche State on the North Coast of Peru

2002 ◽  
Vol 13 (4) ◽  
pp. 371-400 ◽  
Author(s):  
Brian R. Billman
Keyword(s):  
Political Development ◽  
Archaeological Sites ◽  
North Coast ◽  
Arid Environments ◽  
Irrigation Systems ◽  
Moche Valley ◽  
The North ◽  
State Evaluation ◽  
North Coast Of Peru

In this paper, I examine the role that irrigation played in the formation of the Southern Moche state in the Moche Valley, Peru. Specifically, I attempt to test Wittfogel and Steward's hydraulic model, which postulates that in certain arid environments, the managerial requirements of construction and maintenance of irrigation systems played a crucial role in the formation of centralized polities. I formulate and evaluate four hypotheses concerning the role of irrigation systems in the Moche Valley. Those hypotheses are then evaluated using settlement pattern data drawn from two surveys that cover the entire coastal section of the valley and provide information on 910 archaeological sites. Based on those data, I present a sequence of political development for the valley from the formation of the first autonomous village in the Late Preceramic period (2500–1800 B. C.) to the zenith of the Southern Moche state. Evaluation of the four hypotheses indicates that the managerial requirements of irrigation were relatively unimportant; rather, warfare, highland-coastal interaction, and political control of irrigation systems created opportunities for leaders to form a highly centralized, territorially expansive state sometime between A. D. 200 and 700.

scholarly journals Environmental Policy of Mangroves Management in Rembang Regency

2018 ◽  
Vol 31 ◽  
pp. 09002 ◽  
Author(s):  
Ali Roziqin
Keyword(s):  
Environmental Policy ◽  
Environmental Sustainability ◽  
Positive Impact ◽  
Mangrove Ecosystem ◽  
North Coast ◽  
Role Of Government ◽  
Mangrove Area ◽  
The North ◽  
Qualitative Descriptive

Mangrove area is an area overgrown mangrove in a natural or artificial, to maintain the environmental sustainability of coastal areas. In addition to maintaining the ecosystem of biodiversity, the mangrove area also has a role to social-economic, and socio-cultural. Rembang regency is one of the districts on the north coast of Java which has a large mangrove area. However, due to the high economic activity in the region of Rembang Regency, the mangrove area becomes less and damaged. This research to describe how environmental policy to manage mangrove area in Rembang regency with qualitative descriptive approach. The result is the role of government and society gradually able to restore mangrove ecosystem. Moreover the district government through Environmental Agency has made a masterplan for the development of mangrove ecotourism in Pasarbanggi Village. The existence of sustainable mangrove conservation has a positive impact on the environment and society.

The Canadian Sledge Dogs of the Eastern and Western Arctic

Polar Record ◽  
1937 ◽  
Vol 2 (13) ◽  
pp. 59-68 ◽  
Author(s):  
S. Hadwen
Keyword(s):  
Preventive Measures ◽  
Good Condition ◽  
The Arctic ◽  
The North ◽  
Arctic Regions ◽  
Arctic Exploration ◽  
Western Arctic ◽  
Time Of Year ◽  
Working Out ◽  
Better Than

In reading of Arctic exploration one is struck with the ill-fate which has often beset the dogs accompanying the explorers. Recently Baashuus-Jessen (1935) has carefully studied the accounts of many of these important expeditions and, according to this author, the lack of proper food containing right amounts of fat, minerals and vitamins was the principal cause of nervous diseases and malnutrition in the animals. In the Arctic and Antarctic regions, nevertheless, some most successful journeys have been accomplished with the aid of dogs. Unfortunately, it should be added that though the explorers reached their goals, it was often at the expense of their animals. Without doubt, also, when a stage is reached where dogs have to be sacrificed to feed the living, the latter are not in much better condition than those which were killed. Personally I should like to see or hear of an expedition, to one of the Poles or to some other place difficult of access, where all the dogs would return in good condition, to show the world what could be done with proper food and management. This article has been written for the Institute in the hope that the information about sledge-dogs may be of some assistance to those about to undertake expeditions in the Arctic regions. In this connection I should like to say that no other domesticated animal can withstand the hardships of the north better than the dog. He can follow man wherever he goes, and I have wondered why he is not more used, for instance, in mountaineering at the lower levels. The dog, being a native animal, winters well if he is properly fed, and should be at his best when the days begin to lengthen, which is just the time of year long journeys are undertaken. I will conclude by hoping that some of our young men will make a study of this matter: first of all by getting a thorough understanding of the mechanical laws involved in traction and harnessing; secondly, in working out balanced rations with the food available in the different countries where the dogs are to be driven, and also by making a study of hygiene and of preventive measures against disease and parasites; and lastly, by getting some actual practice in dog driving.

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