scholarly journals Voyages of discovery and research within the Arctic regions, from the year l8l8 to the present time: under the command of the several naval officers employed by sea and land in search of a North-west passage from the Atlantic to the Pacific; with two attempts to reach the North pole. Abridged and ar By Sir John Barrow.

1846 ◽  
Author(s):  
John Barrow
Keyword(s):  
North Pole ◽  
The Arctic ◽  
North West ◽  
The North ◽  
Arctic Regions ◽  
The Pacific ◽  
Naval Officers

Chronological list of expeditions and historical events in northern Canada. IV. 1763–89

Polar Record ◽  
1971 ◽  
Vol 15 (98) ◽  
pp. 699-721
Author(s):  
Alan Cooke ◽  
Clive Holland
Keyword(s):  
The Arctic ◽  
Hudson Bay ◽  
Minor Importance ◽  
Hudson's Bay Company ◽  
Southern Boundary ◽  
Northern Canada ◽  
North West ◽  
The North ◽  
The Pacific ◽  
Hudson’S Bay Company

If the Treaty of Paris in 1763 secured the Hudson's Bay Company in its monopoly of Rupert's Land, it also, by the Cession of Canada, opened to British enterprise the river-and-lake routes, discovered by the French, from Montreal to the fur-rich country west of Hudson Bay. This instalment of our list covers the years of the Montreal traders' expansion into the North-west, their crossing of the Arctic watershed into the fur trader's Eldorado, the Athabasca district, their organization into the Hudson's Bay Company's formidable rival, the North West Company, and concludes with the climax of their north-westward surge, Alexander Mackenzie's arrival at the Arctic Ocean in 1789. This activity obliged the Hudson's Bay Company to change its policy of waiting for the Indians to bring their furs to posts on Hudson Bay and made them push inland to compete for furs with the pedlars from Montreal. In the meantime, the Moravians had established missions on the coast of Labrador, searches for a North-west Passage were directed away from Hudson Bay to the Pacific coast of North America, the first scientific expedition was sent to Hudson Bay, and the Indians were decimated by smallpox. Toward the end of this instalment, we begin to draw our southern boundary of “northern Canada” both westward and northward and to omit many expeditions and events of peripheral or minor importance, such as activities south of Saskatchewan River, or of regular occurrence, such as annual voyages northward from Churchill.

The Arctic Grail: The Quest for the North West Passage and the North Pole, 1818-1909

1992 ◽  
Vol 25 (3) ◽  
pp. 374
Author(s):  
Jeff Hickey ◽  
Pierre Berton
Keyword(s):  
North Pole ◽  
The Arctic ◽  
North West ◽  
The North

scholarly journals Elevated Potential Instability in the Comma Head: Distribution and Development

2018 ◽  
Vol 146 (4) ◽  
pp. 1259-1278 ◽  
Author(s):  
Andrew A. Rosenow ◽  
Robert M. Rauber ◽  
Brian F. Jewett ◽  
Greg M. McFarquhar ◽  
Jason M. Keeler
Keyword(s):  
Model Simulation ◽  
Convective Available Potential Energy ◽  
Wrf Model ◽  
The Arctic ◽  
Air Masses ◽  
The North ◽  
Arctic Regions ◽  
The Pacific ◽  
Central United States ◽  
Convective Cells

The development of elevated potential instability within the comma head of a continental winter cyclone over the north-central United States is examined using a 63-h Weather Research and Forecasting (WRF) Model simulation. The simulation is first compared to the observed cyclone. The distribution of most unstable convective available potential energy (MUCAPE) within the comma head is then analyzed. The region with positive MUCAPE was based from 2- to 4-km altitude with MUCAPE values up to 93 J kg−1. Backward trajectories from five sublayers within the region of elevated convection in the comma head were calculated to investigate how elevated potential instability developed. Air in the lowest sublayer, the source air for convective cells, originated 63 h earlier near Baja California at elevations between 2.25- and 2.75-km altitude. Air atop the layer where convection occurred originated at altitudes between 9.25 and 9.75 km in the Arctic, 5000 km away from the origin of air in the lowest sublayer. All air in the layer in which convection occurred originated over the Pacific coast of Mexico, the Pacific Ocean, or arctic regions of Canada. Diabatic processes strongly influenced air properties during transit to the comma head. Air underwent radiative cooling, was affected by mixing during passage over mountains, and underwent interactions with clouds and precipitation. Notably, no trajectory followed an isentropic surface during the transit. The changes in thermodynamic properties along the trajectories led to an arrangement of air masses in the comma head that promoted the development of potential instability and elevated convection.

Arctic Exploration and International Law

1909 ◽  
Vol 3 (4) ◽  
pp. 928-941
Author(s):  
James Brown Scott
Keyword(s):  
United States ◽  
International Law ◽  
United States Navy ◽  
The United States ◽  
North Pole ◽  
The Arctic ◽  
The North ◽  
Arctic Regions ◽  
Arctic Exploration ◽  
Scientific Achievements

The announcement on September 1, 1909, by Dr. Frederick A. Cook, that he had discovered the north pole on April 21, 1908, and the almost contemporary declaration on September 6th, of Robert A. Peary, of the United States Navy, in command of the Roosevelt, that he had discovered the north pole on April 6, 1909, are, if substantiated, not only international events and scientific achievements of the greatest interest and value, but the culmination of centuries of effort, directed not merely to reach the pole, but to shorten commercial routes by the discovery of a northwestern and northeastern passage, to advance our knowledge of arctic geography and to make known in a disinterested and scientific spirit, the flora, fauna, and the physical configuration of the arctic regions.

scholarly journals Not across the North Pole: Plant migration in the Arctic

2011 ◽  
Vol 193 (2) ◽  
pp. 474-480 ◽  
Author(s):  
Matthias H. Hoffmann
Keyword(s):  
North Pole ◽  
The Arctic ◽  
Plant Migration ◽  
The North

Little-known arctic species Montacuta spitzbergensis (Bivalvia: Montacutidae) from the north-western Pacific with notes on Montacuta substriata and Tellimya ferruginosa

2008 ◽  
Vol 88 (2) ◽  
pp. 347-356 ◽  
Author(s):  
Gennady M. Kamenev
Keyword(s):  
Sea Of Okhotsk ◽  
First Record ◽  
Western Pacific ◽  
The Arctic ◽  
Arctic Species ◽  
The North ◽  
The Pacific ◽  
The Pacific Ocean ◽  
North Western ◽  
North Western Pacific

An expanded description of a little-known arctic species Montacuta spitzbergensis from the Sea of Okhotsk with new data on its morphology, ecology and geographical distribution is given. This is the first record of M. spitzbergensis from the north-western Pacific. It differs from other species of Montacuta in its large (to 8.4 mm), elongate–ovate, thick shell with wide, slightly curved hinge plate, wide, short, and shallow resilifer, and weakly developed external ligament. This species occurs in the Arctic Ocean (Spitsbergen, Barents, Kara, Laptev and Chukchi Seas) and the Pacific Ocean (Sea of Okhotsk) at depths from 9 to 232 m at a bottom temperature from −1.62°C to +2.50°C. The hinge structure of the type species of the genera Montacuta and Tellimya is also discussed.

scholarly journals Personal fund of hydropower engineer S. V. Grigoriev of the Museum-archive of the BCH KSC RAS

2021 ◽  
Vol 12 (4-2021) ◽  
pp. 28-36
Author(s):  
O. V. Shabalina ◽  
◽  
K. S. Kazakova ◽  
Keyword(s):  
Scientific Study ◽  
Water Bodies ◽  
The Arctic ◽  
Biographical Information ◽  
North West ◽  
The North ◽  
European North ◽  
Potential Sources ◽  
History Of

The article presents materials from the personal fund of the largest hydropower engineer of the North-West of the USSR S. V. Grigoriev, belonging to the Museum-Archive of History of Studying and Exploration of the European North of the Barents Centre of Humanities of the KSC RAS. The personal documents of the scientist and the practitioner are sources of biographical information given in the article and potential sources for research in the field of the history of the scientific study of water bodies, rivers and the development of hydropower in the Arctic.

Sign in / Sign up

Export Citation Format

Share Document