scholarly journals The North Pole Region as an Indicator of the Changing Arctic Ocean: The Need for Sustaining Observations

ARCTIC ◽  
2018 ◽  
Vol 71 (5) ◽  
Author(s):  
James Morison ◽  
Jeremy Wilkinson ◽  
Matthew Alkire ◽  
Frank Nilsen ◽  
Igor Polyakov ◽  
...  

Sustained observations of environmental conditions in the North Pole region are critical to understanding the changing Arctic Ocean. The Transpolar Drift conduit of sea ice and freshened upper-ocean waters across the Arctic Ocean passes over the North Pole region on its way to the North Atlantic through Fram and Nares Straits. The exported ice and freshened water stratifies the sub-Arctic seas and limits the vertical convection that ventilates the world ocean. Key variables such as ice thickness, bottom pressure, and hydrography in the North Pole region are thus sensitive indicators of changes over the whole Arctic Basin and how these affect the global ocean. Drifting buoys installed in the North Pole region by Great Britain, Canada, France, Germany, Japan, and the U.S. address what would otherwise be a dearth of ocean, ice, and atmosphere observations in the central Arctic. A suite of satellite remote sensing tools such as ICESat/ICESat-2 from the U.S., GRACE from the U.S. and Germany, and CryoSat2 from the European Union extend the conclusions from central Arctic Ocean in situ observations to other regions. Detecting and understanding climate change requires observations over decadal and longer scales. We propose an international program as the key to sustaining these observations in the North Pole region. Such an international program would help immeasurably by 1) facilitating financial sharing of the burden of long-term measurements among several nations, (2) reducing logistics costs through economies of scale, and 3) providing a buffer against national funding, logistics, and geopolitical difficulties.

Author(s):  
V. V. Serikov ◽  
O. Yu. At’Kov ◽  
M. Y. Rubtsov

The survey of the main psychophysiological parameters of pilots before and after the round-the-world oceanic flight around the North pole over the Arctic ocean showed the development of fatigue and General psycho-emotional stress, which indicates some decrease in adaptability, but is not critical to limit the performance of professional duties after rest.


Author(s):  
О.Ю. Атьков ◽  
И.Б. Алчинова ◽  
М.В. Полякова ◽  
Н.Б. Панкова ◽  
С.Г. Горохова ◽  
...  

Целью настоящего исследования стало комплексное изучение динамики перестроек кардиореспираторной системы за время кругосветного океанического перелета вокруг Северного полюса по Северному Ледовитому океану. Методика. В исследовании приняли участие 6 человек, мужчины в возрасте от 39 до 69 лет. Перелет продолжался 6 недель и проходил на высотах до 3000 м. Оценку показателей сердечно-сосудистой системы проводили при помощи приборного комплекса «спироартериокардиоритмограф» (САКР). Результаты. Оценка динамики показателей сердечно-сосудистой системы методом САКР за время кругосветного перелёта выявила у участников экспедиции снижение стресс-индекса и минимальной длительности межсистолических интервалов. Изучение реактивности показателей сердечно-сосудистой системы при проведении нагрузочных проб показало наличие признаков изменения функционального состояния регуляторных систем. The aim of this research was a comprehensive study of the dynamics of cardio-respiratory rearrangements during the round-the-World oceanic flight around the North Pole in the Arctic Ocean. Methods. The study involved 6 men aged 39 to 69. The flight lasted for 6 weeks and took place at altitudes up to 3,000 m. Indexes of the cardiovascular system were assessed using the «spiroarteriocardiorhythmograph» (SACR) instrumental complex. Results. Assessment of the dynamics of cardiovascular indexes using the SACR method during the round-the-world flight showed decreases in the stress index and the minimum duration of inter-systolic intervals in participants of the expedition. Studying the reactivity of cardiovascular indexes during exercise tests showed signs of changes in the functional state of regulatory systems.


1993 ◽  
Vol 67 (S35) ◽  
pp. 1-35 ◽  
Author(s):  
Louie Marincovich

The marine molluscan fauna of the Prince Creek Formation near Ocean Point, northern Alaska, is of Danian age. It is the only diverse and abundant Danian molluscan fauna known from the Arctic Ocean realm, and is the first evidence for an indigenous Paleocene shallow-water biota within a discrete Arctic Ocean Basin faunal province.A high percentage of endemic species, and two endemic genera, emphasize the degree to which the Arctic Ocean was geographically isolated from the world ocean during the earliest Tertiary. Many of the well-preserved Ocean Point mollusks, however, also occur in Danian faunas of the North American Western Interior, the Canadian Arctic Islands, Svalbard, and northwestern Europe, and are the basis for relating this Arctic Ocean fauna to that of the Danian world ocean.The Arctic Ocean was a Danian refugium for some genera that became extinct elsewhere during the Jurassic and Cretaceous. At the same time, this nearly landlocked ocean fostered the evolution of new taxa that later in the Paleogene migrated into the world ocean by way of the northeastern Atlantic. The first Cenozoic occurrences are reported for the bivalves Integricardium (Integricardium), Oxytoma (Hypoxytoma), Placunopsis, Tancredia (Tancredia), and Tellinimera, and the oldest Cenozoic records given for the bivalves Gari (Garum), Neilo, and Yoldia (Cnesterium). Among the 25 species in the molluscan fauna are four new gastropod species, Amauropsis fetteri, Ellipsoscapha sohli, Mathilda (Fimbriatella) amundseni, and Polinices (Euspira) repenningi, two new bivalve genera, Arcticlam and Mytilon, and 15 new bivalve species, Arcticlam nanseni, Corbula (Caryocorbula) betsyae, Crenella kannoi, Cyrtodaria katieae, Gari (Garum) brouwersae, Integricardium (Integricardium) keenae, Mytilon theresae, Neilo gryci, Nucula (Nucula) micheleae, Nuculana (Jupiteria) moriyai, Oxytoma (Hypoxytoma) hargrovei, Placunopsis rothi, Tancredia (Tancredia) slavichi, Tellinimera kauffmani, and Yoldia (Cnesterium) gladenkovi.


1975 ◽  
Vol 15 (73) ◽  
pp. 193-213
Author(s):  
Moira Dunbar

AbstractSLAR imagery of Nares Strait was obtained on three flights carried out in. January, March, and August of 1973 by Canadian Forces Maritime Proving and Evaluation Unit in an Argus aircraft equipped with a Motorola APS-94D SLAR; the March flight also covered two lines in the Arctic Ocean, from Alert 10 the North Pole and from the Pole down the long. 4ºE. meridian to the ice edge at about lat. 80º N. No observations on the ground were possible, but -some back-up was available on all flights from visual observations recorded in the air, and on the March flight from infrared line-scan and vertical photography.The interpretation of ice features from the SLAR imagery is discussed, and the conclusion reached that in spite of certain ambiguities the technique has great potential which will increase with improving resolution, Extent of coverage per distance flown and independence of light and cloud conditions make it unique among airborne sensors.


2010 ◽  
Vol 62 (10) ◽  
pp. 829-832 ◽  
Author(s):  
Jürgen Matzka ◽  
Thorkild M. Rasmussen ◽  
Arne V. Olesen ◽  
Jens Emil Nielsen ◽  
Rene Forsberg ◽  
...  

1975 ◽  
Vol 15 (73) ◽  
pp. 193-213 ◽  
Author(s):  
Moira Dunbar

Abstract SLAR imagery of Nares Strait was obtained on three flights carried out in. January, March, and August of 1973 by Canadian Forces Maritime Proving and Evaluation Unit in an Argus aircraft equipped with a Motorola APS-94D SLAR; the March flight also covered two lines in the Arctic Ocean, from Alert 10 the North Pole and from the Pole down the long. 4ºE. meridian to the ice edge at about lat. 80º N. No observations on the ground were possible, but -some back-up was available on all flights from visual observations recorded in the air, and on the March flight from infrared line-scan and vertical photography. The interpretation of ice features from the SLAR imagery is discussed, and the conclusion reached that in spite of certain ambiguities the technique has great potential which will increase with improving resolution, Extent of coverage per distance flown and independence of light and cloud conditions make it unique among airborne sensors.


2012 ◽  
Vol 27 (1) ◽  
pp. 97-133
Author(s):  
Olya Gayazova

Abstract That the geographic North Pole is the Arctic Schelling point, is implicit in the Russian submission to the Commission on the Limits of the Continental Shelf. I assess this premise vis-à-vis three other approaches to the outer continental shelf delimitation in the Arctic Ocean—the median-line method; a joint submission; and an international zone around the North Pole—and show that both the premise and the alternatives have limitations. Then I explain how an agreement between the Arctic Ocean states (the A5) to establish a seabed nature reserve north of 88°20´N and within 100 nm from the 2,500-meter isobath overcomes those limitations and what positive direct and indirect effects may come from it.


2009 ◽  
Vol 1 (1) ◽  
pp. 499-509 ◽  
Author(s):  
Andrew Serdy

Abstract Despite alarmist media reports and rhetoric from some who should know better, there is no cause for concern about Russian activities on the Arctic seabed. While the melting Arctic Ocean ice cover will have profound consequences for navigation, there is no reason for the resources regime of the continental shelf (including the part beyond 200 nautical miles from the baselines) to be affected, and whatever happens on the seabed will have no effect on sovereignty over the land. The gimmickry of the flag-planting aside, most of the criticism of Russian activities incorrectly assumes they depart from the established international legal framework. In fact they are a good example of compliance with the framework that will have the beneficial effect of contributing to legal certainty about jurisdictional boundaries. Under the rules in Article 76 of the UN Convention on the Law of the Sea for establishing the outer limits of the continental shelf beyond 200 nautical miles, Russia and other coastal States are not making “claims” but merely technical submissions to the Commission on the Limits of the Continental Shelf on where the outer limits of their shelves run. The geological circumstances of the Lomonossov Ridge traversing the North Pole may well support the enclosure of at least part of it within Russia’s continental shelf, and possibly the same would apply to a submission by Denmark from the other (Greenland) end of the Ridge, which it has until 2014 to make. In practice, the distance of the central Arctic Ocean from markets, extreme conditions and high extraction costs make hydrocarbon exploitation there unlikely even at the high oil prices of mid-2008.


2005 ◽  
Vol 52 (10) ◽  
pp. 1988 ◽  
Author(s):  
Kelly Kenison Falkner ◽  
Michael Steele ◽  
Rebecca A. Woodgate ◽  
James H. Swift ◽  
Knut Aagaard ◽  
...  

Polar Record ◽  
1990 ◽  
Vol 26 (158) ◽  
pp. 225-232 ◽  
Author(s):  
Randall J. Osczevski

AbstractThe data used by Dr Frederick A. Cook in support of his claim to have reached the North Pole on 21 April 1908 are reinterpreted to support a hypothesis that Cook did not reach the Pole, that his journey towards the Pole lasted only one week, and thathe subsequently discovered and visited Meighen Island. This reconstruction explains how Dr Cook could have made observations of ice conditions and drift, and of an ice island, without having travelled far out on the Arctic Ocean. A possible reason for his failure to announce discovery of Meighen Island is also offered.


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