Journal articles: 'The North Pole'

1

Röver, Corinna. "North Pole." Polar Journal 9, no. 2 (July 3, 2019): 471–72. http://dx.doi.org/10.1080/2154896x.2019.1678990.

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Sokol, Joshua. "North pole, south pole, wormhole." New Scientist 227, no. 3036 (August 2015): 12. http://dx.doi.org/10.1016/s0262-4079(15)31056-3.

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3

Lee, Hyung Mok, Seong Jin Kim, and NEP-Wide Team NEP-Wide Team. "NORTH ECLIPTIC POLE WIDE SURVEY." Publications of The Korean Astronomical Society 27, no. 4 (September 16, 2012): 129–34. http://dx.doi.org/10.5303/pkas.2012.27.4.129.

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4

Todd, Frank S., R. K. Headland, and Norman Lasca. "Animals at the North Pole." Polar Record 28, no. 167 (October 1992): 321–22. http://dx.doi.org/10.1017/s0032247400028072.

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5

Mullis, C. R., J. P. Henry, I. M. Gioia, H. Böhringer, U. G. Briel, W. Voges, and J. P. Huchra. "The North Ecliptic Pole Supercluster." Astrophysical Journal 553, no. 2 (June 1, 2001): L115—L118. http://dx.doi.org/10.1086/320670.

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6

Mazo, Jeffrey. "Who Owns the North Pole?" Survival 56, no. 1 (January 2, 2014): 61–70. http://dx.doi.org/10.1080/00396338.2014.882152.

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7

Laursen, Lucas. "A Sooty North Pole Ahead." Scientific American 313, no. 5 (October 20, 2015): 20–21. http://dx.doi.org/10.1038/scientificamerican1115-20.

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8

Johnson, M. "Winds at the North Pole." Weather 48, no. 11 (November 1993): 388. http://dx.doi.org/10.1002/j.1477-8696.1993.tb05824.x.

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9

OUSLAND, BØRGE, and KJELL OVE STORVIK. "Alone to the North Pole." Sciences 34, no. 4 (July 8, 1994): 10–14. http://dx.doi.org/10.1002/j.2326-1951.1994.tb03768.x.

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10

Xie, Lilin, and S. R. Dickman. "North Sea pole tide dynamics." Geophysical Journal International 121, no. 1 (April 1995): 117–35. http://dx.doi.org/10.1111/j.1365-246x.1995.tb03515.x.

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11

Aagaard, Knut, and James Johnson. "THE NORTH POLE ENVIRONMENTAL OBSERVATORY MOORING." Oceanography 24, no. 3 (September 1, 2011): 100–101. http://dx.doi.org/10.5670/oceanog.2011.60.

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12

Eberhart, J. "Hexagon Found around Saturn's North Pole." Science News 134, no. 18 (October 29, 1988): 278. http://dx.doi.org/10.2307/3973029.

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13

Kunnikov, Andrey V. "NORTH POLE ARCTIC TOURISM IN RUSSIA." Bulletin of the Moscow State Regional University (Natural Sciences), no. 3 (2019): 41–55. http://dx.doi.org/10.18384/2310-7189-2019-3-41-55.

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14

Brooks, Michael. "What's wrong with the north pole?" New Scientist 242, no. 3236 (June 2019): 34–37. http://dx.doi.org/10.1016/s0262-4079(19)31182-0.

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15

Koerner, R. M., Vladimir Snegiryev, and George Watts. "On Skis to the North Pole." Arctic and Alpine Research 18, no. 3 (August 1986): 354. http://dx.doi.org/10.2307/1550895.

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16

Armstrong, Terence E. "Tourists visit the North Pole, 1990." Polar Record 27, no. 161 (April 1, 1991): 130. http://dx.doi.org/10.1017/s0032247400012274.

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17

Rawlins, Dennis. "Byrd's heroic 1926 North Pole failure." Polar Record 36, no. 196 (January 2000): 25–50. http://dx.doi.org/10.1017/s0032247400015953.

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AbstractRichard E. Byrd's record of the 9 May 1926 flight on which he claimed to have reached the North Pole was unsealed several years ago by the archives of Ohio State University. A close examination of Byrd's writings, calculations, and erasures in this diary shows clearly that, although he and Floyd Bennett achieved a farthest-north-seen and made a heroic attempt to attain the Pole, they never reached that destination. Despite efforts by some organisations and individuals to pretend that there is still a serious controversy, Byrd's own diary data variously confirm the belief long held by most polar experts: that the expedition on the dirigible Norge—led by Roald Amundsen and Lincoln Ellsworth, and piloted by Umberto Nobile — was the first to attain the Pole, on 12 May 1926.

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18

Roy, Preety M. "North pole endotracheal intubation: Extubation technique." British Journal of Anaesthesia 117 (October 2016): el_13607. http://dx.doi.org/10.1093/bja/el_13607.

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19

Pounder, E. R. "Physical oceanography near the North Pole." Journal of Geophysical Research 91, no. C10 (1986): 11763. http://dx.doi.org/10.1029/jc091ic10p11763.

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20

Murata, K., H. Matsuhara, T. Wada, K. Arimatsu, N. Oi, T. Takagi, S. Oyabu, et al. "AKARI North Ecliptic Pole Deep Survey." Astronomy & Astrophysics 559 (November 2013): A132. http://dx.doi.org/10.1051/0004-6361/201321505.

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21

Kazanin, G. S., I. V. Zayats, G. I. Ivanov, E. S. Makarov, and A. S. Vasiliev. "Geophysical exploration at the North Pole." Oceanology 56, no. 2 (March 2016): 311–13. http://dx.doi.org/10.1134/s0001437016020090.

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22

Oslund, Karen. "Not one North Pole, but many." Metascience 29, no. 2 (March 19, 2020): 305–7. http://dx.doi.org/10.1007/s11016-020-00513-3.

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23

Newitt, L. R., and E. R. Niblett. "Relocation of the north magnetic dip pole." Canadian Journal of Earth Sciences 23, no. 8 (August 1, 1986): 1062–67. http://dx.doi.org/10.1139/e86-106.

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An analysis of data gathered between May 13 and May 18, 1984, gives a new position for the north magnetic dip pole of 77.0°N, 102.3°W. The pole has moved an average of 11.6 km per year approximately northwest during the past decade. Data used in the analysis consisted of absolute observations of the magnetic declination, inclination, and total intensity for seven sites in the vicinity of the pole. Variometer data from King Christian Island were used in conjunction with the absolute observations to calculate mean values for the quietest 6 h interval during the survey period. Additional data from Resolute Bay observatory allowed further reduction of the observations to representative annual mean values, centred at 1983.9, from which the pole position was determined using the novel method of spherical cap harmonic analysis.

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24

Nayyeri, H., N. Ghotbi, A. Cooray, J. Bock, D. L. Clements, M. Im, M. G. Kim, et al. "Spitzer Observations of the North Ecliptic Pole." Astrophysical Journal Supplement Series 234, no. 2 (February 8, 2018): 38. http://dx.doi.org/10.3847/1538-4365/aaa07e.

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25

Pastor Yabar, A., M. J. Martínez González, and M. Collados. "Magnetic topology of the north solar pole." Astronomy & Astrophysics 616 (August 2018): A46. http://dx.doi.org/10.1051/0004-6361/201832751.

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The magnetism at the poles is similar to that of the quiet Sun in the sense that no active regions are present there. However, the polar quiet Sun is somewhat different from that at the activity belt as it has a global polarity that is clearly modulated by the solar cycle. We study the polar magnetism near an activity maximum when these regions change their polarity, from which it is expected that its magnetism should be less affected by the global field. To fully characterise the magnetic field vector, we use deep full Stokes polarimetric observations of the 15 648.5 and 15 652.8 Å FeI lines. We observe the north pole as well as a quiet region at disc centre to compare their field distributions. In order to calibrate the projection effects, we observe an additional quiet region at the east limb. We find that the two limb datasets share similar magnetic field vector distributions. This means that close to a maximum, the poles look like typical limb, quiet-Sun regions. However, the magnetic field distributions at the limbs are different from the distribution inferred at disc centre. At the limbs, we infer a new population of magnetic fields with relatively strong intensities (~600−800 G), inclined by ~30° with respect to the line of sight, and with an azimuth aligned with the solar disc radial direction. This line-of-sight orientation interpreted as a single magnetic field gives rise to non-vertical fields in the local reference frame and aligned towards disc centre. This peculiar topology is very unlikely for such strong fields according to theoretical considerations. We propose that this new population at the limbs is due to the observation of unresolved magnetic loops as seen close to the limb. These loops have typical granular sizes as measured in the disc centre. At the limbs, where the spatial resolution decreases, we observe them spatially unresolved, which explains the new population of magnetic fields that is inferred. This is the first (indirect) evidence of small-scale magnetic loops outside the disc centre and would imply that these small-scale structures are ubiquitous on the entire solar surface. This result has profound implications for the energetics not only of the photosphere, but also of the outer layers since these loops have been reported to reach the chromosphere and the low corona.

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26

Bussey, D. Ben J., Kirsten E. Fristad, Paul M. Schenk, Mark S. Robinson, and Paul D. Spudis. "Constant illumination at the lunar north pole." Nature 434, no. 7035 (April 2005): 842. http://dx.doi.org/10.1038/434842a.

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27

Bower, R. G., G. Hasinger, F. J. Castander, A. Aragón-Salamanca, R. S. Ellis, I. M. Gioia, J. P. Henry, et al. "The ROSAT North Ecliptic Pole Deep Survey." Monthly Notices of the Royal Astronomical Society 281, no. 1 (July 1996): 59–70. http://dx.doi.org/10.1093/mnras/278.1.59.

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28

Gerdes, Albert, and Jens Matthiessen. "Was the North Pole Once Ice Free?" German Research 27, no. 2 (November 2005): 24–27. http://dx.doi.org/10.1002/germ.200590017.

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29

Brosch, N., E. Almoznino, D. Engels, S. Bowyer, and M. Lampton. "FAUST observations near the North Galactic Pole." Monthly Notices of the Royal Astronomical Society 316, no. 1 (July 21, 2000): 58–70. http://dx.doi.org/10.1046/j.1365-8711.2000.03548.x.

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30

Serdy, Andrew. "The Long Grass at the North Pole." Yearbook of Polar Law Online 12, no. 1 (December 13, 2021): 210–27. http://dx.doi.org/10.1163/22116427_012010014.

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Though legally no more significant than any other point in the Arctic Ocean, into which State’s continental shelf the geographic North Pole will ultimately fall is politically charged for the three States involved – Canada, Denmark (Greenland) and Russia – that have submitted to the Commission on the Limits of the Continental Shelf outer limits within which the Pole falls. The 2014 Danish submission, for an area extending beyond the equidistance line with Canada, was in that sense paradoxically helpful to Canada, as Denmark, with the northernmost land territory, is by definition closest to the Pole, which must therefore lie on its side of any such line drawn between itself and any other State; thus Denmark gave cover to Canada which needed to take a similar approach to define its continental shelf entitlement as including the North Pole. Boundaries will eventually have to be delimited, but as it likely to be 20 years before the Commission examines the last of the submissions, the three States have ample pretext to postpone this step until then, a solution likely to suit them all.

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31

Pickman, Sarah. "Book review: North Pole: Nature and Culture." cultural geographies 27, no. 4 (May 28, 2020): 683–84. http://dx.doi.org/10.1177/1474474020926186.

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32

CRAWFORD, M. H. "Study Puts Admiral Peary at North Pole." Science 246, no. 4937 (December 22, 1989): 1564–65. http://dx.doi.org/10.1126/science.246.4937.1564-c.

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33

Morison, James, K. Aagaard, K. K. Falkner, K. Hatakeyama, R. Moritz, J. E. Overland, D. Perovich, et al. "North Pole Environmental Observatory delivers early results." Eos, Transactions American Geophysical Union 83, no. 33 (2002): 357. http://dx.doi.org/10.1029/2002eo000259.

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34

Griffin, R. F. "Spectroscopic binaries near the north galactic pole." Journal of Astrophysics and Astronomy 6, no. 1 (March 1985): 71–73. http://dx.doi.org/10.1007/bf02719531.

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35

Griffin, R. F. "Spectroscopic binaries near the north galactic pole." Journal of Astrophysics and Astronomy 6, no. 3 (September 1985): 159–64. http://dx.doi.org/10.1007/bf02714996.

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36

Griffin, R. F. "Spectroscopic binaries near the North Galactic pole." Journal of Astrophysics and Astronomy 6, no. 2 (June 1985): 77–83. http://dx.doi.org/10.1007/bf02715079.

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37

Ross, Heather J. "The North Pole: A heart transplant first." Journal of Heart and Lung Transplantation 30, no. 3 (March 2011): 237–40. http://dx.doi.org/10.1016/j.healun.2010.11.017.

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38

Godfrey, D. A. "A hexagonal feature around Saturn's north pole." Icarus 76, no. 2 (November 1988): 335–56. http://dx.doi.org/10.1016/0019-1035(88)90075-9.

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39

Griffin, R. F. "Spectroscopic binaries near the north galactic pole." Journal of Astrophysics and Astronomy 12, no. 3 (September 1991): 265–68. http://dx.doi.org/10.1007/bf02702881.

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40

Griffin, R. F., and J. J. Eitter. "Spectroscopic binaries near the North Galactic Pole." Journal of Astrophysics and Astronomy 13, no. 2 (June 1992): 209–16. http://dx.doi.org/10.1007/bf02702311.

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41

Griffin, R. F., and D. W. Beggs. "Spectroscopic binaries near the north Galactic Pole." Journal of Astrophysics and Astronomy 12, no. 4 (December 1991): 289–310. http://dx.doi.org/10.1007/bf02702318.

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42

Wang, Xiaoming, Zhijie Jack Tseng, Qiang Li, Gary T. Takeuchi, and Guangpu Xie. "From ‘third pole’ to north pole: a Himalayan origin for the arctic fox." Proceedings of the Royal Society B: Biological Sciences 281, no. 1787 (July 22, 2014): 20140893. http://dx.doi.org/10.1098/rspb.2014.0893.

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The ‘third pole’ of the world is a fitting metaphor for the Himalayan–Tibetan Plateau, in allusion to its vast frozen terrain, rivalling the Arctic and Antarctic, at high altitude but low latitude. Living Tibetan and arctic mammals share adaptations to freezing temperatures such as long and thick winter fur in arctic muskox and Tibetan yak, and for carnivorans, a more predatory niche. Here, we report, to our knowledge, the first evolutionary link between an Early Pliocene (3.60–5.08 Myr ago) fox, Vulpes qiuzhudingi new species, from the Himalaya (Zanda Basin) and Kunlun Mountain (Kunlun Pass Basin) and the modern arctic fox Vulpes lagopus in the polar region. A highly hypercarnivorous dentition of the new fox bears a striking resemblance to that of V. lagopus and substantially predates the previous oldest records of the arctic fox by 3–4 Myr. The low latitude, high-altitude Tibetan Plateau is separated from the nearest modern arctic fox geographical range by at least 2000 km. The apparent connection between an ancestral high-elevation species and its modern polar descendant is consistent with our ‘Out-of-Tibet’ hypothesis postulating that high-altitude Tibet was a training ground for cold-environment adaptations well before the start of the Ice Age.

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43

Barwood, Martin J., Holly Burrows, and Jessica Cessford. "North Pole Marathon Laboratory Lessons and Field Success." Aerospace Medicine and Human Performance 87, no. 5 (May 1, 2016): 493–97. http://dx.doi.org/10.3357/amhp.4498.2016.

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44

Kharitonov, V. V., and V. A. Morev. "Hummocks near the North Pole 35 drifting station." Russian Meteorology and Hydrology 34, no. 6 (June 2009): 379–83. http://dx.doi.org/10.3103/s1068373909060065.

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45

Arlov, Thor B. "Review of The North Pole, by Kathan Brown." Polar Research 25, no. 2 (June 2006): 183–85. http://dx.doi.org/10.3402/polar.v25i2.6297.

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46

SELTZER, RICHARD. "Radar images hint ice at Mercury's north pole." Chemical & Engineering News 69, no. 47 (November 25, 1991): 22–24. http://dx.doi.org/10.1021/cen-v069n047.p022.

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47

Peralta-Ferriz, Cecilia, James H. Morison, Scott E. Stalin, and Christian Meinig. "Measuring Ocean Bottom Pressure at the North Pole." Marine Technology Society Journal 48, no. 5 (September 1, 2014): 52–68. http://dx.doi.org/10.4031/mtsj.48.5.11.

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AbstractHigh-precision deep Arctic Bottom Pressure Recorders (ABPRs) were developed to measure ocean bottom pressure variations in the perennial ice-covered Arctic Ocean. The ABPRs use the tsunami detection DART acoustic modem technology and have been programmed to store and transmit the data acoustically without the need to recover the instrument. ABPRs have been deployed near the North Pole, where the ice cover is a year-round challenge for access with a ship. Instead, the ABPRs have been built as light-weight mechanical systems that we can install using aircraft landing on the ice. ABPRs have provided the first records of uninterrupted pressure data over continuous years ever made in the central Arctic. The ABPR data have allowed us to identify and understand modes of Arctic Ocean bottom pressure variability that were unknown before the ABPR records and have offered new means of investigating and understanding the rapidly changing Arctic system. The ABPR records have also shown outstanding agreement with the satellite-sensed ocean bottom pressure anomalies from GRACE, providing ground truth data for validation of the satellite system. Due to the successful science findings as well as the ABPRs' capability to fulfill the upcoming potential gaps of pressure measurements between GRACE and a GRACE follow-on mission, we highlight the urgent need to develop and maintain an Arctic observing network using ABPRs.

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48

Karáth, Kata. "Why the North Pole is heading towards London." New Scientist 230, no. 3069 (April 2016): 10. http://dx.doi.org/10.1016/s0262-4079(16)30643-1.

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49

Imbert, B. C. "Solo man-hauling journey to the North Pole." Polar Record 23, no. 144 (September 1986): 340. http://dx.doi.org/10.1017/s0032247400007178.

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50

Hansen-Magnusson, Hannes. "Arctic geopoetics: Russian politics at the North Pole." Cooperation and Conflict 54, no. 4 (November 29, 2018): 466–87. http://dx.doi.org/10.1177/0010836718815526.

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The article develops a geopoetic approach to Russian Arctic politics. It rests on the empirical observation that due to climate change, the Arctic landscape is undergoing profound transformations, which has led to multilateral governance efforts but also unilateral pursuits. In this general heterogeneity, Russia’s policies have raised the most pressing questions regarding the country’s motivations to engage in the region. Cultural approaches to global politics are most suitable to create holistic understandings and explanations in this regard, but they lack discussing a spatial dimension of Russian identity. By developing a geopoetic account, the article complements this research through methodological insights from critical geography. Geopoetics focuses on the cultural roots and their cognitive-emotional dimension, on the basis of which claims to the Arctic and related policies resonate with a broader audience. The article argues that Russian policies have their foundation in a utopian ideal of Soviet socialist realism that was widely popularised in the 1920s and later decades. Applying the hermeneutic tool of topos, the article highlights that three features stand out that interweave into a coherent imaginary of the Arctic: first, the heroic explorer; second, the conquest of nature; and third, the role of science and technology. Analysts would do well to bear in mind how the Arctic becomes intelligible when commenting on policies.

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Journal articles on the topic 'The North Pole'

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