"The sea fryseth not": science and the open polar sea in the nineteenth century

2013 ◽  
Vol 32 (2) ◽  
pp. 235-351
Author(s):  
Christopher Carter

While generally dismissed by historians as a romantic fantasy, the theory of an open polar sea fit into the context of a more unified view of the natural world developed in the early nineteenth century and exemplified by romantic philosophical ideas. Oersted's discovery of electromagnetism encouraged research into the possible connections between electricity, magnetism, heat and light. At the same time, there was renewed interest in geomagnetism inspired by Hansteen's revival of the four-pole theory of the Earth's magnetic field. Incorporating these works into a new theory of climate created a space for an ice-free Arctic by allowing a milder climate in the high latitudes. This attempt to fuse the study of meteorology and geomagnetism reinforced existing beliefs in an open polar sea and placed this sailor's dream into a holistic worldview that joined different natural phenomena in an effort to find one unifying principle behind all of nature.

2015 ◽  
Vol 26 (1) ◽  
pp. 1
Author(s):  
Doug Morrison ◽  
Ivan Barko

In January 1787, on board Lapérouse's Boussole anchored off Macao, the chevalier de Lamanon wrote a letter to the marquis de Condorcet, the then permanent secretary of the Académie Royale des Sciences in Paris. Lamanon's letter contained a summary of his magnetic observations made up to that point on Lapérouse's famous but ill-fated expedition. The letter, amongst other detail, included evidence that the Earth's magnetic field increased in intensity from the equator towards the poles. Sent to Condorcet via the then minister for the French Navy (the maréchal de Castries), the letter was subsequently lost, but not before it was copied. The copy, with early nineteenth-century ownership identified first to Nicolas Philippe Ledru and subsequently to Louis Isidore Duperrey, was itself then lost for over 150 years, but recently rediscovered bound-in with other manuscripts related to the Lapérouse expedition and terrestrial magnetism, including instructions by Ledru and remarks written in the 1830s and 1840s by Duperrey on Lamanon's letter and observations. The significance of Lamanon's letter and the Ledru and Duperrey manuscripts to the history of geomagnetism is discussed here. Duperrey's notes are transcribed in French for the first time and the Lamanon, Ledru and Duperrey manuscripts are translated into English, also for the first time.


1951 ◽  
Vol 4 (02) ◽  
pp. 135-148 ◽  
Author(s):  
A. V. Thomas

The Earth's magnetic field can evidently be divided into its horizontal and vertical components, the horizontal component being of more immediate interest to the navigator since it directs the compass needle in the horizontal plane. Whereas on the magnetic equator the full field is horizontal (about 0·400 c.g.s. units), in high latitudes, with the angle of dip between 60° and70°, H, the horizontal force, maybe about 0·180 c.g.s. units. At the magnetic poleHis negligible and, given the opportunity, the compass needle would point vertically downwards, the instrument then having no directional properties in the horizontal plane.


Author(s):  
A. Soloviev ◽  
A. Khokhlov ◽  
E. Jalkovsky ◽  
A. Berezko ◽  
A. Lebedev ◽  
...  

2011 ◽  
Vol 12 (2) ◽  
pp. 1-9
Author(s):  
A. E. Berezko ◽  
A. V. Khokhlov ◽  
A. A. Soloviev ◽  
A. D. Gvishiani ◽  
E. A. Zhalkovsky ◽  
...  

1967 ◽  
Vol 20 (1) ◽  
pp. 101 ◽  
Author(s):  
KJW Lynn ◽  
J Crouchley

Results of a study at Brisbane of individual night-time sferics of known origin are described. A propagation attenuation minimum was observed in the 3-6 kHz range. The geographic distribution of sferic types was also examined. Apparent propagation asynunetries were observed, since sferics were detected at greater ranges to the west than to the east at 10 kHz, whilst the number of tweek-sferics arising from the east was about four times that arising from the west. Comparison with European studies suggest that these asymmetries are general. These results are then " interpreted in terms of an ionospheric reflection cgefficient which is a function of the effective angle of incidence of the wave on the ionosphere and of orientation with respect to the Earth's magnetic field within the ionosphere.


2019 ◽  
Vol 287 ◽  
pp. 10-20 ◽  
Author(s):  
Kazuhiro Okayama ◽  
Nobutatsu Mochizuki ◽  
Yutaka Wada ◽  
Yo-ichiro Otofuji

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