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1

Glaβmeier, Karl-Heinz, Heinrich Soffel, and Jörg F. W. Negendank. Geomagnetic Field Variations. Berlin, Heidelberg: Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-540-76939-2.

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2

Sh, Dolginov Sh. Research on the geomagnetic field. Washington, DC: National Aeronautics and Space Administration, 1989.

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3

Musaba, L. Design and performance of synchronous motor drives with field-weakening. Manchester: UMIST, 1996.

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4

Janoo, Vincent C. PCC airfield pavement response during thaw-weakening periods: A field study. [Hanover, N.H.]: US Army Corps of Engineers, Cold Regions Research & Engineering Laboratory, 1996.

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5

Livermore, R. A. The time-average geomagnetic field since the late Palaeozoic. Norwich: University of East Anglia, 1985.

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6

Barraclough, D. R. International Geomagnetic Reference Field 1985: Grid-point values and charts. Aberdeen, Scotland: Secretary General of IAGA, 1986.

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7

Constable, Catherine. Final report on geomagnetic field models incorporating physical constraints on the secular variation. [Washington, DC: National Aeronautics and Space Administration, 1993.

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8

Shui xia di ci dao hang ji shu: Technologies on Underwater Geomagnetic Field Navigation. Beijing: Guo fang gong ye chu ban she, 2013.

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9

Pyrhönen, Olli. Analysis and control of excitation, field weakening and stability in direct torque controlled electrically excited synchronous motor drives. Lappeenranta, Finland: Lappeenranta University of Technology, 1998.

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10

Xanthakis, John N. Geomagnetic field variation as inferred from archaeomagnetism in Greece and palaeomagnetism in British lake sediments since 7000 B.C. Athēnai: Grapheion Dēmosieumatōn tēs Akadēmias Athēnōn, 1991.

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11

Langel, R. A. Types and characteristics of data for geomagnetic field modeling: Proceedings of a symposium held in Vienna, Austria, August 23, 1991. Greenbelt, Maryland: Goddard Space Flight Center, 1991.

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12

McLean, Susan. Bibliography of historical geomagnetic main field survey and secular variation reports at the World Data Center-A for Solid Earth Geophysics. Boulder, Colo: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Environmental Satellite, Data, and Information Service, National Geophysical Data Center, 1993.

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13

Dennis, Smith, World Data Center A for Solid Earth Geophysics., and National Geophysical Data Center, eds. Bibliography of historical geomagnetic main field survey and secular variation reports at the World Data Center-A for Solid Earth Geophysics. Boulder, Colo: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Environmental Satellite, Data, and Information Service, National Geophysical Data Center, 1993.

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14

Kinoshameg, Samantha E. The effects of a simulated geomagnetic sudden storm commencement complex magnetic field treatment on experimental allergic encephalomyelitis (EAE) in female lewis rats. Sudbury, Ont: Laurentian University, School of Graduate Studies, 2004.

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15

A new method for interpreting tectonomagnetic field changes using a natural geomagnetic stress sensor: A contribution to the Joint German-Turkish Earthquake Prediction Research Project. Frankfurt am Main: P. Lang, 1989.

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16

O'Connor, Rodney Philip. A relationship between the amplitude and spectral characteristics of the geomagnetic field and the occurrence of sudden infant death in Canada: A possible cellular mechanism supported by a mathematical modeland experimental evidence for involvement of calcium signalling and nitric oxide. Sudbury, Ont: Laurentian University, Department of Biology, 2001.

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17

Karl-Heinz, Glassmeier, Soffel H. Chr, and Negendank Jörg F. W, eds. Geomagnetic field variations. Berlin: Springer, 2009.

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18

Karl-Heinz, Glassmeier, Soffel H. Chr, and Negendank Jörg F. W, eds. Geomagnetic field variations. Berlin: Springer, 2009.

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19

Geomagnetic field variations. Berlin: Springer, 2009.

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20

Karl-Heinz, Glassmeier, Soffel H. Chr, and Negendank Jörg F. W, eds. Geomagnetic field variations. Berlin: Springer, 2009.

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21

Glaßmeier, K. H., Jorg Negendank, and Heinrich Soffel. Geomagnetic Field Variations. Springer, 2009.

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22

Paterson, Greig A., Christopher J. Davies, and Ron Shaar, eds. The Evolving Geomagnetic Field. Frontiers Media SA, 2019. http://dx.doi.org/10.3389/978-2-88945-895-0.

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23

Dubrov, A. The Geomagnetic Field and Life: Geomagnetobiology. Springer, 2013.

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24

Hale, Christopher James *. Evidence of the archean geomagnetic field. 1986.

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25

Biological Sensitivity to the Geomagnetic Field. Oxford University Press, 2005.

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26

Dubrov, A. The Geomagnetic Field and Life: Geomagnetobiology. Springer, 2013.

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27

Antunes, Fernando Luis Marcelo. A microprocessor-controlled DC servo-drive with spill-over field weakening. 1990.

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28

A, Langel R., Baldwin R. T, and United States. National Aeronautics and Space Administration. Scientific and Technical Information Program., eds. Types and characteristic of data for geomagnetic field modeling. [Washington, DC]: National Aeronautics and Space Administration, Office of Management, Scientific and Technical Information Program, 1992.

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29

Center, Goddard Space Flight, ed. The geomagnetic field and radiation in near-earth orbits. Greenbelt, Md: National Aeronautics and Space Administration, Goddard Space Flight Center, 1999.

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30

A, Langel R., Baldwin R. T, and United States. National Aeronautics and Space Administration. Scientific and Technical Information Program., eds. Types and characteristic of data for geomagnetic field modeling. [Washington, DC]: National Aeronautics and Space Administration, Office of Management, Scientific and Technical Information Program, 1992.

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31

L, Killeen T., and United States. National Aeronautics and Space Administration., eds. Upper thermosphere winds and temperatures in the geomagnetic polar cap: Solar cycle, geomagnetic activity, and interplanetary magnetic field dependencies. [Washington, DC: National Aeronautics and Space Administration, 1995.

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32

R, Ridgway J., and Goddard Space Flight Center, eds. Processing of DMSP magnetic data and its use in geomagnetic field modeling. Greenbelt, MD: National Aeronautics and Space Administration, Goddard Space Flight Center, 1989.

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33

Geological Survey (U.S.), ed. IGRFGRID: A program for creation of total magentic field (International Geomagnetic Reference Field) grid representing the Earth's main magnetic field. [Reston, Va.]: U.S. Dept. of the Interior, Geological Survey, 1990.

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34

Geological Survey (U.S.), ed. IGRFGRID: A program for creation of total magnetic field (International Geomagnetic Reference Field) grid representing the Earth's main magnetic field. [Reston, Va.]: U.S. Dept. of the Interior, Geological Survey, 1990.

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35

M, Gorodnit͡s︡kiĭ A., ed. Anomalous magnetic field of the World Ocean. Boca Raton: CRC Press, 1995.

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36

Opgenoorth, Hermann J., Claudia Stolle, Nils Olsen, and Arthur D. Richmond. Earth's Magnetic Field: Understanding Geomagnetic Sources from the Earth's Interior and its Environment. Springer, 2017.

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37

Fuller, M., T. Yukutake, and M. J. S. Johnston. Tectonomagnetics and Local Geomagnetic Field Variations: Proceedings of IAGA/IAMAP Joint Assembly August 1977, Seattle, Washington. Springer, 2014.

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38

Fuller, M. Tectonomagnetics and Local Geomagnetic Field Variations: Proceedings Of Iaga/Iamap Joint Assembly August 1977, Seattle, Washington. Ingramcontent, 2013.

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39

Yu, Yongjae. Anhysteretic remanent magnetization and thermoremanent magnetization of magnetite : application to paleomagnetism and geomagnetic field intensity determination. [2002], 2002.

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40

United States. National Aeronautics and Space Administration., ed. Magnetospheric substorms and tail dynamics: Final technical report. [Washington, DC: National Aeronautics and Space Administration, 1998.

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41

Types and characteristics of data for geomagnetic field modeling: Proceedings of a symposium held in Vienna, Austria, August 23, 1991. Washington, D.C: National Aeronautics and Space Administration, Office of Management, Scientific and Technical Information Program, 1992.

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42

United States. National Aeronautics and Space Administration., ed. Annual performance report for analysis of plasma measurements for the Geotail mission: Period covered, 1 October 1994-30 September 1995. Iowa City, Iowa: Dept. of Physics and Astronomy, University of Iowa, 1995.

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43

"Magnetotail particle dynamics and transport": Final report for NAGW-1176. [Washington, DC: National Aeronautics and Space Administration, 1995.

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44

United States. National Aeronautics and Space Administration., ed. "Magnetotail particle dynamics and transport": Final report for NAGW-1176. [Washington, DC: National Aeronautics and Space Administration, 1995.

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45

Sergeenkov, Sergei. 2D arrays of Josephson nanocontacts and nanogranular superconductors. Edited by A. V. Narlikar and Y. Y. Fu. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780199533046.013.21.

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This article examines many novel effects related to the magnetic, electric, elastic and transport properties of Josephson nanocontacts and nanogranular superconductors using a realistic model of two-dimensional Josephson junction arrays. The arrays were created by a 2D network of twin-boundary dislocations with strain fields acting as an insulating barrier between hole-rich domains in underdoped crystals. The article first describes a model of nanoscopic Josephson junction arrays before discussing some interesting phenomena, including chemomagnetism and magnetoelectricity, electric analog of the ‘fishtail‘ anomaly and field-tuned weakening of the chemically induced Coulomb blockade, a giant enhancement of the non-linear thermal conductivity in 2D arrays, and thermal expansion of a singleJosephson contact.
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46

Livermore, Roy. Probably the Best Theory on Earth. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198717867.003.0002.

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The magnetic bar-code on the ocean floor provides convincing evidence of moving continents, yet, as with the discovery of the structure of DNA, few are convinced—at first. Drilling in the deep oceans and geochemical work at mid-ocean ridges provides further evidence in support of the Vine–Matthews Hypothesis. Application of the hypothesis to data collected in the Pacific and Atlantic Oceans establishes sea-floor spreading as the process that creates new oceans and, in conjunction with reversals of the geomagnetic field, stamps the bar-code into the rocks beneath the sea bed.
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47

Barany, Zoltan. Armies of Arabia. Oxford University Press, 2021. http://dx.doi.org/10.1093/oso/9780190866204.001.0001.

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In Armies of Arabia—the first book to comprehensively analyze the Gulf monarchies’ militaries—Zoltan Barany explains the conspicuous ineffectiveness of these forces with a combination of political-structural and sociocultural factors. Based on over 150 personal interviews and meticulous multidisciplinary research, he offers a fascinating account of Arabia’s armies starting with Ibn Saud’s conquest of much of the peninsula and ending with the ongoing war in Yemen. He explores the ruling families’ role overseeing their militaries to ensure their loyalty and examines the backgrounds and career trajectories of soldiers and officers. Barany argues that Arabia’s armies remain ineffective because they are characterized by an absence of meritocracy, the domination of personal connections over institutional norms, disregard for personal responsibility, half-hearted leadership, casual work ethic, and training lacking intensity, frequency, and up-to-date settings. Massive expenditures on armaments are primarily payoffs to the United States for protecting them and have resulted in bloated arsenals and large-scale corruption. The setbacks of the Saudi-led coalition’s disastrous war in Yemen starkly illustrate the Gulf armies’ humiliating combat record. The book concludes with thoughts on waste (of human potential, resources, institutions) as a dominant theme of Gulf military affairs, considers likely changes in response to long-term weakening demand for oil, and suggests ways in which the effectiveness of Arabia’s armies could be raised. Chock-full of insights and stories from the field and written with a general audience in mind, Armies of Arabia is essential reading for anyone interested in military affairs and Middle Eastern politics, society, and international relations.
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48

Martin, Graham R. Touch, Taste, and Magnetoreception. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780199694532.003.0004.

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Touch and taste provide information about objects in contact with, and inside, the body for use in detection and manipulation of food items. Four main types of touch receptors are found distributed in most parts of the body but some birds have ‘bill tip organs’ with very high concentrations of touch receptors. Three main types of bill tip organs are found in waterfowl, parrots, shorebirds, ibises, and kiwi. They allow birds to locate hidden objects with the bill alone and parrots to use their bills as third limbs. Seven types of taste receptors exist in birds, mainly in the mouth cavity but also within the gut. Information from these receptors play key roles in food intake and aids shorebirds in detecting profitable feeding locations. Detection of the geomagnetic field, by means of two known mechanisms, is probably widespread among birds. It plays a key role in direction and position finding.
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49

Livermore, Roy. All at Sea. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198717867.003.0009.

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According to first-generation plate tectonics, sea-floor spreading was nice and simple. Plates were pulled apart at mid-ocean ridges, and weak mantle rocks rose to fill the gap and began to melt. The resulting basaltic magma ascended into the crust, where it ponded to form linear ‘infinite onion’ magma chambers beneath the mid-ocean tennis-ball seam. At frequent intervals, vertical sheets of magma rose from these chambers to the surface, where they erupted to form new ocean floor or solidified to form dykes, in the process acquiring a magnetization corresponding to the geomagnetic field at the time. Mid-ocean ridge axes were defined by rifted valleys and divided into segments by transform faults with offsets of tens to hundreds of kilometres, resulting in the staircase pattern seen on maps of the ocean floor. All mid-ocean ridges were thus essentially identical. Such a neat and elegant theory was bound to be undermined as new data were acquired in the oceans.
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