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  • 1
    Publication Date: 2012-09-15
    Description: Love and Gannon (2009) discovered that statistically, over a fifty year period the difference in the dawn and dusk disturbance-field H component at low latitudes (hourly averaged) is linearly proportional to Dst. If the difference is designated by δDD in units of nT/RE, then the Love-Gannon (L-G) relation is δDD = −0.2 Dst. At any time departures from the relation can be large. Nonetheless, the relation is evident for all values of Dst and persists throughout magnetic storms, both the main phase and the recovery phase. The Love-Gannon discovery presents a problem to current understanding of the relation between the causes of δDD and Dst because the dawn dusk asymmetry in the disturbance field is presumably governed by a long-established magnetosphere-ionosphere coupling theory which predicts a characteristic time scale (the shielding time) of less than an hour whereas the characteristic time scale for Dst (the ring current decay time) is more like ten hours. Thus, without forcing both time scales toward each other to the limits of their ranges, a linear proportionality between δDD and Dst cannot be derived from the current understanding of the causes of the asymmetry and the ring current. This conclusion is the paper's main contribution. In addition, we attempt to get around the conflict of time scales by looking at other possibilities for generating δDD that depend directly on the ring current. The most promising of these is the possibility that the ring current decay mechanism creates a quasi-permanent, local-time modification of the ring current compared to what it would be in the absence of the decay mechanism and that this modification causes a field-aligned current that closes through the ionosphere and generates the asymmetry δDD. This idea has the virtue of coupling the asymmetry directly to the ring current and of accounting for the persistence of the L-G proportionality through the recovery phase of magnetic storms.
    Print ISSN: 0148-0227
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 2
    Publication Date: 1989-12-15
    Description: The plasma science experiment on Voyager 2 made observations of the plasma environment in Neptune's magnetosphere and in the surrounding solar wind. Because of the large tilt of the magnetic dipole and fortuitous timing, Voyager entered Neptune's magnetosphere through the cusp region, the first cusp observations at an outer planet. Thus the transition from the magnetosheath to the magnetosphere observed by Voyager 2 was not sharp but rather appeared as a gradual decrease in plasma density and temperature. The maximum plasma density observed in the magnetosphere is inferred to be 1.4 per cubic centimeter (the exact value depends on the composition), the smallest observed by Voyager in any magnetosphere. The plasma has at least two components; light ions (mass, 1 to 5) and heavy ions (mass, 10 to 40), but more precise species identification is not yet available. Most of the plasma is concentrated in a plasma sheet or plasma torus and near closest approach to the planet. A likely source of the heavy ions is Triton's atmosphere or ionosphere, whereas the light ions probably escape from Neptune. The large tilt of Neptune's magnetic dipole produces a dynamic magnetosphere that changes configuration every 16 hours as the planet rotates.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Belcher, J W -- Bridge, H S -- Bagenal, F -- Coppi, B -- Divers, O -- Eviatar, A -- Gordon, G S Jr -- Lazarus, A J -- McNutt, R L Jr -- Ogilvie, K W -- Richardson, J D -- Siscoe, G L -- Sittler, E C Jr -- Steinberg, J T -- Sullivan, J D -- Szabo, A -- Villanueva, L -- Vasyliunas, V M -- Zhang, M -- New York, N.Y. -- Science. 1989 Dec 15;246(4936):1478-83.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17756003" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 3
    Publication Date: 1979-06-01
    Description: Extensive measurements of low-energy positive ions and electrons were made throughout the Jupiter encounter of Voyager 1. The bow shock and magneto-pause were crossed several times at distances consistent with variations in the upstream solar wind pressure measured on Voyager 2. During the inbound pass, the number density increased by six orders of magnitude between the innermost magnetopause crossing at approximately 47 Jupiter radii and near closest approach at approximately 5 Jupiter radii; the plasma flow during this period was predominately in the direction of corotation. Marked increases in number density were observed twice per planetary rotation, near the magnetic equator. Jupiterward of the Io plasma torus, a cold, corotating plasma was observed and the energylcharge spectra show well-resolved, heavy-ion peaks at mass-to-charge ratios A/Z* = 8, 16, 32, and 64.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Bridge, H S -- Belcher, J W -- Lazarus, A J -- Sullivan, J D -- McNutt, R L -- Bagenal, F -- Scudder, J D -- Sittler, E C -- Siscoe, G L -- Vasyliunas, V M -- Goertz, C K -- Yeates, C M -- New York, N.Y. -- Science. 1979 Jun 1;204(4396):987-91.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17800436" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 4
    Publication Date: 1981-04-10
    Description: Extensive measurements of low-energy plasma electrons and positive ions were made during the Voyager 1 encounter with Saturn and its satellites. The magnetospheric plasma contains light and heavy ions, probably hydrogen and nitrogen or oxygen; at radial distances between 15 and 7 Saturn-radii (Rs) on the inbound trajectory, the plasma appears to corotate with a velocity within 20 percent of that expected for rigid corotation. The general morphology of Saturn's magnetosphere is well represented by a plasma sheet that extends from at least 5 to 17 Rs, is symmetrical with respect to Saturn's equatorial plane and rotation axis, and appears to be well ordered by the magnetic shell parameter L (which represents the equatorial distance of a magnetic field line measured in units of Rs). Within this general configuration, two distinct structures can be identified: a central plasma sheet observed from L = 5 to L = 8 in which the density decreases rapidly away from the equatorial plane, and a more extended structure from L = 7 to beyond 18 Rs in which the density profile is nearly flat for a distance +/- 1.8 Rs off the plane and falls rapidly thereafter. The encounter with Titan took place inside the magnetosphere. The data show a clear signature characteristic of the interaction between a subsonic corotating magnetospheric plasma and the atmospheric or ionospheric exosphere of Titan. Titan appears to be a significant source of ions for the outer magnetosphere. The locations of bow shock crossings observed inbound and outbound indicate that the shape of the Saturnian magnetosphere is similar to that of Earth and that the position of the stagnation point scales approximately as the inverse one-sixth power of the ram pressure.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Bridge, H S -- Belcher, J W -- Lazarus, A J -- Olbert, S -- Sullivan, J D -- Bagenal, F -- Gazis, P R -- Hartle, R E -- Ogilvie, K W -- Scudder, J D -- Sittler, E C -- Eviatar, A -- Siscoe, G L -- Goertz, C K -- Vasyliunas, V M -- New York, N.Y. -- Science. 1981 Apr 10;212(4491):217-24.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17783833" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 5
    Publication Date: 1982-01-29
    Description: Results of measurements of plasma electrons and poitive ions made during the Voyager 2 encounter with Saturn have been combined with measurements from Voyager 1 and Pioneer 11 to define more clearly the configuration of plasma in the Saturnian magnetosphere. The general morphology is well represented by four regions: (i) the shocked solar wind plasma in the magnetosheath, observed between about 30 and 22 Saturn radii (RS) near the noon meridian; (ii) a variable density region between approximately 17 RS and the magnetopause; (iii) an extended thick plasma sheet between approximately 17 and approximately 7 RS symmetrical with respect to Saturn's equatorial plane and rotation axis; and (iv) an inner plasma torus that probably originates from local sources and extends inward from L approximately 7 to less than L approximately 2.7 (L is the magnetic shell parameter). In general, the heavy ions, probably O(+), are more closely confined to the equatorial plane than H(+), so that the ratio of heavy to light ions varies along the trajectory according to the distance of the spacecraft from the equatorial plane. The general configuration of the plasma sheet at Saturn found by Voyager 1 is confirmed, with some notable differences and additions. The "extended plasma sheet," observed between L approximately 7 and L approximately 15 by Voyager 1 is considerably thicker as observed by Voyager 2. Inward of L approximately 4, the plasma sheet collapses to a thin region about the equatorial plane. At the ring plane crossing, L approximately 2.7, the observations are consistent with a density of O(+) of approximately 100 per cubic centimeter, with a temperature of approximately 10 electron volts. The location of the bow shock and magnetopause crossings were consistent with those previously observed. The entire magnetosphere was larger during the outbound passage of Voyager 2 than had been previously observed; however, a magnetosphere of this size or larger is expected approximately 3 percent of the time.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Bridge, H S -- Bagenal, F -- Belcher, J W -- Lazarus, A J -- McNutt, R L -- Sullivan, J D -- Gazis, P R -- Hartle, R E -- Ogilvie, K W -- Scudder, J D -- Sittler, E C -- Eviatar, A -- Siscoe, G L -- Goertz, C K -- Vasyliunas, V M -- New York, N.Y. -- Science. 1982 Jan 29;215(4532):563-70.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17771279" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 6
    Publication Date: 1986-04-18
    Description: The vector helium magnetometer on the International Cometary Explorer observed the magnetic fields induced by the interaction of comet Giacobini-Zinner with the solar wind. A magnetic tail was penetrated approximately 7800 kilometers downstream from the comet and was found to be 10(4) kilometers wide. It consisted of two lobes, containing oppositely directed fields with strengths up to 60 nanoteslas, separated by a plasma sheet approximately 10(3)kilometers thick containing a thin current sheet. The magnetotail was enclosed in an extended ionosheath characterized by intense hydromagnetic turbulene and interplanetary fields draped around the comet. A distant bow wave, which may or may not have been a bow shock, was observed at both edges of the ionosheath. Weak turbulence was observed well upstream of the bow wave.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Smith, E J -- Tsurutani, B T -- Slvain, J A -- Jones, D E -- Siscoe, G L -- Mendis, D A -- New York, N.Y. -- Science. 1986 Apr 18;232(4748):382-5.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17792150" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 7
    Publication Date: 1986-07-04
    Description: Extensive measurements of low-energy positive ions and electrons in the vicinity of Uranus have revealed a fully developed magnetosphere. The magnetospheric plasma has a warm component with a temperature of 4 to 50 electron volts and a peak density of roughly 2 protons per cubic centimeter, and a hot component, with a temperature of a few kiloelectron volts and a peak density of roughly 0.1 proton per cubic centimeter. The warm component is observed both inside and outside of L = 5, whereas the hot component is excluded from the region inside of that L shell. Possible sources of the plasma in the magnetosphere are the extended hydrogen corona, the solar wind, and the ionosphere. The Uranian moons do not appear to be a significant plasma source. The boundary of the hot plasma component at L = 5 may be associated either with Miranda or with the inner limit of a deeply penetrating, solar wind-driven magnetospheric convection system. The Voyager 2 spacecraft repeatedly encountered the plasma sheet in the magnetotail at locations that are consistent with a geometric model for the plasma sheet similar to that at Earth.〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Bridge, H S -- Belcher, J W -- Coppi, B -- Lazarus, A J -- McNutt, R L Jr -- Olbert, S -- Richardson, J D -- Sands, M R -- Selesnick, R S -- Sullivan, J D -- Hartle, R E -- Ogilvie, K W -- Sittler, E C Jr -- Bagenal, F -- Wolff, R S -- Vasyliunas, V M -- Siscoe, G L -- Goertz, C K -- Eviatar, A -- New York, N.Y. -- Science. 1986 Jul 4;233(4759):89-93.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/17812895" target="_blank"〉PubMed〈/a〉
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 8
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] A second encounter took place on September 21 1974 but the spacecraft passed the planet on the Sunward side at too great a distance to permit observations inside the planet's bow shock. The third and last encounter (Mercury III) took place on March 16 1975 at which time the spacecraft passed within ...
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  • 9
    ISSN: 1573-093X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract The assumption of the existence of steady state, linearized, inhomogeneous solar wind flow imposes a relation between the perturbation variables such that the solutions are regular at the critical points. The critical point regularity conditions are derived for the case of hydromagnetic flow with no rotation, for which there are two critical points, and the case of hydrodynamic flow with rotation and one critical point. It is possible the organization imposed by the critical points is reflected in correlations observed between solar wind parameters near the orbit of Earth. Analytic asymptotic solutions are also derived to complete the description given previously of the intermediate range flow obtained by numerical integrations. The asymptotic solutions can be described in terms of pressure waves that in general propagate radially with respect to the zero-order flow. The pressure perturbation for expected solar wind conditions is found to increase with distance and the velocity perturbations to decrease.
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  • 10
    Electronic Resource
    Electronic Resource
    Springer
    Solar physics 56 (1978), S. 449-461 
    ISSN: 1573-093X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Physics
    Notes: Abstract Measurements of the north-south (B z component of the interplanetary field as compiled by King (1975) when organized into yearly histograms of the values of ¦B z ¦ reveal the following. (1) The histograms decrease exponentially from a maximum occurrence frequency at the value ¦B z ¦ = 0. (2) The slope of the exponential on a semi-log plot varies systematically roughly in phase with the sunspot number in such a way that the probability of large values of ¦B z ¦ is much greater in the years near sunspot maximum than in the years near sunspot minimum. (3) There is a sparsely populated high-value tail, for which the data are too meager to discern any solar cycle variation. The high-value tail is perhaps associated with travelling interplanetary disturbances. (4) The solar cycle variations of B z and the ordinary indicators of solar activity are roughly correlated. (5) The solar cycle variation of B z is distinctly different than that of the solar wind speed and that of the geomagnetic Ap disturbance index.
    Type of Medium: Electronic Resource
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