_________________________________________________________
Solar
or Interplanetary External Magnetic Field?
Mahmoud E. Yousif
E-mail: yousif_474@yahoo.com/
C/O
Physics Department - The University of Nairobi
P.
O. Box 30197 - 00100 - Nairobi-Kenya
PAC
No: 96.50.Ci; 96.50.Bh; 96.50.Fm; 07.55.Db; 94.30.cj; 52.35.-g; 96.60.T-,
96.60.Tf; 94.30.Lr
ABSTRACT
Analysis of Pioneer V
engulfment with solar plasma on March 30, 1960, showed that solar magnetic
field was not detected by the probe, rather a high interplanetary magnetic
field (IMF) was later measured after first been recorded by Honolulu earth
station; this questioned envisioned embedded solar magnetic field. A proposed
mechanism of solar wind captured at and before the bow shock, producing
Interplanetary-External Magnetic Field (I-ExMF), led to
energization of these particles; while boundaries between IMF represent space
between intermittent produced I-ExMF. Intense I-ExMF (II-ExMF) is
produced around 12.5RE within magnetosheath, igniting
transitory magnetic waves (lion roars); initiating the sudden
commencement and related main phase. Explanation of these, and the
propagation of magnetic disturbances and the interplanetary sector structure,
is based on I-ExMF characteristics. Understanding these
mechanisms will reflect positively on attaining the alternative renewable green
energy that can protect our planet, environment and establishment of more
advanced human society.
1.0 Introduction
Contrary to the name, the interplanetary
magnetic field (IMF) refer to the magnetic field embodied in the solar plasma [Parker,
1958], that means, the solar magnetic field present in the Corona is carried by
the emitted particles, hence the solar wind is said to carry an entrained magnetic
field [McDonald, 2005], which means the solar wind and its entrained IMF,
could be carried all along the nine planet to inflate the heliosphere [McComas et al, 2011], or as far as solar
plasma can reach.
The usage of rockets in
1947 for scientific studies, had lead to the launch of first satellites Sputnik
3 in 1958 for magnetic measurement, then Vanguard 3 in 1959 that measured
strong field near earth, [Heppner, 1967], culminated with more
investigations during the international Geomagnetic Year 1958/57 [Ness and
Burlaga, 2001; National
Academy of Science,1961],
then came series of satellites, the unique of which was Pioneer V which
presented what thought to be the prove for the solar origin of the IMF [Coleman
et al., 1961], then came the Interplanetary Monitoring Platform-1 (IMP-1 or
IMP-A)
satellite, in 1963 to study the IMF, radiation between the earth and the moon,
and earth-sun relationships [Heppner, 1967], all of which resulted in
the discovery of Van Allen radiation belt [Van Allen, 1959], and an anomalies
magnetic field opposite
in direction to the geomagnetic field, several radial distance from the earth [Wilcox,
1966].
The IMP-1 satellite magnetic data was
interpreted as a proof to Pioneer V data [Wilcox and Ness, 1965],
and related to observations on the sun [Wilcox, 1966; Wilcox and Ness, 1965], in
accordance to the solar spiral magnetic field theory by Parker [Parker,
1958], developed into the reconnection theory to resolve auroral problems [Dungey, 1962], but the IMF originated from a page by
Hannes Alfvén to Nature
in 1942 [Alfvén, 1942a], and the frozen in magnetic
field expression appeared later [Alfvén,
1942b], both papers got attention in 1948, when the prominent physicist Enrico Fermi appreciated seminar by Alfvén
in public saying “of course such waves could exist.” [Fälthammar, 2012].
The IMF has brought the idea of neutral points,
with the formation of current sheet, to explain the discontinues changes in
field direction [Dungey, 1967], thus IMF, was suggested to explain detected and measured anomalous
magnetic fields, which opposite in direction to geomagnetic field and
continuously changing in direction [Heppner 1967].
Some thinks the IMF had complicated the solar wind as a material to be dealt
with, [Russell, 2000] and consequences to that, the IMF brought with it
three types of disturbances as a mechanism to allow for the plasma/field to be
interacted with the magnetosphere [Russel,
2000a], thus the IMF had great impact on astrophysics, with nearly all related present
theories and interpretations emerged from it, among such interpretations are:
-
The magnetosphere was suggested [Gold,
1959; Beard, 1964] and conceived to be closed cavity [Beard,
1964].
-
Solar wind was suggested to carry away lines of force of the
outer geomagnetic field as suggested by Parker [Wolfe and Mayers, 1966].
-
The solar wind was envisioned to flow around the
cavity [Dungey, 1961]
-
The introduction of neutral points [Dungey, 1967].
-
The suggestion of reconnection mechanism for
substorms [Dungey, 1961].
-
Interpretation of neutral sheet
[Ness, 1965],
which brought credibility to Dungey [1961],
connection of geomagnetic field lines with the interplanetary magnetic field,
which was also tackled by Alfvén [1963].
-
The
mechanism of Aurora particles in Auroral Oval was thought to be driven by
magnetic reconnection from magnetotail [Dungey,
1963].
-
Connection mechanism also taken to the sun [Priest and Forbes, 2000].
-
The Solar Flare explosion is thought to be activated
through the magnetic reconnection [Priest and Forbes, 2000], and is thought to play major role in the
energy release process and possibly in the subsequent evolution, it has been
invoked to explain chromospheres eruptions and many other solar phenomena [Karpen et al., 1989].
On March 11, 1960, Pioneer V was launched, in
orbit sufficiently far from Earth and its magnetic field and solar wind
interaction region so as to sample the physical properties of the undisturbed
interplanetary medium [Ness and Burlaga, 2001], it was nearly at 5.2
x 106 km or 863RE on the Sun-Earth line on 30
March 1960, when a large solar flare erupted on the sun, the plasma reached the
satellite and earth the following day [Coleman et al., 1961]. Combination
of measured data by Fan et al. [1960a], and Coleman et al.
[1961], lead to a conclusion that Pioneer V didn’t detected the embedded IMF
when first engulfed with the incoming plasma, rather a maximum interplanetary magnetic field of 23γ was
measured eight hours later, and the peak of that IMF was measured by Pioneer V two
hours after a similar peak changed the horizontal component of geomagnetic
field at Honolulu station [Coleman et al., 1961], that lead to a
confusion in determining the source of the IMF, although earlier Fan et al.
[1960a] stated that “our results describe large-scale transient magnetic fields
over great distances from Pioneer V, the magnetometer in Pioneer V
registers field changes at the position of the vehicle perpendicular to its
spin axis.” Local production of IMF was also assume from Pioneer V data as
expressed by Fan et al. [1960a] “Both kinds of observations show that
magnetic fields are being moved or generated in interplanetary
space as a consequence of the solar flare on March 30.” The above lead to
confusion, with no alternatives, they added “The only known way by which these transient
fields could be established, or existing fields
manipulated, is by moving, conducting plasma of solar flare origin.”
The first statement should have lead to more experiments
of that kind instead, a decision was made to support Parker [1958]
theory, and Fan, Meyer, and Simpson [1960] stated that “Therefore,
we believe these Pioneer V results provide the most direct evidence to date for
the existence of conducting gas ejected at high velocity from solar flares, a
concept strongly supported already by many solar and terrestrial observations.”
Although this last statement bears no historical responsibility, but the
question is what if the IMF was and is “generated in the interplanetary
space as a consequence of the solar flare or solar wind interaction with
geomagnetic field?” as inferred from Fan et al. [1960a] first two
statements?
Within five years from Pioneer V launch, the IMF was
envisioned as of solar origin, and after nearly five decades, from endorsement
of Parker theory [Parker, 1958], Pioneer V results
is fading away, and the IMF became more complicated.
These discrepancies,
required a review of the old literatures, related to early satellites
measurements, hence generally, although the radial variation of the IMF
strength up to 19 AU was thought to be in consistent with Parker's model, [Burlaga
et al., 1998], and that is supported by some, who thinks the IMF magnitude
only varies by fractions of a gamma on long time, [Ness et al., 1964], while
Coleman et al. [1960b] deduced that the measurements would be much more
irregular, if the field were imbedded in clouds of turbulent gas emitted from
the sun, and it has been determined that the IMF falls off significantly faster
than predicted by Parker, as stated by Slavin
et al. [1984], who also implies the existence of other factors that may be
responsible about the production and declination of the IMF, where several
studies by Pioneer 11 data suggest that the magnetic field strength decreases
more rapidly with distance than predicted by Parker's model [Smith and
Barnes, 1983].
On the other hand, the
sudden increase in magnetic field which determines the bow shock, boosted an
already existed IMF, such increases is interpreted at the time at which the
average field level deviates from the interplanetary level, it is usually
identifiable within two seconds [Heppner et al., 1967], abnormally strong
IMF, can reach 63γ at 10.5RE, and magnitude of 125γ
had been measured at 8.25RE [Cahill and Amazeein, 1963], while the magnetopause location also depends on the IMF
intensity [Heppner et al., 1967] and that the simultaneous
plasma measurements from OGO-A and Vela 2 satellites shows that the abnormal
bow shock position is primarily the result of an exceptionally strong IMF
occurring simultaneously with an inflated magnetosphere [Heppner et al.,
1967], such anomalies were even detected at the magnetic clouds between 2 and 4
AU which were larger than those seen at 1 AU [Burlaga et al., 1982], all
these raised a question about the limit of embedded solar magnetic field, which
should allowed for alternative option, such as the local production of magnetic
field within the interplanetary space.
Then came the greatest shock; the magnetosphere which
was considered an impenetrable blunt body [Russel,
2000a], was breached, in several places and continually [Angelopoulos et al.,
2008], some tried to seek explanation within the solar IMF-origin, by proposing
Hidden
Portals in Earth's Magnetic Field [Phillips, 2002]. But as the penetration recently proven [Angelopoulos
et al., 2008], it was already been known that, solar wind continually blow
into the magnetosphere [Neugebauer
and Snyder, 1962], and flow of energetic protons is the prominent feature of the magnetosheath [Gosling
et al., 1967], and that, satellites measurements, established strong relation
between increase in magnetic field, solar wind density, and energization
process, Heppner et al. [1967]. All these points to the
extreme complexity of the magnetosheath which is dominated by phenomena such as
local acceleration, injection, and diffusion of high energy electrons, twisted
magnetic fields, turbulent plasma flow, and probably a great variety of wave
phenomena [Wolfe and Mayers, 1966].
The odd status of the
boundaries [Cahill and Amazeein, 1963] are highlighted
as an example to emphasize relationship between these boundaries and
intermittent anomalies magnetic fields, while detection of such southward-directed
rotation of field F, by Exp. 6 around 8RE,
found to be similar to rotation of dipole field lines detected by Exp. 10
between 6-20RE, [Smith, 1962], as these showed
deformation of the geomagnetic field, it also showed existence of different
method that produced these anomalous fields, hence a suggestion of spatial
production of intermittent Interplanetary-External Magnetic Field (I-ExMF)
along the geomagnetic lines of forces; resulted from captured and gyrating
solar wind along these lines of force at or before the bow shock, these characteristics
energized captured particles to higher energy levels. Thus the source of the magnetic
event recorded at Honolulu station and later by Pioneer V [Fan et al.,
1960a], is traced to magnetosheath at 12.5RE, during magnetic
storms, when energetic protons flow across the boundary, where intense I-ExMF
(II-ExMF) is thought to be produced. As the paper tackle the production
of I-ExMF, from perspective related to the IMF, the magnetic
storms are been related to the production of the magnetic waves (Lion roars) [Smith
et al., 1969] which is thought to modulate the produced II-ExMF,
and initiated geomagnetic storms, measured world wide as Dst.
The interplanetary sector structure, which was thought to originate from the
sun [Wilcox and Ness, 1965] is explained based on I-ExMF
related characteristics.
If Lord Kelvin in 1892 can
refute, any connection between magnetic storms and any kind of dynamical action
on the sun [Curto et al., 2007], and
that the autocentric principle can dominate human believes at pre-Copernican dogma
[Carter, 2006], both examples showed how error can form a guiding principle for
an individual or general scientific community.
But what about measurements
carried out IMF by many satellites during the past five decades, all of which
shows IMF existence?
Since solar wind speed
of flows was found to be about 400 km s-1 with density of 5 cm-3
[Russell, 2000], and the IMF resulted mainly from relatively steady magnetic
field of ~4.5nT and a highly variable components [Svalgaard,
et al., 2003], therefore the relatively steady I-ExMF component is
the one always produced at specific local spatial areas as long as the solar
wind continued flowing from the sun and interacts at appropriate planet field,
while the variable components is caused by any increased in solar wind.
The accurate knowledge of mechanism causing
different stages of magnestorm in our near vicinity is the first step towards a
better understanding of our sun, nearest stars, Galactic system, and a process
towards developing the required alternative, sustainable and renewable energy
and related propulsion systems needed by current and future generations.
2.0 Assertion of the Interplanetary Magnetic Field
Pioneer
V measurements were conducted during an active period of March to June 1960, and
gave raises to interplanetary magnetic field of 20-50γ, greater than
normal field component of 2.5γ, although this later been corrected [Ness and
Burlaga, 2001], the field was perpendicular to the probe’s spin of axis,
thus nearly perpendicular to the earth-sun line [Coleman et al., 1961] a
year later, Exp. 10 was launched on March 25, 1961, it confirmed these readings
and added that, a steady increase in measured filed, till 42.5RE,
and from 42.25 to 42.7RE, the field increased by more than
25γ, [Heppner et al., 1963] or an increase of 250% percentage.
Later,
Exp. 12 was launched on August 16, 1961, it confirmed the above, and measured magnetic
fields of 63γ, at 10.5RE, and 50γ at the same
spatial area after 14 hours on an outbound flight, and again on 13 September
1961, it measured a field of 125γ at 8.25RE, while
changes in both angles α and ψ indicate that the field
immediately outside the boundary is antiparallel to
the earth’s field [Cahill and Amazeein, 1963].
Mariner 2, launched on August 27, 1962, gave measurements that consistent with
interplanetary field in the plane of the ecliptic with a strength of
approximately 5γ normal to a sun-satellite direction, with magnitude
comparable to Pioneer 5 data, but different by 90o [Ness et al.,
1964].
Thus
results from Exps.6, 10, 12 and 14 lead some authors to conclude that the obtained
data seemed to fit Dungey’s [1961] model of
the distorted geomagnetic field, which includes the connection of geomagnetic and
interplanetary field lines [Ness, 1965].
For all these, the interplanetary
monitoring platform IMP-1 (or Exp. 18) was sent to investigate the magnitude,
direction, and temporal variations of the IMF, the results strongly suggested existence of filamentary
structure in the interplanetary medium associated with sources of solar
magnetic fields, interpreted as stretched from the sun by the plasma as discussed
by Parker [1958], it also explained the abrupt decrease of magnetic
field magnitude to zero as a null surface separating regions of opposite fields
[Ness et al., 1964].
2.1
Re-Visiting the
Historical Experiment
Exps.6,
10, 12, 14 and 18, probes were sent to confirm the measured high IMF magnitude
by Pioneer V, which occurred nearly concurrently with the registration of large
amplitude change in the horizontal component of the geomagnetic field, at
Honolulu station shown in Figs.1-A&B [Coleman et al., 1961], the measurements
confirmed strong link between both events [Coleman et al., 1961].
In
one of their reports about that experiment, there was doubts about where IMF was produced, as Fan et al.
[1960a] stated “great transient magnetic fields was produced far from Pioneer V, but measured by
Pioneer V”, such discrepancy is
clear from the statement that,
“solar
plasma either carries magnetic fields, or manipulate an interplanetary magnetic
field [Fan et al., 1960a].” But there is no
mention about an embedded magnetic field, rather they referred it indirectly to
the sun due to lack of alternative, where Fan et al. [1960b] stated that
“The only known way by which these transient fields could be
established, or existing fields manipulated, is by moving, conducting plasma of
solar flare
origin.”
Since
the measurements represent a corner stone in the current theory for the solar
origin of the IMF, and all related explanations emerged from it, we would like
to re-visit the experiment, because we observed loophole in it, in addition to
the failure of current models to replicates the great source of energy contained
within the solar wind.
The
large event of March 30, 1960, was detected and analyzed by Pioneer V, while
the probe was nearly 5.2 x 106 km or 863RE on the
Sun-Earth line [Fan et al., 1960a]. The ejection of plasma from the
solar flare of importance 2 at 14:55 – 18:58 U. T. on March 30 led to the
commencement of the geomagnetic storm and the beginning of the cosmic radiation
intensity decrease at about 12:00 U. T. on March 31; with average velocity of
2000 km/sec, the time difference between plasma arrival at Pioneer V and at the
earth was estimated around ~43 (50) minutes [Fan et al., 1960a].
Fig.1,
is a composition of both Figs.2.a&b by Coleman et al. [1961] depicting
magnetic field measurements at both Pioneer V and Honolulu station, with the same
time sequence of events, the other is Fig.2-A, by Fan et al. [1960a], it
shows timing of the solar flare, and plasma arrival at Pioneer V and the earth.
These three figures are combined in Fig.1-A-B-C respectively, in a manner
representing the true timing and sequence of March 30/31, 1960 events, from the
start of solar flare, plasma arrival at Pioneer V, plasma arrival at earth
boundary, the starts of change in horizontal component at Honolulu and
detection of IMF by Pioneer V; all these can be described in the following
sequences, where the numbers of these sequences are printed at top of Fig.1-C,
and traceable to the timeline and designated positions:
1- The
first flare Started on 30 March 1960, at 14:55–18:58 U.T. Fig.1-C. [Fan et
al., 1960a]
2- Arrival
of first plasma at Pioneer V orbit on 31 March 1960, at 05:40 U.T. (~50 minutes
before arrival at earth), Fig.1-C. [Fan et al., 1960a].
3- Arrival
of first plasma with speed greater than 2,000 km s-1, to earth on 31
March at 6:30 U.T. (50 minutes after first arrival at Pioneer V), till Fig.1-A.
[Fan et al., 1960a].
4- First
increase in IMF as measured by Pioneer V on March 31, 1960, at 07:20 U.T. (1h
40 min. after plasma first arrival at Pioneer V), from Fig.1-B&C.
5- Severe geomagnetic storm, accompanied by major earth current disturbances, a complete blackout of the North Atlantic communications channel, and auroral displays, started on earth on March 31 at
08:00 U.T. (2h 20min after plasma first arrived to Pioneer V), Fig.1-A. [Arnoldy et al., 1960]
6- Maximum
magnitude of horizontal field registered at Honolulu, on March 31, 1960, at
11:50 U.T. (6h 10 min. after first plasma arrival at Pioneer V), Fig.1-A. [Coleman
et al., 1961].
7- Maximum
magnetic field of 23.4γ registered at Pioneer V on 31 March, at 1:50 U.T.
(8h 10 min. after plasma first arrival to Pioneer V), Fig.1-B. [Coleman et
al., 1961].
From
this sequence and in relation with Fig.1 (A, B, and C), the following
observations are made:
-
For more than 1:40
hours, after been engulfed with plasma, Pioneer V didn’t detect any increase in
the interplanetary magnetic field, as shown in Fig.1-B.
-
After solar
plasma arrival to the earth at 6:30 U.T., magnetic fields at Pioneer V start
increasing gradually, while it first decreased at Honolulu station.
-
Magnetic field
recorded at Honolulu station increased and reached maximum reading, as shown in
Fig.1-A, by point 6 at 11:50 U.T., after 6:10 hours from plasma arrival at
Pioneer V.
-
Maximum magnitude
of 23.4γ measured by Pioneer V, as shown in Fig.1-B, by point 7 at 13:50
U.T. after 8:10 hours from Pioneer V first engulfment with the plasma, and after 2:03 hours from maximum field measured at
Honolulu, the same measurement was recorded at Fort Belvoir [COLEMAN et al.,
1960a].
Since
Pioneer V failed to detected any increase in IMF for more than 1:40 hours, after
first engulfed by solar plasma, and the magnetic fields charts for both
Honolulu station and pioneer V start changing simultaneously, afterwards as
shown in Fig.1-A&B, and the maximum magnitude of magnetic field recorded at
Honolulu occurred before Pioneer V, and since Fan et al. [1960a] first conclusion was in
line that “large-scale transient magnetic fields over
great distances from Pioneer V, measured by Pioneer V”,
therefore we concluded that the magnetic field which was measured at
Honolulu station and the IMF at Pioneer V, were produced from one source, and
it is not of solar origin, and that:
1- If
the IMF was embedded in the plasma, Pioneer V should have detected it, instantly
when Pioneer V was first engulfed with the solar plasma.
2- If
the IMF was embedded in the plasma, Pioneer V should have detected it before
Honolulu station.
3- Sequence
of events showed that, the magnetic field spreads towards both Honolulu, where
it disturbs the horizontal component of geomagnetic field, and to Pioneer V,
thus both fields’ moves oppositely from one source of production.
4- The
IMF was produced at a period of time, between plasma arrival to the earth boundary
and first magnetic change at Honolulu station.
5- The
IMF was produced at a spatial location, nearer to Honolulu station rather than to
Pioneer V.
Based
on above conclusion, a model will be presented based on measurements and
analysis been carried out during the past five decades.
3.0
Boundaries or Spatial Produced Interplanetary
Magnetic Fields?
Reviewing Exp.12 measurements
given by Cahill and Amazeein, [1963] in Fig.2;
it showed many anomalies fields, some were interpreted as boundaries, with magnitudes
greater than the computed fields, with difference ΔF = F
(measured) – B (computed). In these measurements, the number of changes
between fields are nearly equivalent to number of change in angles detected by
both ψ and α, as given in Table.1, which is derived
from figures, 4, 5, and 6 [Cahill and
Amazeein, 1963].
From
Figures |
Radial
Distance (RE) |
Number
of Bx Change |
Number
of ψ Change |
|
Fig.4 |
1st |
4.3
to 8.74 |
40 |
42 |
2nd |
10.4 to
13.1 |
27 |
32 |
|
Fig.5 |
1st |
4.4 to
5.73 |
9 |
14 |
2nd |
5.5 to
13.2 |
61 |
66 |
|
Fig.6 |
4.5 to
10.9 |
44 |
49 |
Table.1. Number of
measured magnetic fields boundaries (Bx),
is equal to change in angle ψ, as given in Figures 4, 5 and 6, by
Exp.12 [Cahill and Amazeein, 1963], the
boundaries are thought to represents intermittent production of magnetic
fields.
The change in magnetic
fields or boundaries phenomena was revealed by satellites measurements [Heppner,
1967; Gosling et al. 1967], the satellites were found to cross several
boundaries during such experiments, with thickness of each boundary range from
100 km to 1000 km, [Cahill and Amazeein, 1963;
Heppner, 1967], and a single and multiple crossings of the shock are
observed [Gosling et al., 1967], while seven boundaries crosses took
place within three hours [Burlaga and Ogilvie, 1968], and as the
boundary is traversed, often multiple crossings of the boundary occur for which
the boundary apparently sweeps back and forth across the spacecraft [Gosling
et al., 1967], and boundaries were perpendicular to the earth-sun line in
many cases [Heppner, 1967; Coleman et al., 961; Ness et al.,
1964], which means they were perpendicular to the magnetic lines of force,
while such fields were detected by Exp.12 at lower radial distance of 4 to 4.5RE,
as shown in Fig.2, which is a representation of Figure 5 by Cahill and Amazeein
[1963], and the fields also has been detected between 42.25 to 42.7RE,
with magnitude of 25γ [Heppner et al., 1963]. While for
magnetopause, the magnetic field directions adjacent to the boundary were, in general
tangential to the magnetopause surface but oppositely directed on the two
sides, although they were perpendicular in some cases [Heppner, 1967], and
Coleman
et al. [961] concluded that geomagnetic field termination
took place near 14RE on the ground that the field
intensities between 7 and 13RE were greater than expected, and
the field on the far side of the boundary decreased more rapidly than 1/r3,
and power level of fluctuation decreased in passing the boundary [Heppner,
1967], while on some other passes there is indication that the boundary has
moved past the satellite [Cahill and Amazeein,
1963], this been consolidated by results obtained from Exps.12, 14 and 18 in
sunward hemisphere, which showed that the termination near 14RE
as detected by Pioneer 1 and 5 is now identified with the shock front [Heppner,
1967], and Exp.12 located the magnetopause near the earth-sun line of the noon
meridian, which was consistently identified by the change in field direction,
and the change in angle, an indication that the field outside the boundary was
anti-parallel to the field inside [Heppner, 1967], while Wolfe and Mayers [1966], located maximum distance of magnetopause
in their Table.1 at 30.7RE, and they put the transition
region at 31.5RE, which forced one to question position of the
geomagnetic fields, or the magnetosphere boundary, does it extended to 30RE?
The average boundaries positions are probably
strongly determined by the interplanetary solar wind velocity, density, and
direction of flow, [Gosling et al., 1967], but it was found that, the
fluctuating part of geomagnetic field, between the shock wave and the
magnetosphere is not part of the geomagnetic field, but rather the compressed
and distorted interplanetary field [Spreiter
and Jones, 1963].
These
discrepancies lead Heppner et al. [1967], to question factors determining
magnetosphere boundaries? The nature of bow shocks multiple crossings? The
speedy movements of the bow shock, and variations in the field associated with
the shock, and to state that, “it is more complex than the internal
plasma pressure”, while Montgomery et al. [1970], questioned the
existence of several regions, and Bame et
al. [1980] questioned criteria that constitute judgment for the encounter
of the bow shock?
These
and many others, forced itself due to oddness of these boundaries, for example,
the fast crossing of total shock structure in less than 12 seconds, while 20
crosses took place in a single pass [Heppner et al., 1967], these
clearly shows that, the link between these boundaries are, spatial anomalies
magnetic field divided by empty space, where field directions are opposite on
both sides of the boundary, and these phenomena can exist from 4RE
[Cahill and Amazeein, 1963], to more than 241.40RE
as detected by ACE [Russell et al., 2000].
Hence
one can suggested that, what had been crossed is something different from solid
spatial fixed structure, therefore these fields boundaries suggests the
existence of variable intermittent production of spatial magnetic fields along
the geomagnetic lines of force.
4.0 Gyrating
Solar Wind
As
shown in Fig.1-B&C, and the above events explanations, it took the
energetic protons only 50 minutes to cross to magnetosphere peripheries from
Pioneer V, so why it took more than one hours for any sign of IMF to be
detected at Pioneer V? And 8 hours for IMF to reached maximum magnitude at
Pioneer V?
There
is a delay between the start of sudden commencement storm due to the existence
of bow shock, where great turbulence associated with unstable magnetic fields [Watermann et al., 2009], and solar wind
existed with varied speed and density [Montgomery et al., 1970], it is
where solar wind changes flow from supersonic to subsonic [Axford,
1962], this is thought due to reduction in particle’s velocity to gyrating
frequency, while there are increase in particle’s density and magnetic field
strength [Axford, 1962], which are due to
particle’s concentration while gyrating around the geomagnetic lines of force.
The
process of capturing solar wind, constitute part of the magnetic force, lead to
drop in particle speed as it experienced a large change in momentum, [Thomsen
et al., 1986], and since gyration was detected as gyrating ions
distributions observed between ~9 and ~83 RE from the shock,
which are characterized by gyromotion around the magnetic field [Meziane
et al., 2001], and gyrating protons in both quasi-perpendicular and
quasi-parallel geometries of backstreaming in the foreshock, and multiple
reflections along the shock, [Thomsen, 1985] or the gyrating ion
distributions, which may be gyrotropic, which
is a torus in velocity space whose symmetry axis is parallel to the magnetic
field [Thomsen, 1985], it is also commonly observed in association with
the magnetic foot and overshoot of quasi-perpendicular, supercritical shocks [Paschmann et al., 1982] and it was observed
by Wind spacecraft at distances larger than 20RE, and can be
found at more than 80 RE from the shock [Eastwood et al.,
2005], such existence allowed Anderson et al. [1985] to state that, gyrophase bunching is an inherent and fundamental property
of the bow shock for ions, and for Electron under certain conditions.
Therefore
solar wind and the streaming ions are thought to interact with the geomagnetic
lines of force before and at the bow shock spatial boundary, the resulted
interaction cause charged particles to gyrate around the geomagnetic lines of
force, producing magnetic force [Yousif, 2003] given by
Where, Bg
is the geomagnetic field in Tesla, Be/p is the
electron’s or proton’s circular magnetic field (CMF) [Yousif,
2003a] in Tesla, rm is the
magnetic radius in meter, c is speed of light, ϑ is factor
related to the capturing process, θ is
the angle between the two fields during the capturing process, q is the
elementary charge in Coulomb, vs
is the solar wind velocity when captured and the magnetic force Fm
is in Newton (N).
4.1
Production of Interplanetary External Magnetic
Field (I-ExMF)
The
exterior of geomagnetic field is typically 30 to 40γ, occasionally it
rises above 75γ, and seldom below 20γ, and fluctuations are seen from
10RE outwards to 14RE as measured by
Pioneer I [Cahill and Amazeein, 1963], and a
large fluctuations were observed in the magnetic field components between 9.5RE and 15.7RE
[Coleman et al., 1960a], and large fluctuations in solar wind flow speed
and flow direction occurred simultaneously with the solar wind ion density
fluctuation [Bame et al., 1980], and the
turbulent flow in the plasma cloud might cause regions of enhanced magnetic
field to exist [Bryant et al., 1962], related these to magnetic
fluctuation at comet Halley observed by both VEGA-1 and VEGA-2 spacecrafts,
which seems more turbulent than those in the undisturbed solar wind [Le et
al., 1991], and the total magnetic fields measured by ACE at 241.40RE
and Wind at 183.64RE, gives anomalous field of ~35γ
each, while Geotail at 20.22RE,
measured ~45γ an increase of 28%, and the Interball
which was at 11.46RE, in the magnetosheath measured total
field of ~56γ [Russell et al., 2000], and since all these large
anomalous fields lead many to state that magnetic fields should not be
neglected in theoretical treatments [Fairfield, 1976], therefore the
incoming solar plasma which carrying nearly equal parameters, if it is embedded
with solar magnetic field, then the fields should have measured higher
magnitudes solarward not downstream, thus the increase of 28% and 60% measured
by above Geotail and Interball
respectively, are of changeable parameter not like solar wind [Russell et al.,
2000], which gives impression that, the IMF is locally produced magnetic field,
rather than originated from the sun.
With
boundaries been interpreted merely as distances between intermittent local
spatial produced magnetic fields, and suggestion that solar wind gyrate around
the geomagnetic lines of force, as given by Eq.{1},
and gliding downstream along the guiding center [Kern, 1967]. And with
disregard to Gold [1959] abstract ideas on transportation of magnetic
field of solar origin with solar gas, regulation of ionized material in the
magnetosphere by insulating sheath, and instability of material on tube of
force, therefore the IMF is thought to be produced within, before and after the
area of the great turbulence interaction [Bame
et al., 1980] and fluctuated magnetic field, or the bow shock, [Mariani, 1965; Ness et al., 1964; Cahill
and Amazeein, 1963], therefore the captured solar
wind (electrons and protons) given by Eq.{1}, gyrates along the geomagnetic
lines of force, in clusters waves of electrons or protons, with above high
density concentrations, this would produced the above mentioned intermittent
magnetic fields, namely the Interplanetary-External Magnetic Field (I-ExMF),
it is produced in a manner different from known induction theory, as shown in
Fig.3-A, the magnetic fields are produced in a range of magnitudes, with angles
continually giving impression of either away from the sun or toward the sun, such as observed by IMP-1
satellite [Wilcox, 1966] or as shown in Figs.3&5, the produced I-ExMF
is such that, it opposed the initial geomagnetic field producing it, and in
line with Lenz’s Law, that “Produced I-ExMF is in such a direction
that it opposes the field that produced it.” [Trinklein, 1990]
The
ExMF idea was first mentioned by Kapitza,
who thought the production of intense magnetic field outside an atom, could
cause change in atoms characteristics [Kapitza,
1967], the I-ExMF which
is thought to represents the filamentary structure detected in the
interplanetary medium by IMP-1 [Ness et al., 1964], thus
the
intermittent boundaries shown in Fig.2, are local spatial produced I-ExMF,
and each produced I-ExMF may give diverse magnitudes,
proportional to number (or density) of the solar wind (electrons/protons) and
the length of gyrating particles along the geomagnetic lines of force as shown
in Fig.3-A.
If
number of electrons or protons in solar wind interacted with geomagnetic lines
of force along one meter is denoted by (nm), with field
intensity (Bg), therefore
produced I-ExMF
as
a result of interaction given by Eq.{1}, and shown in Fig.3&4, is given by
Where,
l is the effective length of the
magnetic lines of force, Be/p is circular magnetic
field (CMF) produced by electrons or protons, me/p is
electron’s or proton’s mass, vs is
velocity of the solar wind particles, and the produced Interplanetary External
Magnetic Field (BIEx) is in
Tesla.
4.2
Solar Wind Energization Process
The magnetopause was
identified by the rapid jumps and very large magnitudes of fields with abrupt
change of direction at 9.7RE [Ness et al., 1964], but
magnetopause position was later been identified by appearance or disappearance
of streaming protons that are determinate feature of the magnetosheath, and are
not generally observed inside the magnetosphere [Gosling et al., 1967]. These
energetic magnetosheath particles are accelerated and transmitted by the bow
shock [Katırcıoglu et al.,
2009], where energetic electrons expanded to 182 keV
[Sibeck et al., 2002], and these
energetic particles are found to be a general feature related to anomalous
produced magnetic fields [Fredricks et al.,
1970].
Thus
it was also found that, the increase in electrons density, lead
to an increased in magnetic field magnitude, thus increasing electron’s
energy. [Neugebauer
et al., 1971], and that, ions heating, occur behind the magnetic
structure [Morse and Greenstadt,
1976].
Therefore
particles acceleration in nature is thought to be carried out in the follows
sequence:
Electrons
and/or protons high density = (or synonymous to)
gyrating around magnetic lines of force → anomalous magnetic
field = (or synonymous to) production of I-ExMF → accelerated
particle = (or synonymous to) energization of particles.
As
this process is what is consistently been found, Paschmann
et al. [1988]; Neugebauer et al., [1971];
Morse and Greenstadt, [1976], that the energization
process, taking place during I-ExMF production, is related to
electrons/protons density, therefore any detected momentary increase in solar
wind density in the interplanetary space means a capturing gyrating process as
given by Eq.{1}, that could lead to production of the I-ExMF given
by Eq.{2}, hence both of these leading to the energization of the solar wind,
therefore energy given at step i by Ki
is given by [Yousif, 2004]
Where, γPS is the relative magnitudes of both the P
& S-ExMF
in production of ExMF
[Yousif, 2004], and K is the energy gained by a particle.
If BIEx
given by Eq.{2} continuously increasing, then energy built up gained by charged
particles given in Eq.{3} may be approximately computed as measured [Yousif,
2004]
Where, K1, K2
… Kn are
energization executed, ε = εi where εi is the error of
continuity approximation at step i, KT is the total approximate
energy acquired or gained by the charged particle in Joules.
5.0
The Sudden Commencement Magnetic Storm-First
Approach
Magnetosheath
streaming protons, [Gosling et al., 1967], were similar to the one which
engulfed Pioneer V on March 31, 1960 [Fan et al., 1960a], and later
ignited the sudden commencement detected at Honolulu and Pioneer V [Coleman
et al., 1961].
Vela
2A was on the magnetosphere side and close to the boundary, when it recorded
movements of such protons on June 9, 1965 then an IMF starts increases at 04:40
U.T. (to be linked with IMF increase at Pioneer V), then streaming protons
fluxes appeared at 04:55 U.T., causing changes in earth’s field [Gosling et
al., 1967], another Sudden Commencement (SC) storm occurred on March 12,
1965; at the impulse, Vela 2A was within the magnetosheath and close to the
average position of the magnetopause, when great influx of protons were
detected, simultaneously with an increase in the horizontal component of the
field at Guam station [Gosling et al., 1967].
The
persist existence of energetic protons at magnetosheath boundary with
magnetopause, prior to the start of the SC and the start of magnetic changes on
magnetopause and earth surface, as demonstrated by above examples, was also
recorded by IMP-1 where, immediately after the geomagnetic sudden commencement
storm at 21:14 U.T., on December 2, 1963, a clear unique event was observed to
occur in the interplanetary magnetic field data three minutes before the
terrestrial magnetic field event [Ness
et al., 1964], such strong relation between the geomagnetic storms and
protons streaming into magnetosheath, also exhibited by the large ion flux
during January 31, 1964 geomagnetic storm, which occurred when IMP-1 was in
inbound to 15.7RE, and it detects flux with large
fluctuations in both flux and direction of incidence, [Wolfe and Mayers, 1966], and since the daily variation of sudden impulses (si) at Honolulu seems to be diurnal, with maximum
around noon and minimum around midnight [Nishida and Cahill, 1964], this
means the si or the initial positive phase (Dst > 0) is related to solar wind activities blowing from the sun, as proposed [Akasofu and Chapman, 1963], but how
variations in the solar wind produce the variations in the magnetic field
measured on Earth as Gannon [2012] asked?
The relative magnitudes of si’s at various observing points, showed that large
magnitude three times greater than that of Honolulu, was obtained around a
radial distance at 12.46RE [Nishida and Cahill, 1964],
which could be inferred as at/or near to the source of the magnetic field
production, and that region (12.46RE) is the region of high
turbulence in the magnetic field, which separates the magnetopause from the
shock wave [Ness et al., 1964], it is where accelerated solar wind are
transmitted by the bow shock [Katırcıoglu
et al., 2009], and since the position of the bounding surface of the
magnetosheath is often inaccurate [Wolfe and Mayers,
1966], and the magnetosheath region was detected at various radial distances,
among them at 15.2 RE, 15.7RE, 16.4 RE,
while the cutoff was detected at 11.3RE [Wolfe and Mayers, 1966], therefore the cutoff could move up to or
bellow, hence the central radial distance of the magnetosheath is thought to be
nearly at 12.5 RE, near si above
region.
Observations
due to Pioneer V failure to detect embedded solar magnetic fields with the
incoming plasma, on March 31, 1960, and with Parker theory strong momentum
[Parker, 1959], force Fan et al. [1960a] to state that “magnetic
fields are either being moved from the sun or generated in the interplanetary
space“, therefore reviewing that failure and the nearly concurrent
detection of IMF by both Honolulu station and two hours later by Pioneer V [Fan
et al., 1960a], which cast great doubt about the solar origin of the IMF,
and with the detection of such as high density magnetosheath solar wind positive
ion density ranging between 35 to 127 cm3 [Gosling et al.,
1967], in contrary to background proton’s solar wind density of 5-10 cm3
[Watermann et al., 2009], such ions
concentration is the main sequence towards achieving - gyration+ I-ExMF +
Energization - process, Paschmann et al.
[1988]; Neugebauer et al., [1971]; Morse
and Greenstadt, [1976], and as Fan et al.
[1960a] stated in regards to origin of Pioneer V measured IMF that, “solar
plasma either carries magnetic fields, or manipulate an interplanetary magnetic
field”, hence as given by Eq.{2}, I-ExMF is produced along
the geomagnetic lines of force by such solar wind concentration; therefore, as
energetic particles accelerated from bow shock towards the magnetosheath, with
gyrating radius due to balance of force given by Eq.{1} with centripetal force
(Bev=mv2/r), thus the magnetic radius become smaller with an
increased in I-ExMF magnitude, given by Eq.{2}, therefore the magnetic
radius is given by
Where,
rm is the magnetic radius, and with
such reduction in radius, and since each geomagnetic storms depends on specific
solar wind that drive them [Gannon, 2012], therefore that state starts
with the production of an intense Interplanetary External Magnetic Field (II-ExMF)
[Yousif, 2004] in the magnetosheath, centered at 12.5RE,
as demonstrated in Figs.3, it is given by
Where, 108 is the relative number of
geomagnetic lines of force in square meter [Yousif, 2003b], γPS is the relative magnitudes of both
produced primary and secondary ExMF (P & S-ExMF),
nm is gyrating number of electrons/protons in volume
of geomagnetic lines of force, l is
the effective length of the magnetic lines of force around which charged
particles gyrates, Bgx is
the previous field intensity, and the produced intense II-ExMF (BIEx) is in Tesla.
5.1
Magnetic Storms and Lion Roars
There
is an intense, sporadic bursts of narrow-band magnetic noise in the earth's
magnetosheath with frequencies near 100 Hz [Smith et al., 1969], with the
Pioneer V measurements during solar activity, Coleman et al. [1960a]
concluded that a collisionless magnetoacoustic waves may be formed in the
interplanetary medium, the burst was detected and found to be a persisted
feature of the magnetosheath [Smith et al., 1967] the signals which is
intense was found to occupy narrow band centered between 100 and 300 Hz
[Smith et al., 1969], when the recorded signal played in a loudspeaker,
the low frequency burst sounded like a roaring lion [Smith and Tsurutani, 1976]. The wave is circularly polarized in a
counterclockwise sense; or the sense where electrons gyrate around the magnetic
field, and found to propagate along the magnetic field [Smith and Tsurutani, 1976], these waves are thought to represents
the gyrating ions which are often associated with low frequency MHD, the center
of which rotates around the ambient magnetic field [Paschmann,
et al., 1979; Meziane et al.,
2001].
A
strong correlation has been found between the probability of lion roars
occurrence and geomagnetic activity [Smith and Tsurutani,
1976], and the level of that activity as measured by KP, and
the probability of occurrence ranges from 10% in magnetically quiet intervals
to 75% during disturbed periods [Smith and Tsurutani,
1976].
But
the observed frequencies of lion roars were found to exist roughly midway
between proton and electron gyrofrequencies [Smith et al., 1969], which
suggest the phenomenon to represents the production of magnetic waves by both
electrons and protons, therefore gyrating charged particles (electrons and
protons), which produced II-ExMF at 12.5RE in
the magnetosheath region, accelerated by the Lorentz force given by Eq.{1}, the
force increased with the produced II-ExMF or BIIEx
given by Eq.{6}, with smaller radius given by Eq.{5}, therefore the
acceleration would creates radiation, and since the II-ExMF is relatively
intense, the produced wave is at low frequency, this frequency is given by [Turku,
2006]
Where,
the cyclotron frequency fc is in
hertz, and proportional to the magnitude of intense II-ExMF.
5.2
The Sudden Commencement & Main Phase-First
Approach
The
occurrence of the interplanetary magnetic field (IMF) data three minutes before
the terrestrial magnetic field event [Ness et al., 1964], with field
events occurred after sudden ion flux, such as that of December 2, 1963, at
21:14 U.T., which started approximately three minutes with a sudden
impulse-type magnetic storm observed worldwide [Wolfe and Mayers, 1966], or the proton flux of March 12, 1965,
detected by Vela 2A while within the magnetosheath and close to magnetopause [Gosling
et al., 1967], and that the sudden flux enhancement of magnetosheath coincided
with the onset of the storm [Nishida and Cahill, 1964], therefore these
events were similar to the solar protons which engulfed pioneer V on March 31,
1960, then caused geomagnetic storm six hours later, detected at Honolulu
station and two hours later by Pioneer 5 [Fan et al., 1960a] and since
magnetosheath boundary at 15.7RE, revealed extremely chaotic
plasma flow characterized by high temperatures (broad energy spectra) and
variability in the direction of incidence and flux amplitude [Wolfe and Mayers, 1966], and that shortly before the terrestrial
observations of the sudden commencement, the field decreased very rapidly and
varied somewhat for several hours, eventually returning to a configuration
similar to that before the storm [Ness et al., 1964], the sequence of
which explained in Fig.3-B&C and also to be related to Fig.1, and since the
center of the magnetic storm is estimated to occur within the magnetosheath at 12.5RE,
from the earth’s center, that point is the center for intense II-ExMF
production as given by Eq.{6}.
In
Fig.4, the whole of Dst shape including the SC, the
main phase (MP) to the recovery phase (RP); is interwoven with low frequency
pulses, each cycle is designated by arrows, but as explained, the source of
magnetic disturbances at the magnetosheath, is where great turbulence in
magnetic field exists [Ness et al., 1964], where there are two types of
waves [Smith et al., 1969], having frequencies ranges from 3 to 300 Hz [Smith et al., 1967], with amplitude
magnitude between 40 and 160mγ [Smith and Tsurutani,
1976] in addition to high amplitudes it do have low durations [Smith et al.,
1969]. As the region is suggested to produced intense II-ExMF
given by Eq.{6}, it is such field thought to be measured
at Honolulu and two hours later at Pioneer V [Fan et al., 1960a]. As
shown in Fig.1, there was second IMF on April 1, 1960 due to the second flare, the
IMF measured 53γ at Pioneer V [Coleman et al., 1960a], and since the
difference in propagation time between Honolulu and Pioneer V to attain IMF
peak magnitudes is two hours as measured in Fig.1-A&B for the first flare
of 31 March, therefore tracing a two hours on the left side of IMF maximum of 53γ
on second IMF of April 1st, will bring the line to the main phase of
Honolulu Dst at point x, with field measurement of
91γ.
Given
Honolulu first magnetic disturbance = 11.6γ, Pioneer V first IMF =
23γ, and Pioneer second IMF = 53γ, and since both data are perceived
to be produced from one source, therefore from these data, the magnitude of the
second Honolulu SC caused by the second magnetic disturbance is given by the
following ratio
Where,
BP1 is Pioneer V first IMF on 31 March, BP2
is Pioneer second IMF on April 1, BH1 is Honolulu first magnetic
disturbance of 31 March, and BH2 is Honolulu supposed
magnitude related to the second magnetic disturbance two hours before the peak
measured at Pioneer V as shown in Fig.1-A & B by the dashed green lines,
the magnitude of the second magnetic disturbance at Honolulu, coincided with
the main phase (MP) of the first magnetic disturbance, thus the impact of the second
26γ is that it changed the recovery phase and formed a strange peak shown
in Fig.1-A as point-x, therefore the net resultant of SC on the MP is the
reduction of the negative magnitude of the MP; that performance, in addition to
the strong relations between occurrence of Lion roars and geomagnetic activity
as measured by KP [Smith and Tsurutani,
1976], with the initial positive phase (Dst > 0) attributed to the impact of a solar
stream on the earth’s magnetic field [Akasofu
and Chapman, 1963], and the sudden commencements are associated with enhancements
of solar wind and the Z component of the IMF with geomagnetic activity [Burton
et al., 1975]. With SC rise time range from 1 to 10 minutes [Curto et al., 2007], and since Pioneer I,
waves were found to be generated between 12 to 15 earth radii; with a lifetimes
of 2 to 5 cycles and periods of 10 seconds [SONETT et al., 1959], and
the Lion roars occurs at nearly the same place, every few seconds for intervals
of minutes to hours [Smith and Tsurutani,
1976], with amplitudes ranging between 40 and 160 mγ.
[Smith and Tsurutani, 1976], while that of DCF does not exceed 70γ during very intense
storm [Akasofu and Chapman, 1963], and with
prominent correlation between lion roars occurrence and decreases in magnetic
field magnitude at magnetosheath, and that all lion roars are accompanied by
decreases in magnetic field, and vice versa, for intervals of tens of minutes [Smith
and Tsurutani, 1976] and the magnetosheath field having
frequencies variations below 1 hz have been reported
extensively, with variable intensity [Smith et al., 1967], and since in
most cases, a negative impulse is superposed on the MI of SC, the period of the
negative impulse differ in each event, and the occurrence of the negative
impulse does not seem to be dependent on geomagnetic activity [Tsunomura, 1998], and the contribution from the
external source of the sudden impulses (si) is
estimated to reach 2/3 of the total magnitude [Nishida and Cahill,
1964], which is thought due to II-ExMF as given by Eq.{6}.
Therefore
it is suggested that, the starts of first frequency of Lion roars given by
Eq.{7} together with II-ExMF magnitude given by Eq.{6}, initiate
the SC of the Dst as shown in Fig.4, and in reaction
to II-ExMF production, the geomagnetic field will opposed such
production, in accordance with Lenz’s law, hence the start of the main phase, therefore
producing a shaped interwoven with low frequency magnetic wave as shown in
Fig.4, therefore such magnetic disturbance can be expressed as follows
Where,
Bg is the geomagnetic field,
BIIEx is
the I-ExMF, fd is
Lion roars frequency, n is the number, and Dst
or the SC-II-ExMF is the magnitude of the magnetic disturbance in
Tesla.
The change given by Eq.{9}, explained the
correlation between changes in the magnetic field magnitude,
direction and the occurrence of lion roars as observed above, where the lion
roars starts when the field magnitude decreases and end as the magnitude
recovers [Smith and Tsurutani, 1976], and
since II-ExMF production is carried out by periodic intermittent
waves of solar winds, this cause intermittent start and decrease of both the
lion roars and the geomagnetic field, all of which occurs during small period
of time, hence explained why the lion roars can occurs
every few seconds for intervals of minutes to hours [Smith and Tsurutani, 1976], and since the streaming protons could
produce both the waves and the field decreases and all three occurs at the same
time [Smith and Tsurutani, 1976], this
understandable since the streaming protons produced the II-ExMF
given by Ex{6}, the later in turn produced Lion roars as given by Eq.{7}, and
both the lion roars and the II-ExMF caused geomagnetic storms and
drop in geomagnetic field given by E.{9}, as a result of that decreases the II-ExMF
ceased and Lion roars stops.
Since the solar protons were arriving before and after
the sudden commencement on March 31, 1960 [Coleman et al., 1961],
therefore the sudden intense production of the SC-II-ExMF given
by Eq.{7} is thought to represents the final resultant of accumulated mechanism
lasted four hours (deduced from Fig.1) during the gyration process that finally
produced the SC-II-ExMF.
No |
1 |
2 |
3 |
4 |
5 |
6 |
7 |
8 |
9 |
10 |
11 |
12 |
13 |
14 |
15 |
16 |
17 |
18 |
19 |
name |
1/1-1 |
1/1-2 |
1/1-3 |
1/2-1 |
1/2-2 |
1/2-3 |
1/3-1 |
1/3-2 |
1/3-3 |
1/4-1 |
1/4-2 |
1/5-1 |
1/5-2 |
1/6-1 |
1/6-2 |
1/7-1 |
1/7-2 |
1/8-1 |
1/8-2 |
polarity |
+ |
+ |
+ |
o |
o |
o |
o |
o |
- |
- |
o |
- |
- |
- |
- |
- |
o |
- |
o |
Measured I-ExMF |
2.2γ |
2.2
γ |
2.4
γ |
4.0
γ |
4.2
γ |
4.2
γ |
4.6
γ |
4.8
γ |
5.8
γ |
5.85
γ |
5.85
γ |
6.1
γ |
6.1
γ |
6.1
γ |
6.1
γ |
6.5
γ |
6.5
γ |
6.5
γ |
6.7
γ |
Table.2.
Data of the first sector, measured by IMP-1 during the first orbit, as given by
Wilcox and Ness, 1965]. These data are used in Fig.6, to show
readings along the yellow and green colors orbit.
5.3 Geomagnetic
Storm Propagation “Pioneer V Events”
As
shown in Fig.1-A-B&C, the SC-II-ExMF recorded maximum
magnitude at Honolulu station before Pioneer V, this due to short distance between
SC-II-ExMF source of production and Honolulu station, thus as the
SC-II-ExMF spreads at the same time along the geomagnetic lines
of force in both directions, hence the time T1 travelled by SC-II-ExMF,
first arrived at Honolulu station, while the same field/time arrived at an
equivalent distance d=x in the opposite direction towards Pioneer V, as
shown in Fig.3-C. But the time for sudden increase in magnetic field at
Honolulu due to SC-II-ExMF production and the start of SC as
given by Eq.{9}, is to be related to detection of the
field after three minutes in later related events [Ness et al., 1964];
therefore the speed at which change in magnetic field propagates towards Honolulu
station is given by
Where,
dxH is the radial distance from the
spatial point at which SC-II-ExMF is produced (12.5RE)
in meters to Honolulu, txH is time
travel by SC-II-ExMF (to reach earth station) in seconds, and the
SC-II-ExMF velocity VSC is in Tesla.
Since
the known propagation velocity of 700 km sec-1 was measured due to
magnetic disturbances on December 2, 1963, by Ness et al. [1964], while
the probe seems to be at 19.7RE, therefore the magnetic
disturbances, or the produced Dst moves towards
Honolulu and Pioneer V at the same time as shown in Fig.3-c, and the suggested Dst production point is at 12.5RE, from
Honolulu, therefore with VSC = 700,000 ms-1, the
time to reach Honolulu is = 114 s equivalent to t = 1:54 minutes.
As
the same SC-II-ExMF was also moving towards Pioneer V (dPE) in opposite direction, at a distance of 5.2x109
meters from earth [Fan et al., 1960a], therefore the distance from
Pioneer V to the SC-II-ExMF spatial production point (x) is given
by
Where,
dPE is the radial distance from Pioneer
V to earth in meters, and dxH is
the distance from SC-II-ExMF production point to earth’s
(Honolulu), and the distance from Pioneer V to SC-II-ExMF production
point dPx at 12.5RE
in meters.
Since
dPE = 5.2 x 106 km [Fan
et al., 1960a], therefore the time for the SC-II-ExMF to
propagate to Pioneer V is given by
From
Ex.{12}, the time required for the produced SC-II-ExMF to
propagate to Pioneer V is 2:03 hours when dPE
= 5.2 x 106 km [Fan et al., 1960a], referring to Fig.1, this
is the difference in time between disturbances arrival to Honolulu and to
Pioneer V, which is 2:00, therefore all parameters are correct, including SC-II-ExMF
production point, and the field which is coming from 12.46RE
in magnetosheath, and larger three times in magnitude than registered si at Honolulu [Nishida and Cahill, 1964].
6.0 What
Is the Sector Structure?
As Exp. 18 was sent to investigate the magnitude, direction, and temporal variations of the
interplanetary magnetic field (IMF), [Ness et al., 1964], the
results were analyzed based on Pioneer V interpretations [Fan et al., 1960a], and the origin of
measured anomalies interplanetary magnetic field was settled to emerged from
the sun and embedded with the plasma, in accordance to Parker theory [Parker,
1959].
But one of the most
complicated interpretations emerged during IMP-1 experiment which lasted three solar rotations of the quiet sun, was the observation of a quasi-stationary corotating structure in the
interplanetary medium [Wilcox and Ness, 1965], the sector structure
consists of seven sectors, divided into four, according to fields direction (+)
to /or (-) from the sun, they are (+2/7) (-1/7) (+2/7) and (-2/7), these
sectors were thought to originate from the sun [Wilcox and Ness, 1965],
and the observed direction of the interplanetary field is on the average was
thought in consistent with the Archimedean spiral picture predicted by Parker
[1958], but the negative and positive sense of the field changes from time to
time [Wilcox and Ness, 1965].
As attention had been drowned to the failure of Pioneer V to detect
embedded solar magnetic field with the solar plasma, and the detection of IMF
eight hours later, both of them were overlooked, and instead solar magnetic
field was chosen as the origin of the IMF due to lack of alternative theory [Fan
et al., 1960a], and distortion from I-ExMF by other planet on 1 December 1963, is excluded
according to that day Orrery [The Orrery,
2013] therefore these
sectors are to be analyzed in accordance with the suggested alternative I-ExMF;
but before that, the main I-ExMF characteristics are to be draw
into attention to help in the analysis of IMP-1 measurements, these characteristics
are:
a- Charged
particles gyrate along the geomagnetic lines of force to produce the
Interplanetary External Magnetic Field (I-ExMF).
b- Many
lines of force will be covered by gyrating charged particles.
c- Line/or
lines of force may have lengthy or intermittent charged particles.
d- Line/or
lines of force may produced intermittent I-ExMF.
e- The
direction of produced I-ExMF is opposite to the geomagnetic field.
f- Each
intermittent produced I-ExMF polarity is opposite to the adjacent
one.
g- Magnitudes
of produced I-ExMF varied from intermittent group to another.
6.1 Spatial Measurements of
I-ExMF
The average magnitude of the IMF within each of the seven sectors was given
in Fig.7 by Wilcox and Ness [1965], the first sector which
represents measurements carried out during IMP-1 first orbit [Wilcox and Ness, 1965], is given in Table.2.
The time required for the 1/7 sector given in table.2, to
rotate past the earth is almost equal to one orbital period of the satellite [Wilcox and Ness, 1965], which is 93.05
hours or 3.9 days [Car, 1966, Ness et al., 1963], and the
interplanetary measurements cannot be made during perigee passes; when IMP-1
within geomagnetic field which is one day [Wilcox and Ness, 1965], therefore
the spatial interplanetary boundary that adjacent to the magnetosphere, where
the I-ExMF is produced, is shown in Fig.5, while the spatial
positions where IMP-1 first orbit, is shown in Fig.6, this is the spatial space
where the I-ExMF could be produced based on Eq.{2}, it is covered
by intermittent strips of yellow and green colors.
As shown in Fig.6, the radial distance of measurements in the interplanetary
space was the satellite apogee which was 30.7 RE [Car,
1966, Ness et al., 1963], starting from around 5RE, most
of the space is covered with solar wind, protons in this case because energetic
protons of MeV were detected by IMP-1, during the three
solar rotations, [Wilcox and Ness, 1965], although it can consist of
electrons or mixture of both.
Each cluster of protons gyrate around the geomagnetic lines
of force producing the I-ExMF; the polarity of which is opposite
to adjacent one and to that of the geomagnetic field, as shown in Figs.3,5&6,
hence fields’ polarities between adjacent produced I-ExMF could
cause confusion. The magnitudes of produced I-ExMF varies with
particle’s density and cluster length according to Eq.{2}, hence with sudden
shift from one proton’s cluster to adjacent with less proton’s density, the
magnitude is reduced, and the field sense of direction, away or toward the sun
[Wilcox and Ness, 1965] could means a movement from one cluster to
another as could be deduce from Fig.6, therefore these represents reversal of
field direction, with an abrupt decreased of field magnitude to zero when
moving from cluster to another, which represents the null point [Ness et al.,
1964], as measured by satellites, and shown in Fig.6 and Fig.3-A.
Given these, and as shown in Fig.6, IMP-1 measurements during the first
orbit started after 5RE, while the satellite moves across and
through clusters of gyrating protons at various angles, while detecting charged
particles [Wolfe and Mayers, 1966], and
since the sector boundary is the
position at which the sense of direction of the interplanetary magnetic field
changes [Wilcox and Ness, 1965], whereas proton’s clusters produced
intermittent I-ExMF which has space between them, hence that is
what are perceived as boundaries according to above definition, and since solar
wind plasma is thought to be organized by sector structure [Wilcox and Ness, 1965],
and as given by Eq.{2}, the I-ExMF production is also
proportional to solar wind density, therefore measurements of magnitudes,
density, polarities and angles of I-ExMF by IMP-1, at positions
designated by green and yellow colors, within the IMP-1 first orbit shown in
Fig.6, or what had been perceived as quasi-stationary corotating structure in
the interplanetary medium [Wilcox and Ness, 1965], is merely
measurements of magnitudes, polarities and angles of local spatial produced I-ExMF.
Such I-ExMF production in magnetosphere peripheries is
also shown in Fig.5, which had been perceived as sector structure [Smith
and Tsurutani 1978].
7.0 Conclusion
The
paper generates many questions, which with little efforts can be resolved, such
as:
-
Re-confirmation
of Pioneer V engulfment with solar plasma, which could be replicated with three
satellites, one at 5x106 km, the second at 17RE and the third at 12.5RE,
to confirm or dispute the first results.
-
How the earth’s
dynamo system compensate the drop given by Eq.{9}?
Acknowledgement
Gratitude to my son Mustafa for waiting
these periods, and friends who helped reduce pains of past
two years while surviving, Mr. John Ongay Kassiba, Ramadan Nimir,
Bona Thiang, Ramadan Omba, Yagoub Adam Sad-Alnur, Ali Abdulrhman, Awutu Aluiuda Ndeke, Rashid James, John
Nassar, Elsafi Noraldin Ibrahim, Boshara Suliman Alnor and
the American Geophysical Union (AGU) for references used.
8.0
Reference
Akasofu, S. I. and
S. Chapman, The Development of the Main Phase of Magnetic Storms, JOURNAL OF
GEOPHYSICAL RESEARCH VoL. 68, No. 1 JANIJARY1,1963.
Alfvén, H., Existence
of electromagnetic-hydrodynamic wave, Nature, 150, 405–406, doi:10.1038/150405d0, 1942a.
Alfvén, H., On the existence of electromagnetic-hydrodynamic waves, Ark.
Mat. Astron. Fys., 29B(2),
1–7, 1942b.
Alfvén, H. A., Hydromagnetics of the magnetosphere, Space Sci. Rev.,
2, 862-870, 1963.
ANDERSON, K. A., R. P. LIN, C. GURGIOL, G. K. PARKS,
D. W. POTTER, S. WERDEN, AND HEME, A Component of Nongyrotropic
(Phase-Bunched) Electron, JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 90, NO. All,
PAGES 10,809-10,814, 1985.
Angelopoulos, V., D. Sibeck,
C.W. Carlson, J.P. McFadden, D. Larson, R.P. Lin, J.W. Bonnell,
F.S. Mozer, R. Ergun, C. Cully, K.H. Glassmeier, U. Auster, A. Roux,
O. LeContel, S. Frey, T. Phan,
S. Mende, H. Frey, E. Donovan, C.T. Russell, R. Strangeway, J. Liu, I. Mann, J. Rae, J. Raeder, X. Li, W.
Liu, H.J. Singer, V.A. Sergeev, S. Apatenkov, G. Parks, M. Fillingim,
J. Sigwarth, First Results from the THEMIS Mission, Space
Sci Rev (2008) 141: 453–476 DOI
10.1007/s11214-008-9378-4, Springer Science+Business Media
B.V., 2008.
Arnoldy, R. L., R. A.
Hoffman, and J. R. Winckler, Solar cosmic rays and
soft radiation observed at 5,000,000 kilometers from earth, J. Geophys. Research, 65, 3004-3007, 1960.
Axford, W. I., The
Interaction Between the Solar Wind and the Earth’s
Magnetosphere, J. Geophys. Res., 67, No. A10,
3791, 1962.
Bame,
S. J., J. R. Asbridge, W. C. Feldman, J. T. Gosling,
G. Paschmann, and N. Sckopke,
Deceleration of the solar wind upstream from the earth's bow shock and the
origin of diffuse upstream ions, J. Geophys. Res., 85, 2981, 1980.
Beard, D. B., The Solar Wind Geomagnetic Field
Boundary, Rev. Geophys., 2, No. 2, 335, 1964.
Bryant, D. A., T. L. Cline, U. D. Desai, and F. B.
McDonald, Explorer 12 observations of solar cosmic rays and energetic storm
particles after the solar flare of September 28, 1961, J. Geophys. Res.,
67, 4983, 1962.
Burlaga, L. F., and K. W. Ogilvie, Observations of
the magnetosheath-solar wind boundary, J. Geophys.
Res., 75, 6167, 1968.
Burlaga, L. F., L. Klein, N. R. Sheeley
Jr., D. J. Michels, R. A. Howard, M. J. Koomen, R. Schwenn, and H. Rosenbauer , A
magnetic cloud and a coronal mass ejection, Geophys.
Res. Lett., 9(12), 1317–1320, doi:10.1029/GL009i012p01317, 1982.
Burlaga, L. F., N. F. Ness, Y. M. Wang, and N. R. Sheeley Jr. , Heliospheric magnetic field
strength out to 66 AU: Voyager 1, 1978–1996, J. Geophys.
Res., 103(A10), 23,727–23,732, doi:10.1029/98JA01433,1998.
Burton, R. K., R. L. Mcpherron,
and C. T. Russell, An Empirical Relationship Between Interplanetary Conditions
and Dst, Vol. 80, No. 31, Journal of
Geophysical Research, November 1, 1975.
Cahill, L. J., and P. G. Amazeein, The boundary of the geomagnetic field, J. Geophys. Res., 63, 1835-1854,
1963.
Car, Frank A., Flight Report Interplanetary
Monitoring Platform Imp-I-Explorer Xviii, N a t i
o n a l Aeronautics And Space
Administration Washington, D. C. April 1966.
Carter, Brandon ANTHROPIC PRINCIPLE IN COSMOLOGY, arXiv:gr-qc/0606117vl 27 June 2006
COLEMAN, P. J., JR., C. P. SONETT. D. L. JUDGE, AND
E. J. SMITH, Some preliminary results of the Pioneer-5 magnetometer experiment,
JOURNAL OF GEOPHYSICAL RESEARCH, VOLUME 65, NO.
6 JUNE 1960a.
Coleman, P. J., Jr., L. Davis, and C. P. Sonett, Steady Component of the Interplanetary Magnetic
Field: Pioneer V, Physical Review Letters, Vol. 5, pp. 43-46, July 15,
1960b.
INTERNATIONAL
GEOPHYSICAL YEAR WORLD DATA CENTER A IGY WORLD DATA CENTER A, CORPUSCULAR
RADIATION, MAGNETIC FIELD, AND MICROMETEORITE OBSERVATIONS WITH SATELLITES AND
SPACE PROBES, Rockets and Satellites, National Academy of Science, No. 14, July
1961.
Coleman, P. J., Jr., C. P. Sonett,
and L. Davis Jr., On the interplanetary magnetic storm: Pioneer V, J.
Geophys. Res., 66(7), 2043–2046, doi:10.1029/JZ066i007p02043, 1961.
Curto, J. J., T.
Araki, and L. F. Alberca, Evolution of the concept of
Sudden Storm Commencements and their operative identification, RESEARCH NEWS
Earth Planets Space, 59, i–xii, 2007.
Dungey, J.W.,
Interplanetary magnetic field and the auroral zones, Phys. Rev. Letters, 6, 47-48, 1961.
Dungey, J. W, THE INTERPLANETARY MAGNETIC
FIELD AND THE AURORAL
ZONES, University Park,
Pennsylvania, March 15, 1962.
Dungey, J. W.: 1963,
in C. DeWitt, J. Hieblot, and A. Lebeau
(eds.), The Earth's Environment, Gordon and Breach, New York.
Dungey, J. W, (A Model
With an Interplanetary Magnetic Field), Physics of Geomagnetic Phenomena, Vol.II,
Edt. By S. Matsushita and Wallace H. Campbell, Academic
Press, New York, 1967.
Eastwood, J. P., E. A. Lucek,
C. Mazelle, K. Meziane, Y.
Narita, J. Pickett, and R. Treumann, The foreshock, Space
Sci. Rev., 118 , 41– 94, 2005.
Fairfield, D. H., A SUMMARY OF OBSERVATIONS OF THE
EARTH'S BOW SHOCK, Physics of Solar Planetary Environments: Proceedings of the
International Symposium on Solar-Terrestrial Physics, Boulder, Colorado, Volume
II Vol. 8, 1976.
Fälthammar, Carl-Gunne, The scientific legacy of Hannes
Alfvén, Article first published online: 18 MAY 2012,
Eos, Transactions American Geophysical Union, Volume 93, Issue
21, pages 201–202, 22 May 2012.
Fan, C. Y., P. Meyer, and J. A. Simpson, Rapid
reduction of cosmic radiation intensity measured in interplanetary space, Phys.
Rev. Letters, 5, 269, 1960a.
FAN C. Y., P. MEYER, and J. A. SIMPSON, Preliminary
Results from the Space Probe Pioneer V, JOURNAL OF GEOPHYSICAL RESEARCH VOLUME
65. No. 6, 1960b.
Fredricks, R. W., G. M
Crook, C. F. KenneI, l. M, .Green,
F. L. Scarf, P. J. Coleman and C. T. Russell: OGO 5 Observations of
electrostatic turbulence in bow shock magnetic structures. J. Geophys. Res.
75, 3751-3768, 1970.
Gannon, J.L., Superposed epoch analysis and storm statistics
from 25 years of the global geomagnetic disturbance index, USGS-Dst: U.S. Geological Survey Open-File Report 2012–1167, 15
p. 2012.
Gold, T., Plasma and Magnetic
Fields in the Solar System, J. Geophys. Res., Vo. 64, No. A11, 1665, 1959.
Gosling, J. T., J. R. Asbridge,
S. J. Bame, and I. B. Strong, Vela 2 measurements of
the magnetopause and bow shock positions, J. Geophys.
Res., 72, 101, 1967.
Heppner, J. P., (Satellite and Rocket Observations) Physics of Geomagnetic Phenomena, Vol.II, Edt.
By S. Matsushita and Wallace H. Campbell, Academic Press, New York,
1967.
Heppner, J. P., N. F. Ness, C. S. Scearce, and T. L. Skillman (1963), Explorer 10
magnetic field measurements, J. Geophys. Res., 68(1), 1–46, 1963.
Heppner, J. P., M. Sugiura, T. L. Skillman, B. G. Ledley,
and M. Campbell, Ogo A Magnetic field observations, J.
Geophys. Res. 72, 5417-5471, 1967.
Kapitza, P., Collected Papers of
P. Kapitza (The Production of and Experiments in
Strong Magnetic Field), Edited by D. Ter Hear, Pergamon Press, Oxford, 1967.
Karpen, Judith T.,
Spiro K. Antiochos, C. Richard Devore, and Leon Golub, Dynamic Responses To Magnetic Reconnection In Solar
Arcades, The Astrophysical Journal, 495:491È501, 1998 .
Katırcıoglu, F. T., Z.
Kaymaz1, D. G. Sibeck, and I. Dandouras,
Magnetosheath cavities: case studies using Cluster observations, Ann. Geophys., 27, 3765–3780, 2009
Kern, John W., (Magnetosphere and Radiation Belts), Physics of Geomagnetic Phenomena, Vol.II,
Edt. By S. Matsushita and
Wallace H. Campbell, Academic Press, New York, 1967.
Le, G. and C. T. Russell, THE MAGNETIC FIELD
TURBULANCE AT COMET HALLEY OBSERVED BY VEGA 1 AND 2, Cometary
Plasma Processes, Geophysical Monograph 61, American Geophysical
Union, 1991.
Mariani, F., Results on
magnetic field inside and outside the magnetosphere, Lecture given at ESTEC (European
Space Technology Centre) in Noordwijk 011 December
17th, 1965.
McComas, D. J., H. O. Funsten, S. A. Fuselier, W. S.
Lewis, E. Möbius, and N. A. Schwadron,
IBEX observations of heliospheric energetic neutral atoms: Current
understanding and future directions, GEOPHYSICAL RESEARCH LETTERS, VOL.
38, L18101, 9 PP., 2011.
McDonald, Richard, Planetary Magnetic Fields,
themcdonalds.net, 2005. http://www.themcdonalds.net%2Frichard%2Fastro%2Fpapers%2F602-magfields.pdf
Meziane, K., C. Mazelle, R. P. Lin, D. LeQue´au,
D. E. Larson, G. K. Parks, and R. P. Lepping,
Three-dimensional observations of gyrating ion distributions far upstream from
the Earth’s bow shock and their associated with low-frequency waves, J. Geophys. Res.,
106, 5731, 2001.
Montgomery, M. D., J. R. Asbridge,
and S. J. Bame: Vela 4 plasma observations near the
earth’s bow shock. Journal of Geophysical Research, Space
Physics, Vol. 75, No. 7, 1970.
Morse, D. L. and E. W. Greenstadt:
Thickness of magnetic structures associated with the earth’s bow shock. J. Geophys. 81, 1791-1793, 1976.
National Academy of Science, International
Geophysical Year World Data Center A, IGY World Data Center A, Corpuscular
Radiation, Magnetic Field, And Micrometeorite Observations With Satellites And
Space Probes, Rockets and Satellites, No. 14, July 1961.
Ness, N. F., The Earth's magnetic tail, J.
Geophys. Res., 70 (13), 2989–3005,
doi:10.1029/JZ070i013p02989, 1965.
Ness, N. F. and L. F. Burlaga , Spacecraft
studies of the interplanetary magnetic field, J. Geophys.
Res., 106(A8), 15,803–15,817, doi:10.1029/2000JA000118,
2001, DOI: 10.1029/2000JA000118, Article first published online: 19 DEC
2012
Ness, N . F., C. S. Scearcea, and J. B. Seek , Initial
results of the Imp 1 magnetic field experiment, J. Geophys.
Res., 69, 3531-3569, 1964.
Neugebauer, M., and C. W.
Snyder, The mission of Mariner II: Preliminary observations, solar plasma
experiment, Science, 138, No. 3545, 1095-1096, Dec. 1962.
Neugebauer, M., C. T.
Russell, and J. V. Olson, Correlated Observations of Electrons and Magnetic
Fields at the Earth’s Bow Shock, Journal of Geophysical Research, Vol.
76, No. 19, July 1, 1971.
Nishida, A. and L. J. Cahill Jr., Sudden
impulses in the magnetosphere observed by Explorer 12, J. Geophys. Res., 69(11), 2243–2255, doi:10.1029/JZ069i011p02243, 1964.
Parker, E. N., "Dynamics of
the interplanetary gas and magnetic fields." Astrophysical
Journal 128, 664, American
Astronomical Society, Provided by the NASA Astrophysics Data System,
1958.
G. Paschmann, N. Sckopke, S.J. Bame, J.R. Asbridge, J.T. Gosling, C.T. Russell, E.W. Greenstadt, Association of low-frequency waves with suprathermal ions in the upstream solar wind. Geophys.
Res. Lett. 6, 209–212, 1979.
Paschmann, G., N. Sckopke, S. J. Bame, and J. T.
Gosling, Observations of gyrating ions in the foot of the nearly perpendicular
bow shock, Geophys. Res. Lett., 9, 881, 1982.
Paschmann, G., G. Haerendel, N. Sckopke, E. Mobius, H. Luhr, and C.W.
Carlson, 3-Dimensional plasma structures with anomalous flow directions near
the Earth’s bow shock, J. Geophys. Res., 93, 11,279 –11,294, 1988.
Phillips, Tony, Hidden Portals in
Earth's Magnetic Field, NASA science, Science News, 2012.
http://science.nasa.gov/science-news/science-at-nasa/2012/29jun_hiddenportals/
Priest, Eric and Terry Forbes,
Magnetic Reconnection MHD Theory and Applications, Cambridge University,
2000.
http://assets.cambridge.org/052148/1791/sample/0521481791WSN01.pdf
RUSSELL, CHRISTOPHER T., THE SOLAR WIND AND
MAGNETOSPHERIC DYNAMICS, Institute of Geophysics and Planetary Physics
University of California, Los Angeles, U.S.A. ,
Originally Published In: Correlated Interplanetary and Magnetospheric
Observations, (ed. by D.E.Page), P. 3, D. Reidel Publ. Co., Dordrecht, Holland, 1974.
Russell, C. T., Solar Wind and Interplanetary
Magnetic Field: A Tutorial. 63p., 2000. http://wwwssc.igpp.ucla.edu/ssc/tutorial/solwind_magsphere_tutorial.pdf
Russel, C. T., The
Solar Wind Interaction with the Earth’s Magnetosphere: A Tutorial, IEEE
TRANSACTIONS ON PLASMA SCIENCE, VOL. 28. NO., 2000a.
http://www-ssc.igpp.ucla.edu/personnel/russell/papers/SolWindInteraction.pdf]
Russell, C. T., Y. L. Wang, J. Raeder, R. L. Tokar, C. W. Smith, K. W. Ogilvie, A. J. Lazarus, R. P. Lepping, A. Szabo, H. Kawano, T. Mukai, 7 S. Savin, Y. I. Yermolaev, 8 X.-Y. Zhou, and B. T. Tsurutani, The interplanetary
shock of September 24, 1998: Arrival at Earth, J. Geophys.
Res., 105, 25,143 – 25,154,
2000.
Sibeck, D. G., T. D. Phan, R. Lin, R. P. Lepping and
A. Szabo, Wind observations of foreshock cavities: A
case study, JOURNAL OF GEOPHYSICAL RESEARCH, VOL. 107, NO. A10, 1271,
doi:10.1029/2001JA007539, 2002.
Slavin, J. A., E. J.
Smith, and B. T. Thomas , Large scale
temporal and radial gradients in the IMF: Helios 1, 2, ISEE‐3,
and Pioneer 10, 11, Geophys. Res. Lett., 11(3), 279–282, doi:10.1029/GL011i003p00279. , 1984.
Smith, Edward J., A Comparison of Explorer VI and
Explorer X Magnetometer Data, Journal of Geophysical Research Volume 67, No. 5,
1962.
Smith, E. J., and A. Barnes,
Spatial dependencies in the distant solar wind: Pioneer 10 and 11, in
Solar Wind 5, NASA Conf. Publ., NASA CP CP 2280, 521, 1983.
Smith, E. and Tsurutani, B., Magnetosheath lion roars. Journal of
Geophysical Research 81(A13), Article first published online: 19 DEC 2012,
DOI: 10.1029/JA081i013p02261, 1976.
SMITH, EDWARD J., AND BRUCE T. TSURUTANI,
Observations of the Interplanetary Sector Structure up to Heliographic
Latitude, VOL. 83, NO. A2, JOURNAL OF GEOPHYSICAL RESEARCH, 1978.
Smith, Edward J., Robert E. Holzer,
Malcolm G. McLeod and Christopher T. Russell, Magnetic noise in the magnetosheath
in the frequency range 3–300 hz,
Journal Of Geophysical Research Vol. 72, No. 19, 1967.
SMITH, EDWARD J., ROBERT E. HOLZER AND CHRISTOPHER
T. RUSSELL, Magnetic emissions in the magnetosheath at frequencies near 100 Hz,
JOURNAL OF GEOPHYSICAL RESEARCH, SPACE PHYSICS Vo, 74, No. 11, 1969.
SONETT, C. P., D. L. JUDGE, AND J. M. KELSO,
Evidence Concerning Instabilities of the Distant Geomagnetic Field: Pioneer I, JOURNAL of GEOPHYSICAL RESEARCH, VOLUME 64, No. 8, 1959.
Spreiter, J. R., and W.
P. Jones, On the effect of a weak interplanetary magnetic field on the
interaction between the solar wind and the geomagnetic field, J. Geophys. Res.,
68, 3555-3564, 1963.
Svalgaard, L., E. W. Cliver, and P. Le Sager, Determination of interplanetary
magnetic field strength, solar wind speed and EUV irradiance, 1890–2003, in
Solar Variability as an Input to the Earth’s Environment, ISCS Symp., Eur. Space Agency, Paris, 2003.
Theplanetstoday.com http://www.theplanetstoday.com/
Thomsen, M. F., Upstream suprathermal
ions, in Collisionless Collisionless Shocks in the
Heliosphere: Reviews of Current Research, edited by B. T. Tsurutani and R. G. Stone, AGU, Washington D. C.,
253, 1985.
Thomsen, M. F., J. T. Gosling, S. A. Fuselief, S. J. Bame, and C. T.
Russell, Hot, diamagnetic cavities upstream from the Earth's bow shock, J. Geophys. Res.,
91, 2961-2973, 1986.
Trinklein, F. E., Modern
Physics, Holt, Rinehart and Winston, N.Y, 1990.
Tsunomura, Satoru,
Characteristics of geomagnetic sudden commencement observed in middle and low
latitudes, Earth Planets Space, 50, 755–772, 1998.
Turku, University of: Lecture 4 :
Synchrotron Radiation, 2006.
http://www.astro.utu.fi/~cflynn/astroII/l4.html
Van Allen, J. A., The
Geomagnetically Trapped Corpuscular Radiation, J. Geophys.
Res., 64, No.
A11, 1683, 1959.
Watermann, J., P. Wintoft, B. Sanahuja, E. Saiz, S. Poedts, M. Palmroth, A. Milillo, F. A. Metallinou, C. Jacobs, N.Y. Ganushkina,
I.A. Daglis, C. Cid, Y. Cerrato,
G. Balasis, A.D. Aylward,
A. Aran, Models of Solar Wind Structures and Their
Interaction with the Earth’s Space Environment, Space Sci
Rev DOI 10.1007/s11214-009-9494-9, pp.5. 2009.
Wilcox, J. M., Solar and
interplanetary magnetic fields, Science, 152, 161, 1966.
http://www.sciencemag.org/content/152/3719/161.long]
Wilcox, J. M. and N. F.
Ness, Quasi-stationary corotating structure in the interplanetary
medium, J. Geophys. Res., 70(23),
5793–5805, doi:10.1029/JZ070i023p05793. , 1965.
Wolfe, J. H., R. W. Silva, and M. A.
Myers, Observations of the solar wind during the flight of Imp 1, J.
Geophys. Res., 71(5), 1319–1340, doi:10.1029/JZ071i005p01319., 1966.
Yousif, Mahmoud E. “The Magnetic Interaction”,
Modified version: http://www.exmfpropulsions.com/New_Physics/MIH.htm
Fist published, 09-Oct-2003b, in Journal of Theoretics at: http://www.journaloftheoretics.com/Links/Papers/MY.pdf
Yousif, Mahmoud E. The Spinning Magnetic Field, at: http://www.exmfpropulsions.com/New_Physics/SMFc.htm
First published on 09-Oct-2003a. in Journal of Theoretics at: http://www.journaloftheoretics.com/links/papers/my-s.pdf
Yousif, Mahmoud E. THE UNIVERSAL ENERGIES, at: : http://exmfpropulsions.com/New_Physics/New_Energy/UE.htm
First published, on 18-Jan-2004, in Journal of Theoretics at:
http://www.journaloftheoretics.com/Links/Papers/Yousif.pdf
Published
By: