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Produced by the NASA Center for Aerospace Information (CASI)
NSSDC/WDC-A-R&S 82-28
DATA ANNOUNCEMENT BULLETIN
NAT'DNAL AERONAUTICS ANO SPACE ADMINISTRATION
NATIONAL SPACE SCIENCE DATA CENTER/
WORLO DATA CENTER A FOR ROCKETS AND SATELLITES
Code 601
Godda-d Space Flight Center • Greenbelt, Maryland 20771
November 1982
AVAILABILITY OF IMP-J (IMP 8) INTERPLANETARY
FIELD AND PLASMA DATA FOR THE INTERNATIONAL
MAGNETOSPHERIC STUDY PERIOD (IMS)
INTRODUCTION
One recommendation of the IMS Assessment Symposium# held at NSSDC in May of
1981# was that 5-min resolution composite interplanetary field and plasma data
sets be generated and made available to the scientific community. Hie purpose
of this Data Announcement Bulletin (DAB) is to announce the availability of
such a data set of IMP-J (IMP 8) field and plasma data.
The data set was compiled by Joseph H. King of the Goddard Space Flight Center
Laboratory for Extraterrestrial Physics# using data of that Laboratory and of
the Massachusetts Institute of Technology. Tlie magnetic field data are from
the Goddard Space Flight Center magnetometer (P.I.: N. F. Ness)# and the
plasma data are from the Massachusetts Institute of Technology Faraday cup
experiment (P.I.: H. S. Bridge). The plots and listings were generated by
Charles A. Wallace of the NSSDC staff.
DATA SET MEDIA AND TIME COVERAGE
There are actually two data sets available# one on a single magnetic tape
(NSSDC ID*. 73-078A-02E) and one on microfiche (NSSDC ID: 73-078A-02F) . The
microfiche data set consists of 11 fiche of plots displaying a subset of 3
parameters from the tape# and 41 fiche of listings giving a larger subset of
parameters from the tape.
The tape data set spans the period April 12, 1977, to May 24, 1980. Hie
microfiche data set covers a shorter interval, ending December 31, 1979. Ibis
covers a period from shortly before launch of the IMS-dedicated spacecraft#
the ESA-GEOS 1 synchronous orbit spacecraft of the European Space Agency,
through the end of the IMS data acquisition phase (December 31# 1979) at which
time IMP-J was in the solar wind. (Recall that in its ~ 35 Re# 12.5 day
orbit# IMP-J spends 4-5 days per orbit out of the solar wind, in the Earth's
magnetosheath and magnetotail regions.)
(NASA-T3-85226) AVAILABILITY OF TFP-J (IBP N83- 19658
8) INTFBFL ANETARY FIELD AND PLASMA DATA FOR
THE INTERN ATIC HAL MAGNETOS PH ERIC STUDY
PERIOD (1B2) (NASA) 26 p BC AC3/RF AO 1 Unclas
CSCL 93A G3/89 02559
V
ORIGINAL PAGE IS
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EXPECTED READER USE OF PLOTS, LISTINGS, AND TAPE
The purpose of the plots Is to enable the reader to Identify tines when
interplanetary variations are likely to have interesting nagnetospheric
effects. On the other hand, the purpose of the listings is to permit the
reader to quantify the state of the interplanetary medium for previously
Identified inceresting intervals of limited durations ; either the listed
parameters, or others readily computed therefrom, nay be of Interest. The
purpose of the tape data set, in addition to being the source of the plots and
listings data set, is to enable statistical studies and to enable the
quantification of the interplanetary nediun for individual intervals whose
long duration .enders working fron the data listing inconvenient.
COMPILATION OF THE TAPE DATA SET
This merged data set was generated as follows. First a 5-min IMF tape was
created. This tape contained 5-min averages of 15.36 s resolution field para-
meters for hours when, based on magnetic field data signatures, IMP-J was
judged to be beyond the Earth's bow shock for the entire hour. Plasma
parameters, averaged at MIT over ~ 1-2 min resolution, were taken from an
MIT-supplied tape for the times of the IMF records, and were merged onto the
IMF tape. The resulting tape is available to the scientific community from
NSSDC. Its format is shown in Appendix A. Note that in addition to basic
field and plasma data, information is given on magnetic connectivity between
IMP-J and the Earth's bow shock. There are field data in all records (whose
number, 136325, represents a 42% overall data coverage between the first and
last times), and there are plasma data in 79% of the records. This tape was
used to generate the associated plots and listings data set.
DESCRIPTION OF PLOTS
Rather than plot each of several interplanetary parameters, computed
parameters for each of two basically different ways the solar wind affects the
magnetosphere are displayed. Sample plots are shown in Appendix B.
Interplanetary pressure variations are responsible for large scale
magnetospheric compressions and relaxations* For example, shock associated
interplanetary pressure enhancements cause rapid magnetopheric compressions
recorded at the Earth's surface as geomagnetic storm sudden commencements.
One parameter plotted is interplanetary pressure, kNV 2 . After computing
pressure in units of dynes/cm 2 (N in cm"^, V in km/s, k * 1.67 x 10” 14 ), it is
plotted logarithmically on a scale from 1 to 100. Because of the neglect of
heavier nuclei, pressures are underestimated by typically 20%. It should be
noted that the magnetopause standoff distance is proportional to the sixth
root of the solar wind pressure.
The other mode of interaction between the solar wind and the magnetosphere is
electrodynamic. Many studies have shown that this interaction depends on
solar wind speed and on the intensity and orientation of the IMF. The more
nearly antiparallel the IMF and geomagnetic fields are in their interaction
region, the stronger the interaction. However, the details of the interaction
mechanism, and hence the most: appropriate combination of interplanetary
parameters, are problems on which a consensus has not yet been reached. For
2
ORIGINAL PAGE 18
OF POOR QUALITY
example, sine* 1978 Akasofu and coworkers Hava advocated
apailon > l 0 2 VB 2 sin* (8/2) aa tha moat appropriate parameter, where V, B, 9,
and 1 Q are flow apeed, magnetic field intensity, polar angle of the Y-Z
projection of the IMP vector, and an empirically determined effective
magnetoapheric cross-sectional radiua. However the aimple product B s *v (B a in
GSM coordinate#), which ia proportional to the y component of the molar wind
convection electric field, haa been uaed for a yet longer period and continuea
to be favored by many*
Both epsilon and B z *v were plotted on the same panel* Bpailon was computed in
unite of ergs/s, after which epailon (erge/a)/3*2 x 10 ^ 7 va s plotted logarith-
mically from 1 to 100. B_*V was computed in units of volta/m [3 x 10* x B x
(nT) x V (km/s)/c (3 x 10'° cm/a)], after which -B X *V (volta/m) x 10* was
plotted logarithmically from 1 to 100. These scales were chosen to yield
profiles only when the solar-wind- to-magnetosphere energy transfer is expected
t be very significant (B Z *V < 0, epsilon > 3.2 x 10 17 ). It may be observed
tl. \t these two parameters generally track each other well. Since most ~ 5 min
scale variations in these parameters follow from field variations rather than
flew speed variations, mean speeds (400 km/s) were used for those 5 -min
records having field data but no plasma data. On the plots, such times are
identifiable by the presence of epsilon and B Z *V traces and the absence of a
simultaneous pressure trace. In order to avoid the ambiguity between data
gaps and off-scale parameter values, off-scale values have been plotted near
the bottom or top of the appropriate panel.
DESCRIPTIONS OP DATA LISTINGS
The data listings provide the basic field and plasma parameters, as well as,
the computed, plotted parameters. A partial listing is shown in Appendix C.
Field parameters include the average field magnitude, Cartesian components in
solar magnetospheric coordinates, and the vector standard deviation— i.e. (ox 2
+ o y 2 + oz 2 P' 2 -- and the field azimuth angle. Plasma parameters include the
bulk flow speed (k»/s), proton density (ca“^) ; . proton temperature (deg K,
times 10~3), and the flow longitude and latitude angles (deg). These angles
are positive for flow from west and from south of the sun, respectively. In
preparing this data compilation, it was noted that the flow latitude angle
became increasingly positive with time. Over the 1975-1980 period, the trend
could be reasonably fit with the linear equation: Theta (deg) * 0.25 +
1 . 125*T, where T is fractional years since 1975.0. In consultation with MIT
personnel, *his trend was attributed to Instrumental effects, and it was
subtracted from the MIT-supplied data before generating the composite
field/plasma tape and listing therefrom.
The computed parameters listed are pressure (dynes/cm 2 , times 10”^), epsilon
(ergs/s, times 10" 1 ®), and B Z *V (nT*km/s). Note that between the plots and
listings, epsilon involves a different normalization factor (3.2 x 10 17 vs
10^), and B Z *V involves different units (volts/m vs. nT*km/sj 1 volt/m ■
10 6 nT*Vm/s) . As noted above, V » 400 kra/s was assumed in computing both
epsilon and B Z *V for records having field data but no plasma data.
3
ORIGINAL PAGE IS
OF POOR QUALITY
ORDERING INFORMATION
When making inquiries about the data, please refer to the NSSDC IDs:
73-078A-02E for the tape data set
73-078A-02F for the microfiche data set
Researchers residing in the United States should direct inquiries to
National Space Science Data Center
Code 601.4
Goddard Space Flight Center
Greeibelt, Maryland 20771
Telephone: (301) 344-6695
FTS: 344-6695
Researchers who reside out tide the United States should direct inquiries to
florid Data Center A for Rockets and Satellites
Code 601
Goddard Space Flight Center
Greenbelt, Maryland 20771, U.S.A.
Telephone: (301) 344-6695
Telex: NASCQM GBLT 89675
4
APPENDIX A
ORIGINAL PAGE IS
OF POOR QUALITY
FORMAT OF 5-HIN RESOLUTION MTRGBD IMP-J IMF-PLASMA TAPE
This IMP-J tape contains 5-minute nlasma parameter averages provided by MIT,
5-minute INF averages computed from GSFC 15.36 sec data, and information on
whether the 5-min IMF vector intersects the Earth's bow shock. Only times
when IMP-J is in the solar wind are included. There are magnetic field data
in every record. Some records have fill data (■* 0.0) in the plasma words.
The tape is a 9-track, 1600-bpi, binary tape created on an. IBM 3081 computer.
The tape format is fixed block with a logical record length of 45 words (180
bytes), blocked 150 logical records per physical record. The physical record
length is 6750 words (27,00C bytes). The last physical record on the tape may
be short, but is an integer multiple of logical records.
The IBM JCL for the DCB parameter used to create the tape was:
NL, 9 TRACK, DEN 3, RECFM-FB, LRECL-180, BLKSIZE-27000
Format of logical data record:
word
type
data
1 .
1*4
Year
(77,
78, 79, 80)
2.
1*4
DDay
(Jan
1 - Day 0)
3.
1*4
Minute of
day at start of average (0, 5... 1435
4.
1*4
Number of
1.28 s IMF values in 5-min B average i
that each
15.36 s average consists of up to 12
1.28
s values)
5.
1*4
Number of
15.36 s IMF values in B average
6.
1*4
Number of
points in plasma parameter averages
7.
R*4
*gsm
8.
R*4
y GSM
►
IMP-J position, km
9.
R*4
Z GSM
10.
R*4
Geomagnetic Latitude of Sun (degree)
11.
R*4
< 1 b|
>
nT
12.
R*4
< Bx gsm >
nT
A-1
APPENDIX A (continued)
ORIGINAL PAGE IS
OP POOR QUALITY
word
13.
14.
15.
16.
17.
18.
19.
20 .
21 .
22 .
23.
24.
25.
26.
27.
28.
29.
30.
31.
32.
33.
34.
type
R*4
RM
R*4
R*4
R*4
R*4
R*4
R*4
R*4
R*4
R*4
R*4
R*4
R*4
R*4
R # 4
R*4
R*4
R*4
R*4
R*4
R*4
data
< b *gsm : nT
< B ZqSM > "T
(< Bx > 2 ♦ < By > 2 + < B 2 > 2 )V 2
0 ®GSM de^reea (from <By>, <By>, <Bx>)
♦bq SM degrees (from < B x >, < By >)
%
h nT,
in generation of 5 -min averages from 15.36 n values
{ < ° x 2 + Oy 2 + a z 2 >}V2 these o's arise in the generation of
15. 36 s averages from 1.28s values
Maximum value of any of the o's contributing to word 21
V, km/s (bulk flow speed)
° v , km/s
N, cm”3 (proton density)
a N, cra“3
W, km/s (thermal speed)
a w , km/s
degrees, flow azimuth ( + from west)
° ( j > , degrees
® v , degrees, flow latitude (+ from south)
°9, degrees
y GSE position, km)
Z GSB (IMP"* 11 position, km)
APPENDIX A (concluded) ORIGINAL PAG” F0
OF POOR QVAUVf
word
type
data
35.
R*4
<
B Y G SE >
36.
R*4
<
b *gse > nT
37.
R*4
X*
38.
R*4
y
km, in G8E, point of intersection between IMF line
through IMP-J, and the bow shock (see footnote)
39.
R*4
2.
40.
R*4
Distance (km) along B between IMP-J and bow shock intersection
point
41.
R*4
Angle ( in degrees ) between ^ and bow shock normal at
intersection
42.
R*4
B 2
,*V (nT x km/s)
43.
R*4
E
(ergs/s)-2 x 10 14 x V x B 2 x SIN 4 (1/2 tan” 1 /l B ycSMl\\
B *GSM J I
44. R*4 1.67 X 10“ 14 X N x V 2 , dynamic pressure in dynes/cm 2
45. Spare
NOTES: In word 31 0 V (on this tape) » 0 V (on MIT tape) - (.25 + 1.125T) deg
where T is fractional years since 1975.0
In words 42 and 43, V * 400 is used for records with no plasma data.
Words 37-41 * -999. for no-intersection cases. (Intersection calculations are
based on a model bow shock - Fairfield, J. Geophys. Res ., 76 , 6700 - adjusted
for simultaneously observed solar wind pressure when available. )
A-3
LL61 *21
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