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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 


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