Supported by the National Aeronautics and Space Administration … · S-3 project scientist at...

121
/ m EXPLORER 12 MAGNETOMETER RECORDS 16 AUGUST, 1961-6 DECEMBER, 1961 by Robert S. Hyde and Laurence J. Cahill, Jr. Supported by the National Aeronautics and Space Administration under Grants NsG-33.-60 and NsG-624 and Contract NASw-155 and by the Air Force under Contract AF29(601)-4618. https://ntrs.nasa.gov/search.jsp?R=19670016631 2018-06-24T02:47:25+00:00Z

Transcript of Supported by the National Aeronautics and Space Administration … · S-3 project scientist at...

/m

EXPLORER 12 MAGNETOMETER RECORDS

16 AUGUST, 1961-6 DECEMBER, 1961

by

Robert S. Hyde and

Laurence J. Cahill, Jr.

Supported by the National Aeronautics and Space Administration

under Grants NsG-33.-60 and NsG-624 and Contract NASw-155 and

by the Air Force under Contract AF29(601)-4618.

https://ntrs.nasa.gov/search.jsp?R=19670016631 2018-06-24T02:47:25+00:00Z

Explorer 12 Magnetometer Records

16 August, 1961 - 6 December, 1961

Robert S. Hyde and Laurence J. Cahill, Jr.

This set of records was prepared in the Physics

Department of the University of New Hampshire between

August 1962 and August 1966. The data from which these

records were made were provided by the NASA Goddard Space

Flight Center, in digital form, on magnetic tapes. The

data tapes contained magnetic field measurements from a

three-component Schonstedt Instrument Company fluxgate

magnetometer, the time of the measurements, and several

other useful related measurements. Each sensor had a

nominal range of ± i000 gammas in measurement of the magnetic

field component along its sensitive axis. One sensor,

the Z sensor, was aligned approximately (within 2° ) with

the spin axis of the satellite throughout the flight.

The spin rate was approximately 30 rpm. The other two

sensors, X and Y, were orthogonal to the first sensor and

to each other. Each sensor was sampled in sequence X, Y,

Z during a 50-millisecond interval, and the sample rate was

three times each second. During ground processing the

analog magnetometer signals were digitized with an effective

digitization channel width of 24 gammas. Each component

measurement had an uncertainty due to digitization of ± 12

gammas, as well as other errors due to possible changes

in preflight calibration. The other errors have been

/

i

discussed in several papers on the Explorer 12 magnetometer

data. These papers are listed in the bibliography.

The X, Y, Z measurements were used to compute

B = / X2+y2+z2 , _ = tan -i / x2+y 2 /Z and

= _0 + _At + tan -I Y/X (where _ is spin angular velocity

At is time between measurement and "see-sun" time and _0

angle between sun sensor and x sensor, Figure i). In an

average of several individual measurements, the digitization

error, if random, may be reduced. The data points shown in

these records are averages of 32 individual computed values

(occasionally 16 values) of B, a and _. One data point was

computed every 500 km in radial distance. The time interval

between points varies from a few minutes near 5 R to ane

hour near apogee. The records have served as an initial

survey of the Explorer 12 data, have aided in selection of

periods for more intensive study,!and have provided material

I

for several papers listed in the bibliography. _he records

have been useful in determining the location of the magnetosphere

boundary; the distortion of the field inside the magnetosphere

and the general level of low frequency (<0.001 cps) magnetic

fluctuations in the magnetosphere. They have not been adequate

for detailed studies of the magnetopause, for studies of low

amplitude fluctuations in the magnetosphere or for any studies

of the transition region.

The measured values B, _, _ shown here were plotted by

hand at the appropriate geocentric radial distances specified

on a "Master Orbit" magnetic tape also provided by GSFC.

3.

Data below 5 Re were not plotted because the magnitude

increases rapidly and the field distortion becomes

imperceptible on the scale of these records. The vertical

scale for B is in gammas and the scales for _ and _ in

degrees. The approximate time and magnetic latitude of a

measurement may be obtained from the auxiliary Universal

Time and latitude scales at the top of each record.

The predicted field B, e, and 4, according to the

Jensen and Cain, 1962, reference field, was computed from

information provided on the Master Orbit tape on the

assumption that the spin axis direction was 47 ° Right

Ascension and -27.5 ° Declination in celestial coordinates.

Since the processing and plotting of these data

several errors have been noted in the original plots. In

late 1965 facilities became available at UNH for computer

processing (IBM 1620) and automatic plotting (Cal Comb) of

magnetic tape data. We have reprocessed the Explorer 12

data and have prepared automatic plots of B, _, _ once

every five minutes. The original records have been compared

to these more recently plotted records and corrections have

been made where necessary. In addition, a careful check of

time, magnetic latitude and predicted field has been made.

A number of errors may still remain in these records, but

they are useful in showing the general characteristics of

the outer magnetosphere and its boundary in the fall of 1961.

8

Acknowledgments

The laboratory in which this experiment was planned

and tested was equipped with support under NASA Grant NSG-33-60

and Air Force Contract AF29(601)-4618. The work on the flight

instruments was supported by NASA Contract NASw-155 and the

data analysis proceeded under support of NASA Contract NASw-155

and Grant NSG-624.

We acknowledge the guidance of Dr. Frank MacDonald,

S-3 project scientist at Goddard Space Flight Center in the

planning and development of the experiment. The S-3 project

office at GSFC assisted in many ways during the construction

and testing of the experiment. We are particularly grateful

to Mr. Paul Butler, Project Manager.

Many students and associates at UNH contributed to

the success of the experiment and to the analysis of data.

Paul Amazeen and Wendell Sawyer were major contributors to the

experimental effort, while V. L. Patel and Marilyn Wingersky

shared responsibility in data processing.

The interested and responsible assistance of Erick

Schonstedt, who built the fluxgate instruments, and his associates

was essential to our project. Availability of the Fredericksburg

Magnetic Observatory, under the direction of Mr. Robert

Gebhardt, aided testing of the experiment.

The enthusiastic assistance of many technical and

administrative employees at UNH was essential. Among these

employees were Anne Anders_n, Carl Flanders Herbert Scheibel

and Phyllis Warnock.

References

A. Papers Based Principally on_Explorer 12

Magnetic Results

Cahill, L. J., Jr., A study of the geomagnetic field, Space

Research III, 324-330, (ed. W. Priester), North HollandPub. Co., Amsterdam, 1962.

Cahill, L. J., Jr., and P. G. Amazeen, The boundary of the

geomagnetic field, J. Geophys. Res., 68, 1835-1844, 1963.

Cahill, L. J., Jr. and D. H. Bailey, Distortion of the

magnetosphere during a magnetic storm on September 30,

1961, J. Geophys. Res., 72, 159-169, 1967.

Cahill, L. J., Jr., and V. L. Patel, Further obserations of

the geomagnetic boundary: Explorer 12 UNH Research Report

64-4, 1964, to be published in Planetary---and Space Sci.,1967.

Fairfield, D. H. and L. J. Cahill, Jr., Transition region

magnetic field and polar magnetic disturbances, J. Geophys.

Res., 71, 155-169, 1966.

Mead, G. D. and L. J. Cahill, Jr., Explorer 12 measurements of

the distortion of the geomagnetic field by the solar wind,

GSFC X-640-66-527, November, 1966, to be published in

J. Geophys. Res., 1967.

Nishida, A. L. J. Cahill, Jr., Sudden impulses observed by

Explorer 12, J. Geophys. Res., 69, 2243-2255, 1964.

Nishida, A. and J. H. Young, Explorer 12 observations of

magnetic sudden impulses in the earth's magnetosphere,

Nature, 201, 1113-1114, 1964.

Patel, V. L., Structure of the equations of cosmic electro-

dynamics and photon rest mass, P__s. Letters, 14,105-106, 1965.

Patel, V. L., Low frequency hydromagnetic waves in the magneto_

i 13_sphere: Explorer 12, Planetary and S a___ Sci,_ __485-506, 1965.

Patel, V. L. and L. J. Cahill, Jr., Evidence of hydromagnetic

waves in the earth's magnetosphere and of their propagation

to the earth's surface_ Phv___s° Rev. Letters _ 12_ 213_215_ 1964.

Patel, V. L., L. J. Cahill, Jr., and A. J, Dessler_ Magnetosheath

field geomagnetic index a_ and stability of magnetopause,J. Geophys. Res., 72, 426 430, 1967.

Sonnerup, B. U. O. and L. J. Cahill, Jr., Magnetopause structure

and attitude from Explorer 12 observations, J. Geophys. Re__s.,

72_ 171-182_1967.

S. Papers Based Partiall_.gn Explorer 12

Magnetic Results

Freeman, J. W., J. A. Van Allen and L. J. Cahill, Jr., Explorer 12

observations of the magnetosphere boundarv and the

associated solar plasma on September 13, 1961, J. Geophys.

Res., 68, 2121-2130, 1963.

Hoffman, R. A., L. R. Davis and J. M. Williamson, Protons of

0.i to 5 Mev and electrons of 20 kev at 12 earth radii

during sudden commencement on September 30, 1961, J.

Geophys. Res., 67, 5001-50005, 1962.

Konradi, A. and R. L. Kaufmann, Evidence for rapid motion of

the outer boundary of the magnetosphere, _. Geophys. Res.,

70, 1627-1637, 1965.

Rosser, W. G. U., Changes in the structure of the outer

radiation zone associated with the magnetic storm of

September 30, 1961, _. Geophys. Res., 68, 3131-3148,,1963.

Rosser, W. G. U., B. J. O'Brien, J. A. Van Allen, L. A. Frank

and C. D. Laughlin, Electrons in the earth's outer

radiation zone, J. Geophys. Res., __67, 4533-4542, 1962.

Spreiter, J. R. and W. Jones, On the effect of a weak

interplanetary magnetic field on the interaction between

the solar wind and the geomagnetic field, J. Geophys. Re___ss.,

68, 3555-3564, 1963.

Ca Review Articles

Cahill, L. J., Jr., The geomagnetic field, Ch_. 9, 301-349,

Space Physics, ed. D. P. LeGalley and A. Rosen, John

Wiley and Sons, Inc., New York, 1964.

Cahill, L. J., Jr., Magnetic field measurements in space,

Space Science Rev., l, 399-414, (ed. C. de Jager) 1962.

Hines, C. 0., The magnetopause: a new frontier in space,Science, 141, 130-136, 1963.

D. Abstracts

Cahill, L. J., Jr., Distortions of the geomagnetic field

within the inner magnetosphere, Trans. A.G.U., 46, 116,

1965.

Cahill, L. J., Jr., Study of the outer geomagnetic field,

Trans. A.G.U., 4__3, 217, 1962.

Cahill, L. J., Jr., and S. A. Knowles, Transition region

magnetic fields, Trans. A.G.U., 46, 531, 1965.

Cahill, L. J., Jr., and P. G. Amazeen, Termination of the

earth's magnetic field during the period September 11-14,

1961, Trans. A.G.U., 43, 218, 1962.

Cahill, L. J., Jr., and V. L. Patel, The SC and the main

phase of a magnetic storm in the outer space, Trans. A.G.U.,

43, 459, 1962.

Patel, V. L., and L. J. Cahill, Jr., On the stability of the

magnetospheric boundary, Trans. A.G.U., 46, 530, 1965.

Patel, V. L., and L. J. Cahill, Jr., Polarization of low-

frequency hydromagnetic waves in the magnetosphere,

Trans. A.G.U., 45, 78, 1964.

Patel, V. L., and L. J. Cahill, Jr., The geomagnetic field

boundary and associated solar wind, Tran__ss, A.G.U., 43,459, 1962.

Patel, V. L., and L. J. Cahill, Jr., The magnetic storm of

September 30, 1961: Explorer 12 measurements, Trans.

A.G.U., 43, 218, 1962.

F

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