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UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY PRELIMINARY GEOMAGNETIC DATA COLLEGE OBSERVATORY FAIRBANKS, ALASKA OPEN FILE REPORT 82-03OOL

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Page 1: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals

UNITED STATES DEPARTMENT OF THE INTERIOR

GEOLOGICAL SURVEY

PRELIMINARY GEOMAGNETIC DATA COLLEGE OBSERVATORY

FAIRBANKS, ALASKA

OPEN FILE REPORT 82-03OOL

Page 2: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals

T H I S REPORT WAS PREPARED UNDER THE DIRECTION O f JOHN Bm TOWNSHENDJ C H I E F OF THE COLLEGE OBSERVATORY* WITH THE ASSISTANCE OF THE OBSERVATORY STAFF MEMBERS: JaEa PAPP, € , A , SAUTER, L n Y , TORREPICE* T a K ; CUNNINGHAM AND I N COQPERATION WITH THE GEOPHYSICAL INSTITUTE OF THE U N I V E R S I T Y OF ALASKA, THE COLLEGE OBSERVATORY IS A PART OF THE BRANCH OF ELECTROMAGNETISM AND GEOMAGNETISM OF THE UBSm GEOLO- GICAL suuvEr,

ORD'EX OF CONTENTS

Explanation of Data and Reports

hhgnetic Ac t iv i ty Report

Outstanding Magnetic Effects \

Principal. Magnetic Storms

Prelimina~y Calibration Data and Monthly Mean Absolute Values

Magnetogram Hourly Scalings

Sample Format fo r Normal. and Storm Magnetograms

Normal Magnetograms

Storm lkgnetograrns (When Normal is too disturbed to read)

Page 3: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals

GO1 1 FGF OBS-NTPIARY GFOMAGNET1C BAT4

F 4 s

The preliminary geomagnetic data included here is rnade available t o s c i en t i f i c personnel and organizstions as part of a cooperative e f for t and on a data exchange basis because of the ear ly need by some users. To avoid delay, a l l of the data is copied from original forms processed a t the observatory; therefore it should be regarded as preliminary, Inquiries a b u t this report or about the College Observatory should be addressed to:

Chief, Callege Observatory U. S. Geological Survey 800 Yukon Drive Fairbanks, Alaska 99701

Requests for copies of the magnetograms except for the current month should be addressed to:

Norld Data C e n t e r A NOAA D63, 325 Broadway Boulder, Colorado 80303

GEOMAGNETIC DATA

Normal., Storm and Rapid Rum magnetograms and appropriate cal ibrat ion data a re processed dai ly st the observatory and axe available for analysis o r copyinq. Also available, are mean houxljr scalings, K-Indices, selected magnetic phenomena reports and on a real-time basis are recordings from a 3-compo- nent f l u g a t e magnetometer and F-component proton mgnetometer . Fhgnetic Activity

The K-Index: The K-Index is a logarithmic measure- ment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals beginning 0000-0300, 0300-0600,.2100-2400 IJT. I t is a measure of the difference between the highest and Lowest deviation from a smooth curve t o be expected for s component on a magnetically quiet day, wfthin s three hour interval .

The Equivalent @fly Amplitude, AK: The K-Index f s converted i n to an equivalent range, ak, which is near the center of the lfmiting garmna ranges for a given K. The average of the eight values is called equivalent dai ly amplitude AK. The u n i t I@ has been chosen so as not t o give the i l l u s ion of an accuracy not jus t i f ied .

The schedule for converting gama range t o K, and K t o a k is ss follows:

K - Index 0

The hZegnet1e Daily Character Figure, C : To each Universal day a character is assigned on the basis C=0, if it is quiet; C = l , i f it 1s maderately disturbed; C=2p i f i t fs great ly disturbed. The method used to assign characters a t the College Observatory is based on AK as follows:

AK Range 0- It

11-50 : 1

50* 2

Routine assignment of C was discontinued st College on January 1, 1476.

OBSERVATORY L O C A T I O N

The College Observatory, operated by the U.S. Geological Survey, is Located a t the University of Alaska, Fairbanks, Alaska. It is near the Auroral Zone and the northern l i m i t of the world's greatest earthquake be l t , the circwn-Pacific Seismic 5elt. Although the observatory's basic operation i s i n geo- magnetism and seismalogy, i t cooperates with other s c i en t i s t s and organizations i n areas where the faeil- i t y and personnel can be of service.

The observatory is one of three opersted by the USGS i n Alaska. The others are located a t brraw and S i t l a .

The position of the observatory s i t e is: Geographic la t i tude. . . . . . .a03l. 6'N Geographic longitude.. . . . .U?50.2'W Geomagnetic la t i tude. . . . . .+U. @ Geomagne t ie longitude . . . . . +2 5 6 . 9 Elevation. ................200 meters

Selected Phenomena L Outstandfng Magnetic Effects Prior to January 1, 1976, %he Norm1 and Kapid

R u n records were reviewed st the observatory for selected mgnetic phenomena and the events ident i f ied were formrded t o the IUCC Commission on Magnetic Variations and Disturbances. T h i s m s discontinued on January 1, 1976, but a report on Outstanding Mgnetfc Effects is prepared monthly far this report.

Principsl Magnetic Storms Gradual m d sudden commencement magnet1 c d i s t u r -

bances with st leas t one K-Index of 5 or greater, which a re believed to be part of s world-w5de disturbance, are classified as principal mgnetic storms, The t ine of the storm beginning and end-; direct ion and amplitude of sudden comencements; period of maximum ac t iv i ty ; and storm range a r e reported. MonthLy reports of these data are forwarded to the World Data Center A i n &ulder, Colorado.

kgnetogram Hourly Scalings Mametomam hourl~ searims are averages for

successive of one hour-for the D, H and z elements. The Value i n the column headed "01" is the average for the hour beginning 0000 and ending 0100. Note that the values on the scaling sheets a r e in tenths of mm with t h e decimal point omitted. The user of these sealings should keep in mind tha t the tabular values a r e hourly means and i f he is interested in the detailed morphology of the magnetic f i e ld , he should re fe r d i rec t ly t o the magnetogrms.

Magnetograms The n o m l magnetograms in t h i s report are repro-

duced a t about one-thfrd the s i ze of the orlgfnals. Preliminary base-line values and scale values adopted f o r use d t h the original magnetograms are included. For days when the mgnetic f i e ld is too disturbed for the Normal maipetogram t o be readable, Storm magnetograms are reproduced.

Absolutes, Base-lines and Scale Values To determine the sbsolute value of the mgnetic

f i e ld from the hourly means or from point scalings the following equations should be used:

%, % and BZ are base-line values; SD, % and SZ are scale values; and d , h and z are scalings i n millimeters.

Page 4: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals

U. S. DEPARTMENT OF COMMERCE Mi)AA 'OR' 76-133 NATIONAL OCEANIC AND ATMOSPHERIC ADMINISTRATION (9-72) I

, DATE

OBSERVATORY

COLLEGE, ALASKA

MAGNETIC ACTIVITY (Greenwich civi l timm, counted from midnight to midnight)

-

K-INDICES TIME SCALE ON

n ID - m MAGNETOGRAMS - .- t

% % A 0 0 0 k c h b c c y - N SUM

AK 1 - 20 I n m h

0 0 2 l I 0 0 0 0 03 01 SUDDEN COMMENCEMEHTS

0 0 0 2 1 0 0 06 03 d h m

0 0 1 1 5 4 1 1 1 3 11 2 3 1 2 1 1 2 3 15 08 3 3 5 3 2 2 1 0 19 14

0 0 2 2 1 0 0 0 0 3 3 7 6 6 3 2 5 6 6 6 6 2 3 3 4 4 7 4 3 2 1 6 6 5 5 5 3

3 4 2 1 3 5 5 A 2 2 4 7 6 3 3 1 1 1 0 3 1 2 2 1 1 1 1 . 3 2 0 2 3 2 2 4 5 2 1 1 0

0 0 3 5 6 5 5 3 5 4 9 7 7 6 5 4 3 4 7 8 7 6 5 3 6 4 4 6 6 4 3 3

POSSIBLE SOLAR-F LARE EFFECTS BASED ON

3 3 5 6 7 7 6 1 , INSPECTION OF GRAMS ALONE {WIXHQUT

REFERENCE TOOATA

3 4 5 6 7 7 5 4 FROM OTHER SOURCES)

5 6 4 4 6 7 2 1 1 5 7 ' 7 6 4 3 3 2 4 5 5 5 3 2 2 2 5 4 5 5 2 1

1 2 3 3 5 4 1 1 1 0 5 6 5 4 2 3 3 4 6 5 6 5 4 3 4 2 4 5 5 5 4 3 3 3 4 6 3 4 3 2 3 2 2 3 2 0 0 0

I

- MONTH AND Y E A R

DECEMBER 1982

APPROVED JOIIN B. TOWNSHEND, CHIEF, UXLEGE OBSERV~TORY - OBSERVER IN CHARGE.

NOAA FORM 76-lad SUPERSEDES CLGS FORM 81m * U.S. GOVERNMENT PRlHTtNG OFFlCE:197S-761-057

K S C A L E USED: D I LOWER LIMIT FOR K = 9.. . . . . . ,, CURRENT SCALE VALUE.. . . . ., . LOWER LIMIT FOR K = s . . . . . . . .

H Z

S C A LIH GS AND COMPUTATtOWS HAVE BEEN CHECKED.

683.8 3 73

2550

321.7 7-79

251U

1 1 Imm)

['Y/mm) I

(to nearest 1 OY]

Page 5: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals

si*

pg, p i 1, p i 2, sfe.

Page 6: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals

PR3NCIPAL MAGNETIC STORMS wm-A FOR 8 b U R ~ T ' E U U t . 1 I ' I 1 & l Pnrrlu ' SHVtROHMLHTAL DATA SfRVlCf , NOAA

BOULOCR, COLQRAOO .OSOt U.8.A.

Page 7: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals

AWAL PShTETOGRAPB -

PERIOD C r n I O I P C W W L K P ?ma I rn S C ~ ~ E ' V A U E BASE-

0000U.Z~ 12-/-62 ]2$'00U.75 /2-3/-83 ,! A/&M 3.7 Z / ~ M 37" Y Z ~ O d E

D 1 I

moo U.7, /$ -/ -62 1 2 f 0 0 U . r ~ )5! -31-82 7 s b/mm /275/ b'

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sT0m M k ; E ' ; Y Y ; M

m O D C m f m C ~ R P

FRM IK) SZALE VbLUE I B E S I D B - I

oboa U.T, /J1 -1-83 &?qoo 0.7; 12 -31-82 7 3 / ~ 1 9 6 8 / m ~ 23" y 2 . 2 z

n

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1 ~ O O L J , T ~ 13 -1 -82 lavdoo.~ / s - 3 / - ~ 2 . yg. s K/MM 5 4 ~ 2 b'

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I I I I HO- HEAR d B S O m VALUES* 1

D B 5

27" 5619 L: /a259 - 553 92 + C ( M A I L E D F 3 M l l E R Q - . A A T S M J W A [ : m .

D m m: DEC J 2 3 4 /3 /4 1 5 ,3/ . , * , 5 # 6 * , , -

Page 8: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals

MACMEtOGRkM HOUR t Y ICALtMCS

t J t w ~ r p l m r e d C 1 e m l i m ~ w c n m i a brerr. of a#uetir a t m .

r4 Sirnitiranr m i m el hau imtrtpolstmd. <> Rrcmd oll m b q t l a pn

a m 1 I d k a u ; it +due i m a No rrcord: or ED rrlwa mwm ilmblr brraumm d fnulrr rrrwd.

Page 9: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals

C> R c c a d otl nhcta la p n u nil 01 haw: il vmbwc ia

ivca c w v r r r r rati-ted f u mtrmiea .' p r ~ .

Page 10: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals

MAGHETOCRAM HOURLY 3ChLIHGJ IuntvEus*L T I M E )

I Inrrrpnl* lrA C3 k m l is* ueccrtmin k r m m t u o u r u ~ v SUY ol mmln*lrt rtwm. rJ 5 r # m ~ f w * n t lnrl joa .1

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a m I I m i hour: il w l u c II IJ Fo I,, wrd. n* no w m l m ~ r DATE% W ~ T W ~ A W ;

~ i * r m . t w - r r m m rmr iwt rd

Page 11: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals
Page 12: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals

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Page 13: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals
Page 14: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals

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Page 15: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals

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Page 16: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals

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Page 17: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals

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Page 18: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals
Page 19: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals

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Page 20: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals
Page 21: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals
Page 22: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals
Page 23: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals

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Page 24: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals
Page 25: UNITED STATES DEPARTMENT OFdggs.alaska.gov/webpubs/usgs/of/text/of82-0300l.pdfment of the rrnge of the mmdst disturbed component (D or H) of the geomagnetic field for eight intervals