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S... . - J 4 .6;"a.•.p%...inZj._.s.,. - AFCRL-TR-7S-0185 ENVIROKMEHTAL RtE$EARCH PAPERS, 1O. 503 C'q Tables of Asymptotic Directions and Vertical - Cutoff Rigidities for a Five Degree by Fifteen C Degree World Grid as Calculated Using the "International Geomagnetic Re t erence Field for Epoch 1975.0 M. A. SHEA 0. F. iMART 3 April 1975 JUL 2IM B Appnn~d for publlc r.Inns* distribhulen unllaited. "SPACE PHYSICS LABORATORY PROJECT 8600 AIR FORCE CAMBRIDGE RESEARCH LABORATORIES HANSOM AFB, MASSACHUSETTS 01731 AIR FORCE SYSTEMS COMMAND, USAF "ti

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Page 1: S J - DTICunclassified 1 "-report documentation pager nstruct rnbefore comipleting form iatfcr1_-tr-75-,,185--- -, , '.-.-) tables of asymptotic directions and vertical cutoff rigidities

S... . • -J 4 .6;"a.•.p%...inZj._.s.,. -

AFCRL-TR-7S-0185ENVIROKMEHTAL RtE$EARCH PAPERS, 1O. 503

C'q Tables of Asymptotic Directions and Vertical- Cutoff Rigidities for a Five Degree by Fifteen

C Degree World Grid as Calculated Using the"International Geomagnetic Re terence Field forEpoch 1975.0

M. A. SHEA0. F. iMART

3 April 1975 JUL 2IM

B

Appnn~d for publlc r.Inns* distribhulen unllaited.

"SPACE PHYSICS LABORATORY PROJECT 8600

AIR FORCE CAMBRIDGE RESEARCH LABORATORIESHANSOM AFB, MASSACHUSETTS 01731

AIR FORCE SYSTEMS COMMAND, USAF

"ti

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Qualified requestors may obtain additional copies from the DefenseDocumentation Center. All others should apply to the NationalTechnical Information Service,

-. *, , .•, - -. • • • • , , • •. . : , 4. - t ..... . . . . . .

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Unclassified

"-REPORT DOCUMENTATION PAGER NSTRUCT1 RNBEFORE COMIPLETING FORM

IAtFCR1_-TR-75-,,185--- -, , '.-.-)

TABLES OF ASYMPTOTIC DIRECTIONS AND VERTICALCUTOFF RIGIDITIES FOR A FIVE DEGREE BY 1-IrTEEN DEGRE ___

WORLD GRID AS CALCULATED USING TIHE I1NtERNATIONAL 6 PERAORMING ONG. RE,-ORT I•juSERGEOMAGNETIC REFERENCE FIELD FOR EP&H 1975.0, ERP No. 503

S.. .. O *......... -- *-~*-.. •6 CONTRACT OR GR4ANT NUM9•ER()

/ M. A.:Shea -"" "

. F. /Smart A, ,N AND•

Z. - a5OlM4U A~il T,01 4AMCAN0 CL 0 P R 'i_-

Air Force Cambridge Research Laboratories (PHE) . " foRK UNT NUMBERSHanscorm AFB ,, 860007W 681311Massachusetts 01731 . 6l102FI I 'ONTROLLING OFFICE NAME AND ADORE-S

Air Force Cambridge Research Laboratories (PHEY1 J 3 AprIn75 ZHanscom AFB M ,--- bitM% .ssachusetts 01731 _,"166. - ._ _

I4-. MONITOrI4G AGENCY NAME & AODRESStt dij!elolt from. Comroif-Ilr Ofhlle) IS. (Of thli repoti

Unclassified154 DECL ASSI•ICATION DOWN RADING

SCHEDULE

'6 IST1RI!iT'ON STATEMENT /of thi Report)r

Approved for public release; distribution unlimited.

17. DISTRIBUTION STATEMENT f )*,o ah.tes.ct eo¶.,@d In Block 20. Il difforeri f-om Repo.,)

13 KEY WORDS Con•linue ar tgovers. side it n.e..,.•y and Identify by block nub.er)

Cosmic radiationVertical cutoff rigiditiesGeo agnetic field modelsAsy ptotic directions of approach

20 A( RACT oCnre•erIu s, on e side if nece.sary and Identify by block nu•ber)

Tables of asymptotic directions and vertical cutoff rigidities for a fivedegree by fifteen degree world grid are presented. These values were ob-tained by the integration of vertically incident cosniic-ray trajectoriesthrough the International Geomagnetic Reference Field with time derivativesapplied so that the coefficients form a quiescent model o', the geomagneticfield for Epoch 1975.0. The table of asymptotic directions contains theasymptotic latitudes and longitudes which specify the direction of approach.,

DDJ 1473 -101 1 OP01 IS IS OSSOLETE UnclassifiedSECURITY CLASSIFICATION OF THIS PAGE (WhW D.I.•"v.d)'

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" •UnclassifiedSE-~kT CL AS-~,$PICAT to- OF tnt P~aE'W'qk, VPk Enfatod)

20. Abstract (Cont)

from interplanetary space. of a cosmic-ray particle. These asymptoticdirections are given for each grid point for specific rigidities above themain cone cutoff rigidity. The table of vertical cutoff rigidities containsthe geographic coordinates and L value of each location together with themain cone cutoff rigidity, the Stirmer cutoff rigidity, and the effectivecutoff rigidity. ,,

Unclas!s:ifiedSECURITY CLASSIFICATION OF THIS PAGE(Whýn Doee Estertod)

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Preface

This is the fifth in a set of reports presenting, in tabular form, the iesults

of utilizing high speed digital computers to calculate, by the trajectory-tracing

method, the motion of charged partic'es in a mathematical simulation of the

internal 2eornagnetic fieli. The pr ;pal results of these ertensive calculations,

which have been made over the past 15 years. have beer the determination of the

geomagnetic cutoff rigidity for soecific locations an the earth and the deternina-

tion of the asymptotic directions of the cosmic rays arriving at these locations

frcm specific directions,

It is the intent of the authors to assemble these values in a group of reports

so that they will be available to the scientific community both for analysis of

scientific data and for comparison with other similar values that may become

available by more sophisticated methods. The first four reports in this set

presented various tables of asymptotic directions and cutoff rigidities for Epochs

1955 and 1960. This report contains *-bles of trajectory-derived asymptotic

directions and vertical cutoff rigidities for a world grid as calculated employing

a geomagnetic field model formed by the international Ceomagnetic Reference

Field coefficients with time derim atives appropriate for Epoch 1975. 0.

3

AlI FOICD (I) JILM 1), 1975--475

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Contents

1. :NTRODUCTION 7

2. COSMIC-RAY ASYMPTO'IIC DIRECTIONS 8

3. VERTICAL CUTOFF RIGIDITIES 14

REFERENCES 17

APPENDMX A: Table of Asymptotic Dir-ctions for the World Gridas Calculated Utilizing the International Geo-magnetic Reference Field far Epoch 1975.0 21

APPENDIX B: Table of Vex tical Cutoff Rigidities for a World GridCalculated Utilizing the International GeomnagneticReference Field for Epoch 1975.0 155

Illustrations

1. Illustration of the Definition of the AsymptoticDirection of Approach 12

5

BLn-o FTU

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Tables of Asymptotic Directions and Vertical Cutoff

Rigidities for a Five Degree by Fifteen DegreeWorld Grid as Calculated Using the International

Geomagnetic Reference Field for Epoch 1975.0

I. INTR(ŽI)CTIO%

The knowledge of the asymptotic direction of a cosinic-ray particle and bhe

cutoff rigidity of an observation point on the earth is often npcessarv and some-

times essential for a meaningful analysis of various problems in cosmic-ray

physics. Tie asymptotic direction of a pfrticle having a specific rigidity is the

direction in interplanetary space from which the particle comes prior to its inter-

action with the earth's magnetic fields, and is a primary means of relating cosmic-

ray intensity variations at the ea-"th with the direction of these particles in inter-

planetary space. The cutoff rigidity of a specific location on the earth is the

rigidity below -which cosmic rays are inac2cssible to that location.2' 3

Since both the asymptotic directior.s and the cutoff rigidities are a function of

geographic location, zenith and azimuthal angles. and the calculation of these

values involves considerable computational time, it is impractical to determine

(Received for publication 2 April 1975)

I. McCracken, K.G. (1962) The cosmic-ray flare effect. 1. Soene new methods3f analysis J. Geophxc, lies. 67:423.

2. Stbrmer, C. (1930) Perlodische Elektronenbahen im Fi-'ie eines Elexnentar-magnetedi und Lire Anwendung auf Briiehes Modellversucne und auf Eschen-hagens Elementarwellen des Erdxnagnetismus, Z.Astrophys. 1:237 -274.

3. Rossi, B. (1940) System of units for nuclear and cosmic-ray phenomena,Phys.n N t. 5T:G6G.

PRECDII PACE BWLAN-MW FUMED

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lit, n-! }c-o) it 0Th- atnf lirectrons on the earth.- . v, -, - " .f Ai " <'f, (' : - i n :u ,t rs has allow4'edw a

I -1 1 A. r 1 t' ,- A I al -,Il it i n• to¶ h - r ,a,1e , \ ith ' 'st of thuse calculatior.n

ix.:'. : i r fir l s:i Ž¶:Ivs at- f''•Ži f-- rrax- satirns.

-- r !n' .2. !r ' mute tioe as,-,'n.ptotic,

-',- ." . 1 .... ,ral ,-an2

*.. .. V .* ¼-*.'h-, " t,'l•' the re, ac to r

" r t . i j '. , l" , n 1! 11 eot :):-i-, ar'il% '1' a r7 ie , "' 4s -5 ) analysI 's. 13-! 20

! .. '" I' .',A" " ork a have :: 711arlre I a c "or oisite listinn of all locations for

, 'a "i .t - :T .- , :7r;'r- e r)f this set of nublications

"iistzn-s of as tptotic directions and cutoff rigid-

"If, . in.. 1 a-rn t tr e "Icrv utra -inc- :cethod. The first four publications

-af'-i -e resultl on ,he extensive cutoff rii-dit2t calculations

-- te . an I .E'attn F- o(- h 1155. 0) intermnal eoot>acnet ic field

Z- rel, , ;.ell a, a s-.-atler Set of results obtained usinr- the Jensen and Cain

* 1 6).01 e, ,,",ef..cients. 1 fT ii rep-rt ontains the asv;>- ptotic directions.

ý, n ienio e r-', 0. .a ria cci " ith .:,rd Dn ints 5 ie1 -,rees in latitude and 15

- 'to .- as al-ulat, I ulili in•2 the International ('eontacnetic Refer-

e'::,, '•i'' ii , *'flt t-:,.: - ier;vat',-'e. aipl i ( so that the coefficients for the

fe' i -o'nel are ainro.-riate for a V-75.0 1-hooch. These asymptotic directions

are jive.- in Appenixx A. with a su:x.rnarv of the vertical cutoff rizidities for each

of the wor",t '"ri- hlcatiors j'",en in A.ppendix B.

2. COSMI(R %I XS)Mr•TOTT: l)IRECTIONS

T-n the "ariq,,- t.ujies of COsmic radiation, it is often necessary to know the

-lirection (! oartcle nmotion in the interplanetary magnetic field near the earth

in order I.. relate the intensity observations at a specific location, azimuth, and

zenith: a.. ile on the earth to an interplanetary flux. With this purpose innmind, the

concept cf asymptotic directions of approach has been developed over the years by

researcoers such as Nlalmofors, 28 Brunbery. 29,30 Brunbera and Dattoer3 and

"McCracken. I The asym-totic direction of approach defines the direction of a

velocitv vcctor in Leocenicic coordinates such that the direction of this vector is

narallel to a radial fromn the earth's center. A ,ctarate numerical calculations of

the as'mnt-tiric direction: of approach have long been advocated, 2&.32,33 however,

the earlier work was hninted to dipolar field models because of the complexity

tDue to the larae number of references in the above text, refer to the list ofreferences at the end of this report for spe•ific "if in..tin on reference-% 4 thru33.

8

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of the Prchlern , he a 'Ixe't of hii h-snered diatital con-.puters mari it

nosshble t,) consitr;ct relatively accurte athe-atirai -7.odels of the cenn..•'netlc

field an i to lrteirate the equation of chanced particle rotion in these magnetic

field r..odels. The standard rr-etho I for representin - the r: agnetic field is to

-jefi..e a .a., .- te ntia f!ury, tion t' in tern. -, f -a s •oner, cal harr:.onic exnansion.

In sn•,crr ,,. ',Sri P:a,.ue t:rim tri:;:n,::: it:

n-1I0re (:0 cos . - n sin rn.o I (cos

n7O trio n n0n, R

where j" Sr 7 are the Gauss efcnt,1-'.. (ens O) are- the paitially nor-n nr;alize'I lje e' r functions, and a is the a-,'erage radius of the earth. Thisrmezhod i -,rie- a-e'uately by Chapm..an and Bartles 136 is the method

c.--comronl. used fn-r constructin• models of the ceonmaznetic field. The n_.ainetic

fieldi verTr, I, -:.a" bhe ,7nonp'red t any r."oint where the potential function is valid

by obtainrinic !he derivati.-es of -he potential f ,unction:

Sg = "=I"•r~e o)6r s r

'¾ -I 'U (r,8,c)

£3 -I •U frO8.6)B6 - rsn '•r

The equation for charged particle motion in a magnetic field, in vector form,

is

In spherical coordinates this equation expands to the following differential

equations:

34. 1ory. F-.F. Vi,56'5 S'elected cosmic-ray orbits in the earth's magnetic field.

Phvs. HRev. l03:l1OW.

35. Lust, R. I 1957) impac' zones for solar cosmic-ray particles. Phys. Rev. 105:1827.

36. Chapman, S., and BIrtels, 1. (19511 Geomragnetisrn Vol. 2, Oxford Univ.Press, London.

• l l ll l . . .... • • lll9

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"r e "9~ 6

. fl 6n - ve l~ • . .. 7

2:" M 0 - r r tran

"r-- n-•-T - -9 -- - - r -c

Wj ET ½6 Ar unw^here.

is Ve

In these equations we use the followinoc notatinn-

B -.-osition vector of a cosnmic-ray particle

r radial distance froin the center of the earth

B c o-l at itude

6longitude .-easured eastward from the Greenwich mneridian

v ntagnitude of particle velocity

Vr. vesv velocity conmponents in r, 6, and 6 directions

c velocity of l ight

n" inertial mass of cosmic-ray particle, mc z c -

w-here m is the rest mass o

B vector magnetic induction in Gauss

e cosmic-ray charge in esu.

Since the general equation of particle motion in a magnetic field does not

have a solution in closed form, it is necessary to emnploy numerical methods to

detcr-mine th'P trajectory of a charged particle in the geomagnetic field. Withthe advent of high-speed digital computers, it becamee)hsihI7le toý obtain an

10

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a T Iratr . . i. , -'i r a s ,pecifie, 'i fiel, n-tiel. riqidity, and

.; ,. . . -;rljfjaton of the TR'in" ., Kutta iterationaiii. , -ecarne the standard method, of tracing

S -: . : ". ,- .a ieti- .field. In this prncess• a know-

!e t.'e-ihn t:c ;,:t<-. o i . -or-inrates of one nf)int on the traiectorw is

u i,,:.'. ¼, , , it . erential equations, to give the coordinates of a

.; .r:•r•t. , r ', .t,,r , lReneate-I an.-li-cation ..-C. suifficient n'ints

r: ,i i "' .- 4-:,. we -;t:1ize **e fas t tat the orbit of a ne-a-

t v tl : t l l l cutwarj fIro:-. the earth frItor- a snecific location

-to 1.re:, " I .e -itr-hi of a .,sitt'c narti!-'e of equal rigidit:;

ý', 1.- .* j t. atelv arriving at the same location in the sam-e

e"et' i that use the lifferential equatior. )f mrotion to

, -- a.t:l'me : the IeIon agne! c field bL using the

"-, .. u lave been nuhishe.1. ý-e'.eral times and will not

,-., !o -4ese '

a- p tie ;* w• ,o ":regtrate the trajectorv utiliz.ng the rr. iinim num ber

o -a'cul irn This iv.onlves a co-mpromise between choosing t'"e 1aro•e--t step

-ze t,-, ':.'im-ize co" puter t

ir e anti thpe necess;.tv of using a small step size in

*t}e iv e-n:-t,'nress to keen the error within acceptable lit.its. For these

- aic.-',a1;n r,, the 1/75 world --ril, A we replace-i the library of step sizes Provid-38

ed in the original McCracken progran: with a computed step size that is between

1 :25 anti I ,50 of the distance traveled during one -,yration. In a uniform, field

the time tequired for one gvi' ation is

33.33 P 2-

3T. il•i. - 1951 .'i Arocess for the step-by-step integration of differentialeont.ionsg in. an autom-atic digit-A computing machine. Proc. CambridgePhil. Soc. 47.O6.

38. acCr"racken. K. G. . Rao, 1. R.. , .nd Shea. L .A. (1962" The trajectories ofcosmic rays in a high degree simulation of the geomagnetic field. M. I. T.Tech. Rept No. 77, NYO-2670.

39. S;hea, M. \., `-mart. I). F. . and McCracken. K. G. !19651 A study of verti-calyv incident cosmic-ray traiectories using sixth-degree simulations ofthe geomagnetic field. AFCRI. Environmental Research Papers No. 141.AFC'RL-65-705.

40. Shea, M,. A. , Smart, D. F. . lcCracken, K. G. . and Rao. U. R. (1968) Sup-plernent to IQSY Instruction Manual No. 10. cosmic ray tables - asymp-totic directions, variational coefficients and cutoff rigidities, AFCRL.pSec. Reerts No. 71. AFCRL-68-0030.

11

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A nere P' is; in (xts fA- i iý in nimt , 'n r' sec, an-H i~ sý tha. ratio between the

na -tli le an-I th le e ,)f i hi. if th.- list ,ance rave 'led tir ~j': a uvra -

hon is :tvidelt :,to 50 steps, trier, the stetp size, II, m urits of tit: , ;, a xi-• ::matelv

-•e t.he ear-tL; sna 1'. t' fie! s : n nt ' , w re ,):- nute'i the step lenrtlI

.or each tlunge Kutta iteration. sten. At each sae-n the ofelct-: the )article

,was ,hecke and if thef qurr-nt value n! p iiere,i Cr, the initial value by nore

tha;n I • 10 the interatxn,i was. ieclare. u-.a,-, eatable an:, the traiector-v re-

c.xv ateI witn -nPt C nretinus ite: aize - II ,i. in haT., th~e ,i !work9,befre the existence of the internlanetarv rT-aznetic

:i tl was the orýt' a r, nar-et pte was traced thr'ouah the eeo-

n. a ýnetic ftelI to a listan.e s':-xentv' ar fr,. the earth (selected as 25 earth

ra 1-i by M-(ra-ckeni that t'., effects of the Ceormaznetic fieli on the orbit became

essenti llx inziznn.ficant. At this noint the direction of !notion of the particle was

calculate I in tern-s of tht 4euocentric -oordmnate svstem-. as illustrated in Figare 1.

The aisLvn totic lattude , A, * s v ven by

Ssin v - t cos B

vn (ve CosS v sin C)2]} r

VectorAA

Stationi Meriiofl

%_ S'oTro I ccto't

Stttatoon LLtituo

SStafion Longitude

Figure 1. fllustratictn of the Definition of the AsymptoticDirection of Approach

12

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and the "asy-nrptotic longitude'. 4, bv

L'e - arc tan ve cos e'v; sine

In. i2 Vt ',fice c:urrent know..le.dge o. the magnetosphere and the rrcanetosnheric

tail, the original definition of the asvmptotic direction of anuproach has been some-

what modified to mean the direction (in geocentric coordinates) of the velocity

vector of the cosmic ray when it penetrates the mragnetopause or at some arbitrary

distance down the n-a•netospheric tail, For cosmic-ray trajectories with rigid-

ities far above the cutoff rigidity, the computed asymptotic directions of approach

at the nosition of the mlagnetopause obtained using, a nmagr'etospheric field model

andI those calculated using oniy an internal field are verN innilar. For cosmic-

ray traiectories having rigidities 2 to 3 CA: above the cutoff rigidity (or - 5 GV for

the very high polar latitudes), significant differences occur between the asymptotic

directions com:puted using only internal fields and those computed using magneto-

spheric m,:odels containing both the magnetic fields of internal origin and those due41

to currents on the magnetopause and the magnetospheric tail. Near the cosmic-

ray cutoff riLidity, the asymnptotic directions of approach of cosmic ravs with

rigidities of only a few GTV computed with an internal field, have relatively little

correspor~dnnce to those calculated using rnagnetospheric models.

The assmptotic directions contained in Appendix A of this report are intended

as a reference standard for Epoch 1975.0. These calculations were made using

the international ,eoniagnnetic Reference Field t model of the quiescent internal

geomagZnetic field with the time derivatives applied such that the coefficients were

appropriate for describing the geomagzentic field for Epoch 1975.0. The calcula-

tions were initiated at 20 kin above the surface of an oblate earth where the radius

of the earth r(initiaD is guiven by

r II bK -1 1cosA]k 1/ - 20.0~G(nitial) -ao s

In this equation b is the minimum (polar) radius of the earth (6356. 9 kin). E is the

eccentricity (E 2 6.725 X 10-3) and a is the average radius of the earth (6371. 2 kin).

Calculations were continued to a distance of 25 earth radii, at which time the

asymptotic directions of approach were computed. For a number of cosmic-ray

41. Gall, Ruth, Iimenez, .1., and ()rozco, A. (1969) Directions of approach ofc.mi. rn. fnr high .t e stations, J. G .E.,-s. lRes. 74:352; .

13

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stutiles these asym ptotic directitos are quite useful ,n as-ertainirn2 the amount

of 'ecn:at_$netic hetielint_ -5m ravys un'lerito be fore arricvinn at a specific location

on the earth. ' hesse tables are li•nite'l to the vertical ,'trection with 20 ;V as the

hii'hest rigiditv contained, Except for locations near the equator. hidher rigi -

litto:; A',hav- 5 aym-toti, t(reci,,r s for verticallv incident particles that approach

tIw x- t'c r;-l:al,

Ili ,ur research otilizung : .asvc:.t,)tit dlirectitnw ,f aiitoa-., for cos,:.ic-rav

studies, we fiuiI that tli' asvn:,ptoit i<. -i etions f v'. rtitallv inicijtcýnt particles

are a reasonable approxir:.antiun t, the entire aivsn!ptotic -one of aceptance ex-

.e!,t f't.' i itlitdsC a > 0 (V above the coScic-ra's cutoff rig idity of a specific

location. At rigidities where the :yvro radius of the particle is small compared

to the cad.ius of the earth, the trajectories of all other azimuths and zeniths

anctes are siu-:Itar to the vertical tralectory with a phase angle displacement

which accounts for the initial pitch angle. TI is is sometimes referred to as the,nc11s ~rteffect of the geor-magnetic field..

The asvniptotic directions o)f approach presented in Appendix A are at stand-

ardized intervals of 1 (A' from a magnetic riglidity of either 10 or 20 GV (depen-

dent upon location) down to near the mrain cone cutoff rigidity. Approxim-.ately

0. 5 6% above the r-ain :one cutoff rigidity, the ,eon-aznctic bending is more

extensive and asyvt;ntotic directions are given in 0. 1 (A intervals. Very near

the main cone cutoff rigidity, asymptotic d:rections are given at 0.01 CV intervals.

This report does not include the asynmptotic directions of the allowed trajectories

in the penumbra; however, the results cf the trajectory calculations at 0.01 CV

intervals through the penumbra, including the asymptotic directions for the

allowed rigidities, are contained on magnetic tape available through the World

Data Centers.

3. NERTI'%L CI.ITOFF RCGII)I'UI.S

Cosmic ray cutoff rigidities are obtained by determining the "fate" (whether

an individual rigidity has a trajectory accessible from infinity or is forbidden)

of cosmic-r', trajectories over the entire rigidity spectrum. Starting at a

rigid.ity hig' sbove the highest possible cutoff, cosmic-ray trajectories are cal-

culated at discrete intervals, decreasing in rigidity until we are satisfied that

the cutoff has been reachtd. As the calculations progress down through the

rigidity spectrum-., the results change from the easily allowed orbits to a complex

structure of allowed, forbidden, and quasi-trapped orbits (loosely called penumbra).and finally to a set of rigidities where the trajectories all intersect the solid

ea-th, As a res,..t of thes- tvne of traiectory calculations, we can define three

14

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distinct rigidities: the main cone cutoff. P IM), above which all rigidities are

allowed, the Stbrmer cutoff, P(S), below which all rigidities are forbidden, and

an effective cutoff rigridity, PC, which we have defined as[P (MbDPC = P (M) iP

IP fIs) ]

thus allowing, for the opacity of the -)enumbra. A letaile-1 definition of these

effective cutoffs has been pmblished, and the effect of different spectral slopes

and coupiingc functions has been investigated by Dorman et al.42 In the penumbral

reýion of allowed and forbidden orbits., calculations were mnade at discrete 0.01

CV intervals in an effort to define the structure within this region.

There is an inherent hazard in using the trajectorv-tracing method to deter-

mine the structure within the penumbra in that some of the allowed rigidities

may not be found due to a systematic lin.itation resultine from performing the

trajectory calculations at discrete intervals. In our work -we have made the

specific assumption that if a trajectory is accessible (or forbidden) at a rigidity

Pi, then this result is anplicablt over the intervals between P.i AP/2 where AP

is the size of the rigidity interval. However, we recog, ize that the penumbra

consists of a very complex structure of allowed and forbidden bands, and this

structure is most certainly finer than the 0.01 GV intervals employed. Consequently,

calculations down the rigidity spectrum at finite discrete intervals might miss

some of the allowed rigidities for a specific location and direction.

It is.difficult to be assured that the lowest possible rigidity which may be

allowed for a given loction in a specific direction (that is, the Starmer cutoff

value) has been preciselv determined. We have found that for complex penumbra,

extending the calculations to lower rigidities at smaller rigidity intervals, often

results in an additional allowed rigidity considerably below the previous last

allowed rigidity. This problem and the degree of confidence to which we feel

we have located the lowest possible allowed rigidity is discussed in detail by

Shea and Smart,

42. Dorman, I._ I., Gushchina, H. T. , Shea, M.A., and Smart, ), F. 11972)Cosmic Rays Fffective Cutoff Rigidities, Publishing House "Nauka",Moscow, 1.SS1R.

43. Shea, M. A., and Smart, 1) F. (1974) Tables of asymptotic directions, cut-off rigidities, and reentrant albedo calculations for Palestine. Dallas,and Midland. Texas, AFCRL Special Reports No. j75, AFCRL-TR-74-0159.

S~15

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Tie effect of the currents in the ::,agnetosphere and the magnetospheric tail

were not considlered in these calculations. The work of Gall etal, 44Smart et al,45

46ari Žc.art and >.itiea have shown that the inclusion of these currents and the

magnetospheric tail results in a sienificant lowering of the cutoff values at loca-

tinrs ffir which the internal fielI vertical cutoff rigidity would be < 0.5 CV', and

the-ef ;,-, :are -4houldi he taken when using these tables for these locations. The

effe:t- f these ei-e:nal -,)urice- would result in slight decreases (-0.1 GV) for

tI';-ationsw hOlere the vertica! cutoff rioidity calculated with the internal veornaz -

netic field ,nodet is between 0,5 and 2.0 GV. Little if any effect is found for

locations where the vertical cutoff rigidity is higher than 2.0 G-V.47

Vertical c, .ff risiltities for each of the world grid locations are given in

Appendix L ,';ach grid pocnt is identified by the geographic coordinates, together

with the L vI-ue calculated using the same field model utilized in the trajectory -

tracing proor an; ithat is, the IGRF 2 model). All L values were calculated for

an altitude cf 20 kin, consistent with the initializin, of the trajectory-tracing

technique. The various cutoff rigidity data for each location are in order of main

cone cutoff rigidity, P((MI, the St6rmer cutoff rigidity, P(S), the width of the

penumbra, and the effective cutoff rigidity, PC. All rigidities are in GV.

44. 1,11. Rt.. .- menez, ,nd (.,rncho, L. 196.) l Arrival of low-energy cos-mnic revs via the m-agnetospheric tail, .1, Geophvs. lIes. 73: 1953.

45. Smart, D. F., Shea, M. A.. and Gall, Ruth 119691 The daily variation oftraiectorv-derived high-latitude cutoff rigidities in a model magneto-sphere, .. Geophvs. Res. 74:473l.

46. Smart. IJ. F. . and Shea, M. A. (1972) Doily variation of electron and protongeomagnetic cutoffs calculated for Fort Churchill, Canada. J.Geophys.lRes. 77:4595.

47. Shea, M.A. and Smart, D. F. (1971) Calculation of the magnitude of thedaily variation of vertical cutoff rigidities and associated changes in theneutron monitor response for selected North American neutron monitors.12th International Conf. on Cosmic Rays, Hobart, Conference Papers-niversit- of Tasmania) 3:854.

*The abbreviations for the main cone cutoff rigidity, the Stbrmer cutoff rigidity,and the effective cutoff rigidity in this paper have been changed slightly to permitcomputerized headings in the tables. Earlier worn used the abbreviations Pm,Ps, and Pc for the main cone, Stbrmer, and effective cutoff rigidities respectively.

16

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References

1. McCracken, K.G. t19621 The cosmic-ray flare effect. 1. Some new methodsof analysis, J.Geophvs. Hes. 67:423.

2. Stbrnrer, C. (1930) Periodische Elektronenbahen im Felde eines Elementar-mnaeneten und ihre Anwendungý auf Brdches Modellversuche und auf Eschen-hagens Elementarwellen des Erdrnagnetismus, Z. Astrophbs. 1:237 -274.

3. ikossi, B. (1940) System of units for nuclear and cosmic-ray phenomena,Phvs. Rev. 57:660.

4. Freon, A., and McCracken, K.G. (1962) A note on the vertical cutoff rigid-ities of cosmic rays in the geomagnetic field, J. Geophvs. Res. 67:888.

5. Kodama, NI. (1965) Trajectory-computed vertical threshold rigidities for85 neutron monitor stations, Can. J. Phys. 43:836.

6. Kondo, I., and Kodama, %I. (1965) Geographic distribution of vertical cos-mic ray threshold rigidities. Proc. International Conf. Cosmic flays 1:558.

7. McCracken, K.G., Rao, U.TR.. Fowler, B.C.. Shea, NIA., and Smart. D.F.(1965) Cosmic ray tables (asymptotic directions. variational coefficientsand cutoff rigidities), IQSY Instruction Manual No. 10.

8. Shea, M.A. , Smart, D. F., and McCracken. K.G. (1965) A study of verticalcutoff rigidities using sixth degree simulations of the geomagnetic field,J. Geophys. Res. 70:4 117.

9. Shea, I. A., Smart, D. F., and McCall, John H. (1968) A five degree byfifteen degree world grid of trajectorv-determined vertical cutoff rigid-ities, Can..i. Phlys. 46:SI098.

10. Shea, M.A.. and Smart, D.F. (1966) Vertical cutoff rigidities in the southAtlantic. Space Research VI, ed. R. L. Smith-Rose. Spartan Books,Washington, n. 7 :177

11. Shea. M. A., and Smart, D. F. (1967) Worldwide trajectory-derived cutoffrigidities and their application to experimental measurements, J. Geophys.Res. 72:2021.

17

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References

12. Shea, M. A. 1 19469) A crumpir IOn s o1 0 heoretIci.I ;,ad exper`:,rent :1 ('osmý.i- r;- .'.equ tors. T. Geopbvs. Ties. 74:2407.

t1. Kennev, 1. - u g( er.. . Shea, x .. z. , rid n.1 rt. I). I-, E x',pe.. I p nremen-hi evilu•tion of virio rigidit.: molll I.Geophvs. e. 71ties

14. (a:rr:ich el, Ht I .ra " "h. '.A. SV ,- !. \ .. :La ý n. .. and lPeterson.11. ', . I!tit :\ttfi!iuu( : a!f ne::trao :: umtar . , , tn i; 'he ,' .osphere.(,n. I. P'hxis 4, :'100 ,.

15. (-,rrnichiel, If. Iierrovitch, N.. -eliea, - N I " id' n (1ri9II, Cosmip -r:iv lzilitude s 'r-ev' in Norff? :\rerir:v in, s;ilnrner, I j9 Can..* Phvs. 4.:2037.

.1(. Carmichael, t.. S;he; M, N.A., and I'eterson, .. V N,. f IIl I'I. ("osr ic-raz,"lititude survey in W\estern I ý A nd Ifa:.w:,ii in suninier, 19i66, (an. I.Phvs. 47:2057.

,17. Coetzee. W, V. , Konig, P. 11. , r . . , <toker. 11. I. . v:n der WValt.AX. .1. , and Vrekani. N. .1. (10701 (Cutoff rigidities and lat itude dependenceof muons at 307 gIcm2 in inclined directions. A.ta Phvsica. AcadentiaeScientiaru~i " Iungaricae 29. 1 Proc. I 1th International Con!. on<osmic Rays. Budapest 196

18. Sporre. B. , and P'omerantz. WA. (1970' Time dependence of the positionof the cosmic ray equator, Acta Phvsica Acaderniae Scientiarum Tlungar-icae 29. Suppl. 2 (Proc. 11Ith international Con!, on cosmic Rays, BudapestT' 9-, ):.545.

19. van der Walt, A. 1. , Stoker, P.!t. , ?!iiree, .. P. , and Coetzee, W. F-'. (1970)Latitude distributions of cosmic ray components at sea level and at air-plane al~titudes in the South Atlaintic magnetic anomnaiv, Acta P-hvsica.Academiae Scientiarum itungaricae _% Suppl. (Proc. 11th InternationalConf. on Cosmic FRays, . udaqpest 191591553.-

20. Kent, D. V. , and Pomerantz. 'I.A. 119711 Cosmic ray intensity variationsin the lower atmosphere, J.Geophvs. Res. 76:1652.

21. Shea, '1.A., Smart, D. 1.F, 'McCall, 1. R., and Gumm. B.S. (19741 Tablesof vertical cutoff rigidities for Epochs 1955 and 1960, AFCRL FEnviron-mental Research Papers No.493, AFCRl.-TR-74-C550.

22. Shea, M. A. . Srr.mart, 1, V.. McCall, T. H., and Gumm, B. S. (1974) Tablesof non-vertical cutoff rigidities for 76 various locations, AFCRL Environ-mental Riesearch Papers No.497, AICRL-TR-75-0008.

23. Shea, M. A.. Smart. D. F., 'McCall, .1. R., and GCmm, B. S. (1975) Tablesof Asymptotic Directions and Vertical Cutoff Rigidities for a Five Degreeby Fifteen Degree World Grid Using the Finch and Leaton GeomagneticField Model. AFCRL Environmental Research Papers No. 498, AFCRI-TR-75-0042.

"24. Shea, NI. A., and Smart, D. F. (1975) Asymptotic directions and vertical cut-off rigidities for selected cosmic-ray stations as calculated using theFinch and Leaton geomagnetic field model, AFCRL Environmental Re-search Papers No.502, AFCRL-TH-75-0177.

25. Finch. i. P. , and Leaton, B. R. (1957 ) The earth s main magnetic field-epoch 1955.0 . Monthly Notices Roy. Astron. Soc.. Geophys. Suppl. 7:314.

26. lensen, D.C., and Cain, .. C. (1962) An interim geomagnetic field, (abstract),.1. Geophvs. Ries. 67:3568.

%1

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References

27. fAGA Commission 2, Workrng Group 4 t 1C69) International GeomagneticziReference F-ield 1965.0, J.Geophys. Res. 74:4407-4408.

128, NlAimfors, Karl Gustav 11945) D)etermnination of orbits in the field of a mag-netic dipole w.th apphcations to the theory of the diurnal variation of cos-mic ridiation. Arkiv for 1:±tematik AFtronomie och Evsik 32A, No. 8.

2:. ltrunhierg. tKr'9st-Ake E1953) lxperimental determination of electron orbitsin the field of a magnetic dipole, VPart 1. Tellus V:135.

30. Brunherg, V. -A. (1956) Cosmic ravy in the terrestrial magnetic dipole field,'I ellus VIII, -2.

.II. pA runberg. Erist-Ake and )attner, Adam (1953) Experimental determinationof electron orbits in th,, field of ai magnetic dipole. Part II, Tellus V:269.

32. lern.itre, G., and " allart:,, M. .19-5!j) On the allowed cone of cosmicradiation, Phvs. Rev. 50:493.

33. 'VAlart:i, M. S. (l19i81 An outline of the Lheorv of the allowed cone of cosmicr-dition. TUniv. of Toronto Studies. . lath. Series, No. 3 .

34, Jory, F.S. (1956) Selected cosmic-ray orbits in the earth's magnetic field.P~hvs. Rev. 103: 106',-.

35. ILust, R. 11957) Impact zones !or solar cosm.ic-ray particles, Phys. Rev. 105:1827.

U6 "napian. " a, nd Bartels, .. (1951' Geoimagnetism Vol. 2. Oxford Univ.Press, London.

37. Gill, S. (195l) A process fur the step-by-step integration of differentialequations in an s--itomrlitic dtgital cimputing machine, Proc. CambridgePhil. ioc. 47 : P6.

38. McCracken, K. G., Rao, U. R.. and Shea. M.A. (1962) The trajectories ofcosmic rays in a high degree simulation of the geomagnetic field, 'Al. I. T.Tech. Rept No. 7?, NYO-2670,

39. Shea, M. A.. Smart, D. F.., and McN- racken, K.G. (1965) A study of verti-cally incident cosmic-raŽ- trajector es i.Sing sixth-degree simulations ofthe geomagnetic field. AFCRL Environmental Research Papers No. 141,AECRL-65-705.

40. Shea, M. A,. Smart. D. F. , McCracken, K. G., . and Rao, U. R. (1968) Sup-

plement to IQSY tnstructicn Manual No. 10. cosmic ray tables - asymp-totic directions, variational coefficients and cutoff rigidities, AFCRLSpec. Reports No.'1. AFCRL-63-0130.

41. Gall. Ruth, Jimenez, J., and Orozco. A. (1969) Directions of approach ofcosmic rays fo:' high 'atitude stations, J. Geophys. Res. 74:3529.

42. Dorman, L. 1., (.iUsl:china. F. T., Shea. M. A., and Smart. D. F, (1972)Cosmic Rays Effe ýtive Cutoff. Rigidities, Publishing House "Nauka",

43. Shea, M. A., and Smart, D. F. 11974) Tables of asymptotic directions, cut-off rigidities, and reentrant albedo calculati-ns for Palestine, Dallas.and Midland. Texas, AFCRL Special Reportc No. 175. AFCHL-TR-74-0159.

44. Gall. R., Jimenez. J. , and Camacho, L. (1968) Arrival of iow-energy cos-mic rays via the magneto.spheric tail. J. Geophys. Res. 73:1593.

19

.----- --------. -"-- ------- t----....... ----- - - - ,- .._•... .. .- "- -- • . .. """. .

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Referances

i,. Srmal., D. F. Shea, M.A,, and Gall, He'th ('969) The daily variation of"I tra•i-torv-derived hgh-lathtude cutoff rigidities in a mooel magneto-

sphee,. ,(eaophvs. ies. 74:4731.

4,i. Sm; rt. 1). '.. ,und .hea, M.A. (I'1 92' Dailv v:.riation of electron and protonj•eomagneti- cutoffs calculated for F.ort Churchill. (C'naida..1. (eoph.

47. Shea. M .A.. : Smart, ). D. ( 1971,0 Calcuilation of the -nagnitude of thedaly v,,riatxon of vertical cutoff rigidities and associated changes in thene'utron monitor response for selected North Amerinan neutron monitors,12th International Conf. on Cosmic H .vs, Hobart, Conference Papersft-iiverstT Tasmania) 3:5•.•

20

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Appendix A

Table of Asymptotic Directions for the World Grid as CalculatedUtiizuig the International Geomagnetic Reference Field for Epoch 1975.0

"Table Al lists the asvmiptotic directions for world Lrid locations with grid

points each 5 deerees in latitude and 15 degrees in longitude. The listings are

arranged by latitude with six longitudes to a page, starting with the northern

polar regions and decreasing in latitude to the southern polar regions.

The geographic coordinates are given across the top of each page with the

appropriate rigidity and asymptotic directions given underneath the cocrdinates.

Eacl listing continues with decreasing rigidity values until the first forbidden

orbit is reached, Theso forbidden orbits are desiirnated byv either an "R" or an

"F", representing reeantrant or failed-to-reach-a-solution respectively. The

rigidities are in GV, and the asymptotic directions given in geocentric coordi-

nates to the nearest degree with positive latitude in the northern hemisphere,

negative latitude in the southern hemisphere, and longitudes measured east from

the Greenwich meridian. Negative asymptotic longitudes indicate that the grid

point is in the Western Hemisphere and the cosmic-ray trajectory did not cross

the Greenwich meridian during its orbit from the interplanetary medium to its

detection point. Asymptotic longitudes greater than 360' are indicative of the

number of times the cosmic-ray particle crossed the Greenwich meridian during

its trajectory as it circumscribed the earth.

21

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-------- -- -~

-- - - -- - - - --

.. .~t .C. .o. . . . . . . . .

*~ ~ --- -S - -ofcfc-c- .-'-U-.-.-.-

13 . .- . . . . .

-- C'I

o a 4 f

-22

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Appendix B

Table of /ertical Cutoff Rigidities for a World Grid as CalculatedUtilizing the International Geomagnetic Reference Field for Epoch 1975.0

Tne table in this appendix summrarizes the vertical cutoff rigidity values for

a world grid with locations 5 degrees in latitude and 15 degrees in longitude.

Each of these values has been de.termined by the trajectory-tracing technique

utilizing the International Geomagnetic Reference Field 27 with time derivatives

applied so that the coefficients of the model are appropriate for a 1975.0 Epoch.

The format of this table is:

Geographic Location: The geographic coordinates of each gridpoint are given with the latitude as posi-

tive for the northern hemisphere andnegative for the southern hemisphere,and the longitude in degrees East ofGreenwich.

L value: The L value, in Earth radii, calculatedusing the International GeomagneticReference Field 27 (Epoch 1975.0).

P (1%): The main cone cutoff rigidity (in GV)for this location.

P (S): The Stbrmer cutoff rigidity (in GV) forthis location.

Penumbral width: The difference between the main conecutoff rigidity and the Storrner cutoffrigidity (in GV).

PC: The effective vertical cutoff vi.gidity(in GV) for this location.

155

"P�.ACDIDG PAGE BLAIENO 7• F 4WD

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T e iLfI 31

5u!q.q"Iq 07671E6TICAL CUTOFF RI;IDIOIES FOD OE otRL0 ;RID

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156

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TISL! at ICONTOSUEDI

GEOGRAPHIC L PE-WO SRAL

I .(NTIFICATIDk LITY. 10ONG. A1LUE P(M) P(S) WIOtH PC

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157

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7TA51 81 ICONTINUEJ)

CG EGR4PHZC L PE MJN NR AL

IDENTIFICATION L&T. LONG. 4iLUE P(1) P(S) WIOTH PC

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159

Page 160: S J - DTICunclassified 1 "-report documentation pager nstruct rnbefore comipleting form iatfcr1_-tr-75-,,185--- -, , '.-.-) tables of asymptotic directions and vertical cutoff rigidities

10ERA0PHIC L P(CNU '4'AL

0190PT I0' CI tION LA T. LONG. VALiA Pt01) P (S . 2.1CT P

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