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^m 
 
A TRANSFOmrATION 
 
 OF 
 
 HANSEN'S LUNAR THEORY 
 
 COMI'ARKn -VSITIl TIIK 
 
 THEORY OF DELAUNAY. 
 
 SOrON NEWCOMH, 
 
 SUrKUI.NTKNDKNT AMKKICA.N i:i'lli:.\|];|{l.S, 
 
 AIDKK HY 
 
 JOHN MEIER, 
 
 ASSISTANT AMKlilCAX El'lIEMKIUS. 
 
 57 
 
TIlAXSFOIlMATloV uF fl.WSKNS LINAK THEORY, 
 
 ■a 
 
 I 
 
 TIk- imni.Ticnl .•u:ni.utation ..r' rlu- iiuMiunlirios in tli,. uHMm's , notion (.x.-ruK-d bv 
 II.VNSKX was prolKil.ly tIk- ^TeaK-st st.-p taken in ivrmt tin,,... tuuanl pl.-nin^ tin- tl,.'- 
 ()iy ot tlie Immr i.ei-nirhatioi.s o» nn ac-iiiat.- nnnicrical l.asis. It uas tlu- sf.-j, nlii.-h 
 first reiuU.iv.l it r.-rlaiu liiat .my .Hsrivpancv betuecMi th.- tlM-..ntical an.l ul.st-nxl 
 values ot tlic ni..,,ualiti.-s pr...hi.-..-.l hv rlu- Min an.s,- in.m s.nnc utl,,,- caiiM. i],m). trr-.r^ 
 111 tli...ry. 'I1,e tlie-.i-.tical valii.^. f, nhicl, it k-tl nnist !..• .•unsidMrd tlu- nn.st a.vii- 
 rato wiiicli astmnonn- ij<»\v jj« .».s.>>t<e>. 
 
 Tlio only tlKM.iy wliich .-an f,,niiu-r<- uitl. IIanskn's is tliat of I )i:i,ai nav. H.^ro 
 tlie coodicicuts aiv .K-v<.],.j.<,.l In ,,,,-{.■> .-onv.T-in- s.. sl,,v,lv that sonu- of tlu- r.-s.ilts 
 are still ., little .l.Mil.tfnl. iiotwithstuinlin-- the -ivat .-xtent to which the apj.n.x- 
 inuition was eamo,!. It may U, expeet-.l thai the numerieal theory on whi.-h Sir 
 (JKOKcn; AiKV is now eu-ji-v-l uill form y^ an.,tluT step in advann-, in' which iiotldnjr 
 will Ije wanting- lor tlu- imijH.>t-s .,f accurate astruuoniy, so that three tlu-oiies of tliT- 
 hi-hest order (pf .-, -curacy will uhimately l,e availal.K- for the eonstniction of l„uar 
 tables. The work in .ple^rk.iJ UAw^r >rill uiitinishetl, the residts of jJAXsh.v aiul Dklai;- 
 NAY are the oidy ones now avaiiaMr^ 
 
 rnfortnnately. tlu- tlie-TV .,f FFanskn cannot I.e directly compared with those 
 whi(diliave precc-ded it. owin^r to fli^- peculiar form oi' the variables in .vhich the 
 co-ordinates of the m<H.n an- .-.xpres.,-d. In sayin--- this. 1 do not contest tlu- proj.o- 
 sition tliat this form h;is a<ivaiita:r».-.-i. l!ut, apart from the cpn-stion of its merits in 
 forin, it becomi-s important U> have the means of making- a direct comparison of Han- 
 sen's theory with that of hi> |.re.leees.sors ami c(daborers, who have e.\presse<l the 
 co-ordinates of the nu.oii .iirecfly in terms of tlu- tinu-. This has twice lu-en partiallv 
 done: by the writer in the 0.«»/./*. li^mlii^ for i86S, I (T(.me LX\"I, p. 1197,, ••""h 
 indepeiul(-ntly. by Schjki.lkkj-i.. itt a paper published in 1874 ])y the Danish A( ideniv 
 of Sciem-es. jioth dej.eiul on data for the transformation oiven by IIansk.n' 1 imself, 
 Avluch, thouizh tlu-y may b,,- ac<-iinite enou-li to -,nve an idea of the aj^reement between 
 the^ theories of IIanskn and 1»el4I-xay. camu.t be re^-arded as sulliciently precise lor a 
 satisfactory transformed theory. The object of the present paper is to^make a ti-an>- 
 formation which shall faithfjilly represent IIaxsen's latest theory, aiul be exju-essed in 
 Jirgumenls dopending- directly on the time. 
 
 59 
 
6o 
 
 TKANSl'ORMATION OF HANSENS LVSWs. THEORY. 
 
 I'm 
 
 v^ I. 
 i:\l'l!i:SSI()N OK TIIK MOON'S lAJNGITI UK. 
 In IIax-skn's tliLM.ry tlir iiuu.ii's louj-itude is re|»n.-^-i.j..-.l in tliu followlnj-' form. 
 
 I/, tli'.» luooii's moini jmniiKily ; 
 I/' . tilt' Sim's lui'iiii iiiitiiiiily : 
 c), tlic (listiuicc troiii the uniU- to tlif ]i('ri;:«'-' : 
 (,}'. tlic ili>\..i('.(! from tile ikmIc I(. the x'lar jM-ri'^iee; 
 T, the lon;4'ituil(' of tlic ] n tI ;:■(>(■ : 
 
 r. tlu; iH'ceutrii'ity of liic iiio'>iiV (H-liit. as ux-d l.y Hax-SKN ; 
 )iS.:, the Iliiiiscuiaii ptM-tiirliatioiis of mean aiK-maly: 
 .s'. tlie n.insciiiaii |icrtiirliatioiii> of liuitiKle: 
 I. tlie iiicliuatioii of the moon's orhit. 
 
 'I'hen |)Ut, as iiuxih'ary (|uantitu's, 
 
 ./ — elta (',// + i"'^.-), tlie true anomaly 
 
 tan 
 
 ., 1 
 
 I sin 2 (./ + o.>} + ' tail' I ^iu 4 /-^ «> — etc 
 
 fhe retlnctioii to the eeli[)tie; 
 
 ,,, tan 1 eos (,/'+ m) 
 
 I — snr 1 snr ( / + m) 
 
 — o" 397 ^i" 2 CO 
 
 — I ".198 sin (2//'+ 2 co') 
 
 — o".2S5 sin ( 2 ,'/ — 4 //' 4- 2 &J — 4 cii'X 
 
 the iiiei|Ualities of this reihictioii. 
 
 Then, for the moon's loiigitiido, 
 
 K-/ + ;x+ K-r I!- 
 The latitude, fi, is <;iven by the equation 
 
 1 
 
 1 
 
 sin /:/nsin I sin (/+ w) 4- -*. 
 
 In presenting' Hansen's results in the form <if a. complete and exact numerical 
 theory, several precautions have to lie taken, hi the first plate, all the results must, 
 so fur as possible, depend upon or be reduced to one and the same hcniogeiieous set 
 
i 
 
 TK.VNSI-ORMATION OF HANSEN'S LUNAR THEORY 
 
 6i 
 
 of elcnionts. Tn tlir next pliuv, tlu.s,. iiM..,unIiti..s wl.id, ..xpn-ss tl„, sulutiun ui tin- 
 prohlci.i ot tlii-ce iMMlios, nnisi.lcre.l as iniitcrial points, must 1... s.^arated fn.ni iin- 
 quahtu-s arisinj.' tVun. utlicr sources, sucli, tor instance, as tlie .listan.'c l,..tn-eMi ti.e 
 moon's centres offrmvity an<l fio-ure. and tiie eilipticity cf tli<. eartli. 
 
 Tliree values of tin; eccentricity appear in IIanskn's tlie(.rv and tables: 
 
 (1) A provisional or ideal <-ccentricity, with which fhe ine(Hialities w-re ori-n- 
 nally computed. " 
 
 (2) An apparent eccentricity, uliicli he found to represent the ohserv.-.l motion of 
 the moon's centre of (iuure, and used in his tables. 
 
 (3) A theoretical eccentricity of the true orbit described by the moon's c( ntre of 
 f^ravity. 
 
 Tiiese three values of the element are: — 
 
 (i) r — .05490079 
 
 (2) r = . 05490807 
 
 (3) '==.05489959 
 
 _ Accordinjr to IIanskn's view it is the third value which should be used in c,nn- 
 puthifT the moon's perturbations; ])ut as he actually used the tirst value, it is tia- on- 
 which we should employ in tlie transformation. 
 
 In the case of the inclination there are three correspondino' values, with an addi- 
 tional complication arisin..- from the (pu'stion whether we shall add to the inclination 
 Ji term in the perturbations, 2'.7o5 sin (//+ a,), havinj.- the mean arf^unient of laTitU(h- 
 <is its argument. 
 
 Omitting this term, the values of the inclination will be :— 
 
 (0 1 = 5^ 8' 48" 
 
 (2) 1-5' 8' 43".66 
 
 (3) I = 5" 8' 39".96 
 
 Here, again, it is only the hrst value with which we are con< ■ ; od iii the tran>fonna- 
 tion, because it is the one employed by IIanshn in coin[)uting '.; perturl)ations. 
 
 The IlanseiiiiUi perturbation >t6~ is ai xplicit function of 7, //', a) and co'. So 
 lar as the longitutle is concerned, our present [)robleni is to express./, R and R', and 
 thence L, as explicit ♦unctions of the above four quantities. If we put: — 
 
 2 =. f/ -}- uSz 
 
 Ci, f.,, ?:„ etc., the coefficients of sin „-, sin 2^-, etc. in the development 
 
 of elta {e, z), we shall have, 
 
 f=.^-{-Ci sin ^ -f (',, sin 2^ + etc. 
 
62 
 
 TRANSFORMATION OF HANSEN'S LUNAR THEORY. 
 
 If, thon, WO put // + mU tor ^, (lovclop in |M)\vei-s (»f «r5,r, call {'\ (f),, tlu* part of /'iii- 
 (lopcndnit of i/<'>:\ and (c, ,7)^ tlio (•(.(■niciciit id' {u<'^::)' in./; wo sliiiU have, 
 
 («', r/)„ rr // + '\ sin // + r, sin 2// -f- r, sin 3// + r, sin 4// + etc. 
 
 (/>,//), = 1 + r, cos // + 2(:, cos 2// + .V', cos 3// + etc. 
 
 1 . 2" . 3-' 
 
 (c, y).. = — ,, ''i f*ni // — ^ r, sin 2// — ^ r, sni 3// — etc. 
 
 I 2' 3' 
 
 (f, //);, = - ^ , ( , cos // - - (■, cos 2// - ^ T;, cos 3// - ftc. 
 
 -" »> *3 *• * J 
 
 (f,//), n-—'', sin // + etc. 
 
 etc. etc. 
 
 The coeilicicnts r,, r,,, etc , lU'c (Impendent o)i tli(! eccentricity. Tliu well-known ana- 
 lytical \aliies. and tlu' ninnerica! values obtained hy outtin;-' c rr .05490070, are: 
 
 ^., - 2 c - ' c'' + ^^ r'' = .10976024 = 2 2639",676 
 ''•= = 4 "' ~ 24 '■' + {h ''" - -^^-^^ -'^''-^^^ = 7 7^^"- 269 
 
 64 
 
 I 2 
 
 10 
 
 .> ,/l 
 
 96 480 
 
 '097^5 
 
 960 
 
 — .00017893 iz: 36". 907 
 =: .00000972 =: 2". 005 
 
 — .0000005 7 = c". I 1 S 
 
 \ 
 
 
 900 
 
 — .00000004 ■=. o .007 
 
 Tlie value of ;m5^ is taken, not from IIanskn's tables, but from liis revised results 
 {riven in the Ihirlff/uiiii*. They are found in I'art I, pp. 409-411, and I'art 11, pj). 
 224, 242, 25S, and 26S, and, for convenience of reference, are all collected in Table 
 1 of the present [)aper. In this talde are •i'iven alsd the powers ot' lu').:, the coinputa- 
 tions of which were ail made in duplicate, that of the scjuare bein;^' executed by t 
 inde))endent comj)uter.> 
 
 wo 
 
 We thus have all the data for the numerical value of f, the formula for which \> 
 
 Consider next the tirst term of K, which we niay call Ki. We have 
 
 (0 
 
 K, = — tan- 1 sin (2/+ 2 w), 
 
 which is also to bo developed in ])owors of Hf5,r. 
 
 ^ I'lMlcr lliin Ullf n I'lTciiii' is iniiilc \i> Hiiiiscn'n Iwo papers, Itiirleijunijihr lliioirlixcheu liirichnutiij tUr in dm Miindta- 
 filn toKji'iviiiKlUK Sliintiiijni, in the Ablmiidlunijni dir kiiniijlirh-mchsischen OeuUmUuft dcr ll'inKiiixdiafkii. Hand /A", Xl. 
 
TUANSI'OR.MATION OF HAN.SI:NS LI'NAR TIIKORY. 
 
 63 
 
 Tf WO .sul>Htitut. lur/ ifs v..,l,u. in h-nns of . ..hI ., .,,.1 dovel..,, in ....vc-rs uC . 
 
 If, = — tiin- I X 
 
 24 
 
 + .^c 
 
 :\ 
 
 12 
 
 ■sin (—2.; ■\-2(.i) 
 sin (- ^- _|. 2 o) 
 
 + 
 
 0- 
 
 (^=-s'0 
 
 'c-'+ „r'' I sill 2 0) 
 
 4 
 ■^' +16'' 
 
 j sin ( c + 2 «) 
 j sin ( 2Z -\-2c0) 
 
 + 
 
 + (^4 '■"- 24 '■ J'^'"( 4-4-2^0 
 
 + J^^^' sin( 5-- + -''^) 
 
 + ,6 '^ •'^i" ( 6c + 2 a)) 
 
 Tf, in this o(jniition, we snl.stitute for r and \ tli.-ir numorical valnos and tl.on 
 ddlorentiate witl, respoct to ,:, so as to ol.tain tl.. .•o.-frn^icnts of tl.o i^owers of h6: 
 
 luttmy 
 
 wc have 
 
 1m = 1{, „ + 17, , ^/A',: -f Ifi , (;/,"),--)-' -f otc, 
 
 'm.o = — o".oo6 sin {— fj -\- 2Go) 
 
 — o".942 sin ( 2 &») 
 + 45".62 7sin( // + 2 oj) 
 
 — 41 1".626 sin ( 2 /y-|- 2 &)) 
 
 — 45"-2''^i sin ( 3// + 2 ta) 
 
 — 4". 040 sin ( 4 ^y -)- 2 Qj) 
 
 — o".33S sin ( 5 // -f 20)) 
 
 — o".02 7 sin ( 6 /y + 2 &>) 
 
 K, 1 = + 000 221,2 cos ( /y-f2 0j) 
 
 — .003 991,2 cos ( 2 // -f- 2 f.)) 
 
 — .000 658,6 cos ( 3 // + 2 &j) 
 
 — .000 o;8,3 cos ( 4// + 2 w) 
 
 — .000 008,2 cos ( 5 ,*/ + 2 G)) 
 
 — .000 000, S cos ( 6// + 2 &)) 
 
 • 'TiiWfsof (his and tlio otlior ilcvcldiiiiiciils in lli.. (■Ili],ti.' niiilioii li,i,. ,m.-« ;riv.-n liy t'rof.-.s<.r Cayi.ky in flio 
 M,:m,ni:'< of Ihe Ittnjal Anlroiiumical XooWi/. \,.l. XXIX, l.nt il„. „buvc dLM'l..imiL>nt was .•xe.ntcl in.I.'|.rn.l.-ntly hefort) 
 till' iiitplicability of I'lolVusor Cavi.kv's loriMiilir wa.s ivniarkcil. 
 
64 
 
 \v< 
 
 TRANSFORMATION OF HANSEN'S Ll-'NAR TIIKOUY. 
 
 U, ... = — .0001 I Kill ( // 4- 2 co) 
 -f- .00399 sill ( 2 // 4- 2 f.i) 
 + .00099 m\ ( 3 // 4- 2 a)) 
 4- .000 1 6 sin ( 4 ^ + 2 cj) 
 
 li, :, = 4- .002 7 COS ( 2 // 4- 2 &') 
 
 -f- .0010 COS ( 3 /y 4- 2 <») 
 In the same way, jjuttinj,' 
 
 U..:=itan'i- I sin (4./ 4-4'«') 
 liuvc by siiltstitiiliii';' Inr,/' its viiliu; in ,;, and (U'VC'l(ii»iny in powers olr, 
 
 i 
 
 sill (4/4- 4 ^'' 
 
 1 1 
 
 ('■ sill (2 c 4- 4 m) 
 
 Puttinii' as betbro, 
 
 — 4r sin (3,~4-4<y) 
 
 4- ( I — 1 6 e") sin (4 ~^ 4" 4 <") 
 
 + 4 r sin (52 + 400) 
 
 4- ^- e" sin (6 ,^ 4- 4 go) 
 
 11, - 1:,,, 4- II, /M5.: 4- 1{,,, (;/(5.-y- 4- otc. 
 
 we iiml b\- snbstitiitino- the numerical vahies of I and r 
 
 K.J,, = 4- o".oo7 sill {2 // 4- 4 t.:)) 
 — o".092 sin (3 // 4- 4 &)) 
 4- o".400 sin (4 // 4- 4 '«^) 
 4- o".092 sin (5 // 4- 4 r«') 
 4- o".oi3 sin (6// 4- 4 ^) 
 
 — .000 001 ,3 cos ( 3 ^r/ 4- 4 '«') 
 4- .000 007,8 cos (4 // 4- 4 ^') 
 4- .000 002,2 cos (5 // 4- 4 Gii) 
 
 The terms of li.o (»'^c)- are less than o".ooi. 
 
 The coeflicient uf — s tan 1 in li' is, Avitli suilicient accnracy, 
 
 cos (/4- ai) [14- siir I sin" (/4- «))] 
 
 or 
 
 ( I 4- sin" I J cos ( f-\- 00) sin" I cos (3/4- 3 ^)- 
 
 V 4 / 4 
 
1 
 
 1 
 
 I 
 
 TRXNSI'OKMAiioN or HANSKNS \J\\U rilKony, 
 \W til.' (Icv.i.|.i,„.iits,,ft|„. ,.|li|„i,. „„„;,,„ ^,,. 1,.,^,.^ 
 
 C.S ( y-f ,o) = — '^ r-' CMS (- 2 ,• -f ai) 
 
 s 
 
 ' '" ( 
 
 •(IS ( — ,: -j- m) 
 
 -{■ ( \ — r- ) cos ( ;■ -f- ^)) 
 4- ('■— ■\''') ens (2,; + <o) 
 
 . 9 ., 
 + ^, '■• <'os (3 : 4- a)) 
 
 + ^■' cos (4: + f.>) 
 
 COS (;,,/■+ ] a<) — 
 
 21 
 
 (•- + 3"') 
 
 — ;, '• (■( IS (2-4- 3 <.)) 
 
 + (1 — (jr-) CIS f ; . . ;, M) 
 
 4- 3(' CIS (4:4- • c) 
 
 If WO repi.'S(..iit liy S tli(! (•..(■Ilici.-iii nf v ii, IJ , that is, 
 
 S — — tan 1 cos (./'4- ^') ; 1 4- sin- 1 sin- (./■4- a,)) J, 
 
 S = S„4-S, ^,r5,:4-S,(/.r5,;)-, 
 
 and suppose 
 we shall liave, 
 
 65 
 
 S„ — 4- .0000 :;4 cos (— f/ 4- r.)) 
 
 4" -^0495 5 ^'"^ ^' 
 
 — .0899 78 cos ( // 4- U)) 
 
 — .004936 COS (2// 4- (O) 
 
 — .000306 COS (3 // 4- &)) 
 
 — .000020 COS (4// 4- G)) 
 
 — .000030 COS (2 // 4- 3 G)) 
 
 4- .000 1 ;6 COS (3^-1- 3 t^) 
 4- -000030 COS (4 (/ 4- 3 ft)) 
 4- .000004 *■'"* ( 5 // + 3 &') 
 S, = 4" -0900 sill ( // 4- (,}) 
 4- .0099 sill (2 // 4- &>) 
 4" .0009 sill (37 4- co) 
 
 S, — 4- .045 cos ( // 4- 00) 
 
 4- .010 cos { 2 // 4- f«') 
 
 Mjiltiplying- these several exiiressions by I1an.skn'.s s, we find the value of .s' 8,„ etc., 
 given in Table 11. 
 2 
 
 #^:i-'*v.- 
 
wV**^-**': 
 
 55 TRANSFORMATION Ol' llANSICN'S LINAR TIir.OKV. 
 
 Collecting all tlio cooHirionts of the i...\vers ..f ^mV;, wc lind the following expres- 
 sions for the moon's true eeliptic lon-itii.le, as a function of /m^ ; :— 
 
 Terms Unliti mlrni n/nS:. 
 
 -}- 22639". 676 sin // 
 
 -f 776". 269 sin 21/ 
 
 4. ;/j".907 sill 3// 
 
 4- 2".oo5 sill 4// 
 
 -f o".i 18 sin 5// 
 
 + o".oo7 sill ()(/ 
 
 — o".oo6 sin (— // + 2 co) 
 
 (— o".C)J,2) . 
 
 : • sill 2 f.) 
 
 (- o".397^ 
 
 -f- 45". 62 7 sill ( //+ 2 f«0 
 
 — 41 I ".626 sill ( 2 v -|- 2 c.)) 
 
 — 45".2Si sill (3,'/+ 2 ^)) 
 
 — 4".o1o sill (4// + 2 f«>) 
 _ o".33.S sin (5//+ 2 a>) 
 
 — o".o27 sin (6//+ 2 (.)) 
 
 + o".oo7 sin ( 2// + 4 r*)) 
 
 — o".092 sill ( 3 // + 4 (->) 
 -f- o".400 sill (4// + 4 ^)) 
 + o".092 sin (5// + 4 <-«') 
 4- o".oi3 sin (6// + 4 &)) 
 
 — l".iQS sill ( 2//'+ 2 (o') 
 
 — o".285 sin t^// — 4,'/ H" 
 
 f«) 
 
 4w) 
 
 ('(icffic'u lit (if II '5,:. 
 
 (The ic. 111111:1 pilillls llIT ~i\ llhlrrs iirdrciiiiiils. I 
 
 -)- .109700,2 COS // 
 
 4- .007526.9 COS 2 11 
 
 4" .000536,8 cos ^n 
 
 4- .000038,9 cos 4// 
 
 -■f- .000002,8 cos 5// 
 
 4- .000221,2 cos ( // 4- - ^•') 
 
 — .003991,2 cos (2// 4- 2 f«>) 
 
 — .000658,6 c(»s (3// 4" - f'^) 
 
 — .000078,3 cos (4// 4- 2 M) 
 
 ~ .000008,2 COS (5// 4- 2 r,)) 
 
 — .000000,8 COS (6// -[- 2 <i)) 
 
TRAN'SroRMATION OF HANSEN'S LUNAR TlllCORV. 6? 
 
 — .oooooi,;, CDS (3// -f 4 (.)) 
 
 + .000007,8 (MIS (47 -f 4 G)) 
 
 + .000002,2 ('(ts (5^ + 4r,)) 
 
 + - .^, 
 I--.. =: — .054SS sill f/ 
 
 — .0075;, sill 2// 
 
 — .oooSq sill 3 f/ 
 
 — .ooooS sill 47 
 
 — .0001 I sii. ( // -\- 2 &)) 
 
 + ■00390 sill (2// -f 2 («)) 
 
 + .00099 sill (3// -\- 2 (<■>) 
 + .00016 sin (47 -(- 2 Mj 
 
 I..;, — — .01 8,^ COS // 
 
 — .0050 COS 2 /■/ 
 
 — .0008 (.'OS 3 // 
 
 + .0027 l'(»S (2// -f - &>) 
 + .0010 COS (3// -(- 2 &)) 
 
 'II1C several parts of this expio-^ioii tor L are i^iveu in Table II, oniittiiin- rlie fo]- 
 lowiii;;- terms, wliicli are, however, all inchuled in the coliinin i^'iviiiL"- the concluded 
 coellicieiits in L : — 
 
 1. The terms ot' L,,, explicitly liiveii in the tirst ol' the precedinn- c(jnations. 
 
 2. The exiiressions for //'V;, { 11 ''):)- X "^ ^„ (//'') .:)-'X 'm,:;- fi"d ii/'')-) X \<:.u 
 
 The values ot' die last three expressions are as t'ollows. the nuniliers within the 
 parentheses heiii;;' coetlicients of//, 7, m, and cv/, respecti\(d\- : — 
 
 » '5 „- X IL I 
 
 {,iS,:Yx^^2 
 
 {»'y:fX 1^,: 
 
 — .001 
 
 sill 
 
 (3, 
 
 1 
 
 01 
 
 
 
 \ 
 
 — .002 
 
 sin (0, 
 
 ^ 
 
 
 
 — 2) 
 
 — .00 1 
 
 sin 
 
 (2, 
 
 I 
 
 "1 
 
 0) 
 
 + .001 
 
 
 (', 
 
 2 
 
 2 
 
 2 ) 
 
 + ■0'^3 
 
 sin [2, 
 
 O 
 
 — 1 
 
 2 
 
 -\ \ 
 
 + .001 
 
 sin 
 
 {2, 
 
 — I, 
 
 - 1 
 
 0) 
 
 — -005 
 
 
 (-^ 
 
 2 
 
 "> 
 
 2 ) 
 
 + .002 
 
 sin (3, 
 
 O 
 
 — 1 
 
 -^ 
 
 2 ) 
 
 — .002 
 
 sin 
 
 ( *-', 
 
 o 
 
 0, 
 
 -^) 
 
 — .020 
 
 
 (3. 
 
 1 
 
 
 
 2 ) 
 
 + .002 
 
 sill ( — 
 
 I, 2 
 
 c 
 
 2 ) 
 
 — .004 
 
 sin 
 
 ('. 
 
 n 
 
 0, 
 
 2) 
 
 — .005 
 
 
 (4. 
 
 -> 
 
 T 
 
 > ) 
 
 + .(304 
 
 sin (c. 
 
 '> 
 
 -» 
 
 0, 
 
 ^ 
 
 — .002 
 
 sin 
 
 (2, 
 
 n 
 
 0, 
 
 2) 
 
 — 002 
 
 
 (.- 
 
 I, 
 
 4, 
 
 0) 
 
 — .002 
 
 sin (2, 
 
 _ |, 
 
 4, 
 
 -^ ) 
 
 -f .002 
 
 sin 
 
 (2, 
 
 2 
 
 4, 
 
 -2) 
 
 + .002 
 
 
 (4,- 
 
 I, 
 
 4. 
 
 0) 
 
 — .002 
 
 sin (3. 
 
 ^ 
 
 4. 
 
 — 2 ) 
 
 + .003 
 
 sin 
 
 (3, 
 
 — 2, 
 
 4, 
 
 --) 
 
 + .001 
 
 
 (.i, - 
 
 I, 
 
 4. 
 
 0) 
 
 — .002 
 
 sin (4, 
 
 -^ 
 
 '>, 
 
 — 6) 
 
 + -003 
 
 sin 
 
 <4, 
 
 •^ 
 
 4, 
 
 -:^) 
 
 — .003 
 
 
 (4. - 
 
 '1 
 
 6, 
 
 - 2) 
 
 -• .002 
 
 sin (,■', 
 
 -<j, 
 
 C), 
 
 — 6) 
 
 •j- .002 
 
 sin 
 
 (5, 
 
 
 
 4i 
 
 --^) 
 
 + .016 
 
 sin 
 
 (5, - 
 
 T 
 
 6. 
 
 -2) 
 
 — .002 
 
 sin (2, 
 
 -6, 
 
 4. 
 
 — 6) 
 
 — .001 
 
 sin 
 
 (1. 
 
 — 6, 
 
 4. 
 
 -6) 
 
 + •013 
 
 sin 
 
 (0, - 
 
 
 
 6, 
 
 - 2) 
 
 — .002 
 
 >i"i (3. 
 
 - 6, 
 
 4, 
 
 — 6) 
 
 — .001 
 
 sin 
 
 (2, 
 
 — 6, 
 
 4. 
 
 -6) 
 
 + .002 
 
 sin 
 
 ()•,- 
 
 T 
 
 6, 
 
 -2) 
 
 
 
 
 
 
 — .001 
 
 — .001 
 
 sin 
 sin 
 
 (6. 
 (7, 
 
 — 6, 
 
 — (^, 
 
 
 -6) 
 -6) 
 
68 
 
 TRANSFORMATION OF IIANSKNS LUNAR THEORY. 
 
 Til T.-ililc II tlic (•(tliiiiiu "Sum'" contains tlic sums of tlio torms actuallv iriven in 
 the pivccdinn' coluunis of the talilc 
 
 TIk' uc\t column ^ivcs the com]ilct(' cocllicicnt of cacli term in the ecliptic lon^i- 
 tmle. and is t'ormed l»y addiiiu' to the column "Smu" the omitted ti-i'ms just referred 1o. 
 
 The last c(dunui j^ives. for the larger terms, the elements which the\' principally 
 contain as factors. If these; elements he chaniied, the coellicients nuist he chiiniied by 
 corresponding;' (plan titles. 
 
 vS 2. 
 
 IJKDrCTIOX OF THF, IMM'.CIvDrNd KXIM.'KSSIOXS TO ('XFFOini KLK.MKNTS, AND 
 
 COMI'AHISON WITH I>KI.ArXAV. 
 
 The coeHicients of the precediui>- incfpndities contain as factors certain elements 
 for which different investigators adopt ditl'ereiit values. It is essential to a (dear pre- 
 sentation of results that they should l)e reduceil to a uniform and W(dl-define(l set of 
 elements havinii- j^iveii v;diH-s We tlierefoi-<' coinmeiu'e hv i-educlnu' tin; theorie.s of 
 both Han.skx and Dki.ai NAY to such a system. The (dements principally referred to 
 
 are 
 
 mam 
 
 (a) The ratio of the mean motions of the sini and moon, 
 
 (fj) The lunar eccentricit\'. 
 
 {)') 'Hie solar paralla.K. 
 
 ('M The solar eccentricit\-. 
 
 (f) The iiudination of the moon's orbit. 
 
 Iveally, all tlu'se (dements are coiitaiiieil in all the ineepnilities in a very complex 
 ler. Ihit there is so little doul)t about their true numerical vahu's that it is only 
 necessary to take account of their (dian.u'es uheii they appear as factors in coefHcients 
 of coiisideral)le man'uitnde. The extent to whiidi ea(di tei'm is affected can l)e nai^'hly 
 seen from its analytic e\pressi(m -iveii by 1 )ki..-.i:nav at the end of hi.s n,orir du 
 Moitniurnl <lr la Liit/r, 'i'onie II. We take up the several elements in oi'dei'. 
 
 {a) Untiu „f iiH'ui/ iiHiliniis. This (dement is so certain that no reduction need be 
 made on ;U'counr of it. It is true that theoretical mof'ioiis of the lunar n(!(le and 
 peri<4('e imist implicitly enter in coniKction with this (dement. Mut. fn.m a row^h 
 examination (,f I Iansf.n's integration coeliicicnts on pp. 350-352 of his /fmirf/iirif/'^ J 
 
 do n..t flmik any (d" the laruer coetlicieiits will be aOected by as nuudi as ' of 
 »i • • , , . " 100000 
 
 tiien- ennre amount by any adunssible (diaiinc uf these motions. 
 
 (/;') Errndnvitii of mu,„>\ orhif. The eccentricities used by the tw., investijrators 
 
 are not directly comparable, but may be nio.st convenientlvVompared l)y nHhicing 
 
 each to the coetlicient of .7 in the expressi.m for the moon's' ecliptic lonnjtude. J)i.> 
 
 i.Ar.VAV uses Aiuv's value, niven in his la.st paper (.n the (dements of the nmon's orbit* 
 
 Il.VNsi N corrected his eccentri.dty for u.se in his tables, as alrei.dv mentioned. Tl 
 
 writer (^tained a sniall but w(dl-marked c.,rr(.ction to IIan.skn'.s yuiue from the Green 
 
 • .Nli'inoirs lioviil AHtioiKiiiiical Socioty, Vol. X.XI.X. 
 
 le 
 
TRANSIORMATIO.N OF ll.WSKXS LUNAR TIIF.DRV. 69 
 
 wicli ol)sorvi:tioiis 1846-74, niid tlic AVasliiii;,Hoii Dbscrvatioiis iS62-'74. Tlio four 
 values of tl"0 coi'lliciciit in (|ncstioii arc: — 
 
 AiiiV, used hy Dki.ai NAY, . _ . . 22639". 06 
 
 Hanskn, used ill 'riicor\-, .... 22637".! ^5 
 
 I Ianskx, used in TjiIiIcs, .... 22640".! ^ 
 
 CoiTcctcd \alnc found in 1876,* . . 226:;o".v8 
 
 Altliouj^-h tlicrc is 110 ivasonaMc doiiht that llic ('('ccntricitx- ..f 1I\nsi-:n's tables i-e(|uires 
 
 a iieg-ative coi-i-cction, it will Ix' adopted for the ]air])oscs of coinpai'ison Ijceause it is 
 
 tu)\v the standai'(l ot the cplicniei-idcs with which ^niis(M|UciU coinpai'isons unist Ik; 
 
 made. All the tei-ius ha\ iui;' c as a eoellieieiit, nnisi thci'cfoi'e hr' ineivased Itv tli(^ 
 
 factor 
 
 .00000728 
 
 zr .0001 ^20, 
 .05490 
 
 and those liaviii;^' r'-' l)y d(Uil)lc tins I'actor. The coctlicients in r nnist, in 1)i:i.ai;nav',s 
 theory, bo increased hy the factor 
 
 I .09 
 12639" 
 
 .000048: 
 
 {y) Solid- juira/ld.r. II a\si;n\s theory does not set out with a defiiute solar iiarallax, 
 but with a ratio of the in<'aii distanci's of the sun and ukmiii, which ratio ayain is not 
 the usual one, because IIanskn's h and n' aic the same functions ot' the motion of mean 
 anomaly that the i'sual '/ and n' ar(-(iftlu' sidei'cal mntinns. W'c must tl.ei'efoi'e adopt 
 an indirect pro: ess foi' iindiiiL;- thr i'clatii)ii n\ solar pai'allax and paralhn fie eijuation on 
 his theory. He finds that his thcoi'ctical coctlicimt has to be nniltiidied t)\' the t'actoi' 
 1.03573 b) make it aLi're(» with obseiAation: and then, in ^^ 260 of his l)(ir/c(/Hi/(/, he 
 deduces the solai' parallax 8 '.(1150. DividiuL;' this paiallax by the pn.'cedinj^' factor, 
 we coindude that the [larallax ol his theoi'\- is: — 
 
 8". 6085. 
 
 In turnini^' his tlieorv into numbers I)ki,\i".\ay used 8". 75. The parallax to which 
 both theorii's will be actualK i-eiliii'cd is: — 
 
 8". 848. 
 
 Hence, TIansi-.n'.s tei'nis hasiuL!' the pai'allax as a factoi- inust be inci'eased by tho 
 
 factor 
 
 .02785, 
 
 and Di'.f.AiNAv'.s by the factor 
 
 .on 20. 
 
 ('^) 7'lie solar <■( cri/tr/iifi/^ The solar eecenti'icitx' ot' 1Iansi;n\s tlieorv is: — 
 
 c' =: 0.01679226 (I'^poch !8oo). 
 
 J'ii|ii'r.-i piililislicil li,\ till' CiiniiiiiK.siiui or; llic 'liuiisil, (if \'i'mi,s. I'uit III. 
 
ro 
 
 TRANSFORMATION OK IIANSKN'S LUNAR Tlll'OKY. 
 
 !)i;LArNAv uses la; \'ki{Kiku'.s value :- 
 
 c' := 0.0167 7 1 06 
 
 (Kpdcli 1S50). 
 
 Ill strictness tlicsc twn values are not coniiiarable. owini;' to the diilerenl form of 
 Hanskn's solar tlieorv: l)iit since IIanskx ne;^lects |)erturl)ations of the earth's motion 
 in his liniar theor\-, it ina\ he assnnie(l that there Mill he no (lill'erence between the 
 form in which the eccentricity enters into the two tlieoi-ies. If we carry Lio \'i:iiHii;K"s 
 eccentricit\' hack to iSoo with his secular \ariatioii, we shall ha\e : — 
 
 0.01679228 
 
 (K[)(K'li iSoo). 
 
 This iiia\- he re^anlod as a!»olutely identical with IIanskn'.s value for tin* same e{)ocli. 
 So, ailoptiiii;' I Soo as the epoch, we lia\e oiilv to iiurease Dki.ainav's coeilicients in 
 <■' hv the hictor 
 
 .00002122 
 "707677^ 
 
 .001 205. 
 
 Or, we ma\- re(lnc(; Hansen's values to iS^o In- dividiiii'- them hv 1.00126s, when 
 
 0) 
 
 lie\' will lie comiiaraole wi 
 
 th I) 
 
 KI.Ai'.N.W S. 
 
 lie riieories o 
 
 f IIanskx and hKLAiNAV, thus reduced to a uniform and consistent 
 
 set of elements, are <iiven and compai-ed in Tahle III. I )i;lai:n'Ay'.s results are fre- 
 (juentlv doul)tt'iil h\- a small fraction of a second, owin;^- to the slow converi^eiice of 
 the seri<'S in powers of m, and the table has been arraiij^ed so as to show the extent of 
 
 lie iiiicerramtv tliiis ans^ui;'. 
 
 l'"ollowinLi' the indices expressing;' the arguments are LiiNen. lirst, Hanskn'.s coeiH- 
 
 cients formed from the \aliies in T 
 
 lie 1 1 b\' iniiltij)lyiiin' ii\- 
 
 lie a 
 
 ppidpriate I'actors tor 
 
 reduction alreadv ui\eii. Thev are onl\- iiiven to o".oi, but should the thousandth of 
 
 se 
 
 ccnids lie reqiiiivd they are readiK' obtainaljle. 
 
 'I'll 
 
 correspoiidiiiii' coeflicieiits of Dklai.'NAV are (lei-i\ed principalK' from his | 
 
 ire- 
 
 .sentation of niimerical results in the additions to the ( 
 
 niiUtitssinicc I 
 
 On 
 
 11 to 21 of that 
 
 paper are j^'iveii the si 
 
 /c.s T('i;iji.s tor 1869. 
 
 iinis of the terms in each coelHcient 
 
 which were actually computeil by him. The parallactic terms, as^'iven bv Delainay, 
 
 are s 
 
 till t 
 
 o lie multiiilied b\' 
 
 1 - ,\ 
 
 i + A' 
 
 A beiiiir the ratio of the mass of the moon to that of 
 
 the earili. rutlinu', with Hansen, A — , the coellicient 
 
 80 
 
 rected for this coeflicient and for diiferenco of element 
 
 will he 
 
 8i' 
 
 Tl 
 
 le sums, cor- 
 
 th 
 
 s, are f^wvw m the column 
 
 fli 
 
 I>('/((Hi/ni/ (\). Had all the appreciable terni.s been actually computed, tlie.se coetli 
 cieiits would have been the delinitive ones of Dei.aunay's theory, lint it was fre- 
 ([iiently tbiiiid that the terms, even of the ninth order, where the development c(!ased, 
 were still appreciable: it was, therefore, necessary to estimate the ))robable sum of the 
 
 0111 
 
 itted terms of lii"lier orders from the law of tl 
 
 K! series as (deserved in the terms 
 
 actually computed. These estimates can have no true niatheinatical fouudtitiou, 
 
TUANSI-ORMA riO.N OF IIANSENS LUNAR TIIKUKV. 
 
 71 
 
 1)Ocanso tlicre is 110 proof of tlio iictiiiil law of the scries.* .Still, tlioro is a liii)'li doj^Toe 
 of probability in favor of each one iicinn' ■•'■ '•'"^'^ " ''"'l*' ajipi'oximatiou to the truth. 
 A rigorous coniputation would probal)ly show that a majority dilfcred less than ' of 
 tlieir amount from tlie true \alues, though here and there one mij^'ht be found entirely 
 illusory. The coellicicnts of l(in<iitudc, nioditied by these estimated additions, arc 
 f>'ivcn !)}• 1 )Ei,ArNAV on paj^cs 38-40 of the paper rct'erred to, and are reproiluced, with 
 the necessary corrections for chaiin'cs of elements, in the colunm Dc/aiUKi// (2). 
 
 The ditference of these results, ^iven in the next colunm, is the correction 
 ai)])arently applied l»y Dklacxav for tlie uncomputed terms. It will bi- noted that we 
 liave no indei)endent statement of these tei'uis to refer to, ami can onl\' infer their 
 values fnun the ditfereiu'cs lietween the printed I'esults (1 ) and (2) 
 
 Finally, we have the difference, I/ai/^n/ minus DihuDitiii (2) >liowin^- th(^ dis- 
 crepancies still outstanding;- between the two theories l'',ach one can jndi^e foi' himself 
 liow far these discre[)ancies arise fi'om the uncertainty of Dklainay'.s senn'-empirical 
 corrections, and how far tVom errors in the two theories. 
 
 . One or two terms are woi'thv of a special examination, and amonii' tii(>e the par- 
 allactic C(piation takes the liist I'ank, a> upon it depends the value of the solnr [)ai'allax 
 to l)e derived from a ^^iven observed value of this ecpiation Arrani;'iiij.;' 1 )i:1jAII.nav\s 
 terms according- to the power of ///, which enters as a factor, the result will be that 
 <4'iveii b(dow under the head I',. Dklau.nav omits terms in y- after ///', ami t(.'rms in r 
 after in''. Corri'ctinii' the result i'or an estimated valm- of tliesi' terms, derived b\' in- 
 duction, we shall have those i;i\-en umler the heail !'_.. It will be seen that the terms 
 follow a nearly reyular law up to in'\ but that hi' deviates from this law. Assumin<>' 
 this term to be in error, and estimating' the valr ot' it and the higher terms as those of 
 
 a, ycomcitrical proi^-ression with the ratio we have tln' residts 1';. 
 
 Po 
 
 p. 
 
 Terms In //^ — 73". 1760 — 73". 18 — 73". iS 
 
 iir 
 
 Sum 
 
 \ -o^J-i — 34 -o 
 
 o 
 I 2 .01 
 
 34 -30 
 12 .01 
 
 III' — 12 .0082 
 
 w/' — 4 .()8i2 — 4 .50 — 4 .50 
 
 ///"' — I .9815 — 1 .89 — I .89 
 
 111^' — o .7122 — o .72 — O ."JZ 
 
 — o .48 
 
 III' — o .381 I 
 
 o .72 
 o .3S 
 
 127 .242- 
 
 I 26".c)S — I 2 7".oS 
 
 Our choice nnist lie between the results P. and 1';,. ff we ado])t the fornuir we may 
 add o".26 as an estimate of onnttiu"- terms <,^iving' : — 
 
 1' 
 
 r=-l27".24; P'=:J^P=:-i^4". 
 
 TO. 
 
 • W tiKiy lie iviMiirli.'d I1i;il in llir sni.'s U>v \\\i- .-niiliir ;iici'I,t;iI ion Ori.u \\1 I'l I (Iw Iniiis ol' ii lii^liii- (Udcf 
 
 ac'liiiill.v 111 cliMMHi' llii'ii- -^iK"! (liivt ll.v ciiiiliiir.v m ll ^liiii.ili' xvliiili wmilil li;ivr luiii tMiiiir,! rmiii \\\<>s,- of ;i liiwrr 
 
 (iidiT, 
 
TRANSFORMATION OV HANSEN'S I.INAR TIIKORY. 
 
 If we iulopi tlic latter we li;iv(! 
 
 P rz - i2;".o8 ; 1" = :,; 1' zz - I 23'. 94. 
 
 Si 
 
 Miiltiiilyiii;^- l»y the eoellicieiit i.oiu to reduce to the i)ariilliix 8".S4S the result will 
 be:— ' 
 
 (-^) -i-^5"49 
 (3) - i^5"-33- 
 
 IIankkn's coetHcieut, — i25".43, I'mIIs hi-tween these; results and may he regarded as 
 certainly corn.'ct within less than o".i. 
 
 The other term referred to is that ilependin<i' on the ar;^-ument: — 
 
 of which the principal parts of the coellicienr are, in Dklai'NAv's th(M)ry, — 
 
 3(1 order, 
 4th order, 
 5th order, 
 6tli order, 
 7th order, 
 8th order, 
 9th order, 
 
 Do 
 
 .10 
 
 - 5"-^o 
 + 10'. 1 5 
 
 + 9"-34 
 
 + 5"-^2 
 
 + 2".90 
 
 + i"43 
 
 Dhi.ai'nay seems to have taken i".i8 as the ])r<ibal)le sum of the omitted terms, 
 whereas they should have been taken as o".94 to agree with Hanskn. 
 
 S^ 3- 
 LATITLTDK. 
 
 Taking Hansen's expression lor the moon's latitude :- 
 
 sin /y = sin I sin (/ + gj) -f s ; 
 
 the first step is to form the expression sin i f -{- m) in terms of //, ro, etc. This may be 
 done in two ways. By the first we express the required (piantity as a function of ^, and 
 
TK ANMOkMATION < >K IIANSKNS 1.1 N.\K TllloKV. 
 tlK'H put <l I- /mS; r,„- ,/ ,.,,„1 .!..v,.|,,p j„ p.nvcis ,,(' i,<S:. I'.v tllr lll..,„y 
 
 lit' cllijitic 
 
 sill ( /'-I- r.. 
 
 Oj; 
 
 — , r sill I — > .; -[■ Ml 
 
 9210 ■ .^ • 1 / 
 
 >lli (- 4,; + M) 
 
 -^(~,:s''--k'o"';)-'^---^-) 
 
 -( - ,,'^ + l^ '■'') ^i" (- 2.: -fa;) 
 
 r sill r.) 
 
 + (3X4' 19^ '■")'^'" ^5- + -) 
 
 Si 
 40 
 
 r' .sin {6 .: + (>'') 
 
 + ,- ,, '- sill 7,r + m). 
 
 « 
 
 Tl" we now siil)-.tltiiii_' fVtr .-. »/ -|- >"*> :. t">r r its niiiiu'rical \;ilni', and 
 [mltiiii;' : — 
 
 i|i-\ fluli. 
 
 we sliall liave 
 
 ^in I .-in 11'+ (r = V --p F, ,><^ : + F_, ( i, <y:)- + F, (n 'y:)'' 
 
 F„ ( ill arc = — o' o I 2 sin ( — 3 // + .'.>) 
 
 — o -255 sin (— 2 // -(- r>)) 
 
 — 6' .96S sill ( — (/ -f m) 
 
 — ioi5".S34 sill f.) 
 
 -f eS447".342 .sin ( // + r>)) 
 
 -f- roi2".oii sin ( 2 // -j- 6,j) 
 
 + 62 .45S sill ( 3// + r.i) 
 
 -f- 4 .061 sill ( 4 /y + <i>) 
 
74 
 
 TKANSI'ORMATION t)!-' HANSEN'S M/N \R THEORV 
 
 (ill Jirc) (CoiitM) — + 
 + 
 + 
 
 o".2J2 sit) ( 
 o".oig sill ( 
 o' .001 ^•ill ( 
 
 
 F,, (ill radiusi — — .(.")0(> oooi sin (— i a -r ot) 
 
 — .000 00 1 2 sin ( — 2 ,7 -f «•>> 
 
 — .000 o^^3S sill (— 'J-^*^) 
 
 — .004 9249 >iii ''' 
 + .o.S9^352 sill ( 
 -|- .004 90<j4 sill ( 
 -|- .000 ;i02S >iii ( 
 -j- .000 0197 >iii I 
 -f .000 0013 >iii ( 
 
 i7 + «> 
 
 3, ff + 'y) 
 
 4 <•/ -f <y> 
 
 A> a dice 
 adoptcMl, 
 
 Then 
 
 -}-. 000 OOOI sill (6//-]-") 
 F, — + .000 0002 COS (— 3 fi -f <w) 
 
 4- .000 0025 cos (— 2 7 -f **'> 
 + .000 03 3 S CI tS [— ff-T f^} 
 
 + .089 4352 cos( .7 + *^) 
 
 + .009 S I 27 COS ; 2 '/ + <") 
 
 + .000 90S4CI.S1 3 5r4-i»> 
 
 4- .000 07 S8 cos ( 4 .*/ -r a>> 
 
 4- .000 0066 (MIS ( 5 .'/ -f ^) 
 
 4- .000 0005 cos ( 6 ft -r <") 
 
 !•'._, — 4- .(H/O 02 sin ( — // -r &-'» 
 
 — .044 yz sin ( '/-+- '*•''' 
 
 — .009 S I sill ( 2 // -4- <w> 
 
 — .001 3O .-in ( 3 V 4- oxj 
 
 — .000 16 sin ( 4 '/ — «^* 
 
 — .000 02 sin ( 5 </ ~ oi) 
 
 F;, iz: — .0149 cos ( 7 4- <y) 
 
 — .0065 cos ( 2 ,'/ 4- <^'* 
 
 — .0014 cos ( 3 ,7 4- OJJ 
 
 k upon the value of sin i sin (./'4- wj a >ec<.]i(i uieth*>fl ot" coniinitin;^- it was 
 as toHous. li"t lis put : — 
 
 <yi'—/—'i. 
 
 sin (,/'4- f'A ■= sin f ,7 4- ro 4- 6/} 
 
 — cos 'S /'sin (v + '*ij 
 -f sill ("i./cos {</ 4- <^'j- 
 
TRANsroKM Aiiox ,,|- || sssKNs I.l'NAR Tllli.KY 
 
 75 
 
 Fn.M. tl... ,,..,„..,•!,..] vain., of <\r .Wr.Ay .iv,.,, tl.- p.uMS uf tliis .,,nntitv w.r. 
 tonued, aiul tluMicc its cusun- and sine tn.n, the luimnla. :— 
 
 cos 'W = I — ■ 4- (>ti. 
 1.2 
 
 sin <S / ~ ,S / ~ ■' J.. ,,!,._ 
 
 1.2.3 
 
 'J'licsp ..xpn-ssions wciv fln-n nnilti|.li.Ml l,y t\w sine and cosinr ..|' (,/ + m). 
 
 'I"l'<' incan dilV.ivncc Ix'tuccn the cM-iHcicnts in sin I sin (,/ + r..) Innnd l.v fli.. 
 two nictlK.ds was l(.s> than (i.e.,;,. the lar^vst one hitin^' ".oiu. 
 
 Addiii-' IIanskn's s In this cxpicssi,.!! we havi- the vahu- <.!' sin //. 'I'hfu A itself 
 is (ihtaincil l.y the inrniiila 
 
 A zzrsiii /y-f ' sin' /5' + ■'' sin" /i. 
 
 The pniicipal |.arts,,|' /; aiv o-ivcn In 'I'ahl,- |\\.,f which the rulunnis .L-t'emnj^- to 
 IIanskn's tliciirx sccni lu nccil no cKijIauatiun. 
 
 vs 4. 
 
 iMJtrcTioN (»i-Tiii; i.ATin Mr; ani> comcaimson with kiilai nay. 
 
 .Ml the terms i\\' the latitude CMiitain the inelinatinn ol' the niDon's oi'hit as a factor, 
 and are therefore to he niulti|ilied liy such a constant coellicient that tin' |)i-inci|)al term 
 ot the latitnde shall aLiree with ol)>er\ atioii. 'The transt'oi'ined expressions of IIanskx, 
 L:i\-en in Talile i\', leail to a consistent theory in which the otdficient of the |ii'iiicipal 
 tenuof the latitmle is iS4oV'.24.S. The expressions ,,f Dki.ai xav also lead to a theor\-, 
 in which tliis coellicient is iSpx'.jo. i'lacli of these is to i)e multiplied li\- sncii a 
 iactoi- as shall reihice it to the \alue iniplicitl\- adopted in I Ianskn's tables. There 
 JIansk.n adopts : — 
 
 1 = 5" S' 39". q6, 
 
 which is less hy S'.oi than that of the theorw Hence, from this alone wonld tVdIow 
 the correction : — 
 
 — S".o4 sin ( ,/'+ '«')• 
 
 Hut, the tables contain, anioiiL;' the pei'Inrliatioiis, two terms which depend maiidy on 
 the same ariiinneiit, namely • — 
 
 2". 705 sin (./"J- a>), 
 wliicli, developed by putting;' // + 2 c sin // for./i appears as a perturbation, and 
 
 3'''.7o sin (// + f.)). 
 
„^^ linNSFOiniM-InN nl IINNSKNS I.i;N.\K lliroKV. 
 
 l.li..lM..nnl.u,.l,o,l,.. ..i.u.ni n,Hs.,r(l.u,v.u,l..r,n.i,v..r,l,. 
 
 „„„„, Tl.. >Hin of llu. Iir>t two ..xpivsMnn. l-m.- ^Irvlu,,,.!. l..rnHK. 
 
 _ 5".;, ID >ill *,'/ + ''') 
 -fo".29.:; sill M 
 
 — o".:g2 sill (J '/ + f«'.). 
 Ad.liii- tlir lliinl, 111'' I'nu ill//-}-'.' will l'."'"iiic 
 
 - l".6l(; sill I// + '.'^. 
 
 W,. .iv iw. ron..,.nH.,l .ill: iIh' -n.- in - .H'l ^ '/ f '.-■ 'Hi. ;:iv;il..r |,;.rt -f ih^ir 
 ,,,,,,,,,,,,,,,,,,,. ..,.n>i,l,.,va as ;i r'- l-'-tnH-.-H. .ln.M,Ml,Mi..iiv ul U^ 
 
 in.plirillv .•..il.i.H.l ill 111. Ml,l.. Inil iiu, h^lunuin,' U, ih. pn.M.m ut tliivr InMirs. 
 Willi the liist cinvctiuii tlu' t.-nn in '/ |- '•' Immm.uics 
 
 iS.jOi ■.'):o sill (.7 + '«'). 
 .vliicli i- tli.-.'H.'llinMil iiiipiinlK cMiPiiiMMl ill ll\N>r.N'sl;il.lrs. ,,,.,., 
 
 T„,lii> ,li,. writ.rtniMHl :. mnvrti..,, .4-. ,'.15 iVuni ( Mv-iiwi.-l, ;ni.l ^\ i.slini^'ton 
 ..h.Tvntioiis 1SM.-7.,. iMit it will 1„. ,v,;,i,n.i witliuut riiniiuv. II.mht ;i11 llir rnHh- 
 ri..|it> in 11ansi,n-> /A fis -ivn in T;ihl.' IW mv to 1h. iliniinis!,..! l.\ tlic tiirtor 
 
 .ooooSS. 
 
 iiud thoM' nf l>. l.M-NAV .IIV tn lie inrrc;l<C(l li\ tllf liu'tcr 
 
 .000020. 
 •n„. „.nns In , .•nnl -' ...v to !„■ iiiodilicd liy tlic snnic .■orniciMits .s in ill.- .-isr ..ftlic 
 
 l,,„,_,iln.l.'. TIm Iv h.iMn> wliicli will I- iiltrcrlMlilv uWrvwA liv tli.' cluin-v ..fr rm' 
 
 tlioM' (l(M)fii(lin:.;' nii <.> .■iiid : .7 -j- '■'. 
 
 'I'Im. 1 liii.'atiniis hen- iiKlicat.Ml liav not hccu niadr in tin- ivsnits. l.c-aiisc tli-y 
 
 iuv SI. >ii-lit, and alVi-cl su lew tiTiii^. tliat carii ,iiic ran make iImmii lor liiiiiM'lt. 
 
 I'lic ciluiini Ihhunniii ( 1 j (■..mains, as l.ctorc. tli.' mum ..I tli- l.aiiis a.tnally .•<.iii- 
 niitfd \)\ hi-.LAi-.sAV. am! -iv.-ii liy liiin in tin' Cuiiiniissiuins ilr-< I'viiij^s l.ir iSog. 
 
 In Volmiin Ihhniinni ; : i In- fli.a.'iit.- arc .•..iMvrt;'.! l.y the lii-li.'r Utiio, of wlncli 
 
 the value lias liccii .•stimal.Ml l.y iinlii. •lion, 1> K iN.v liinix-lf .li.l ii..t -i\«- tlu'Sf 
 iul.litiuiis,*!;.) that they liad to he cstiinatcl '.y llii' writer. 
 
 vN 5. 
 
 I'.\|;AI.I,AX. 
 
 IIwskn's tli.'orv Li'ivcs till- pi'i'liirliatioii^ of ilic natural jo-'ai'lllnn of tli.' 111. ton's 
 railiiis v.M'tor. wlii.'Ji aiv tin- n.'Li'ativ.- ..f tli.' pcrtnvl.atioiis of tli.' l..,^'antliiii sine 
 narallax. The valiif ..f ir. in sccnn.l.- ..I' arc, i> foiiinl in tlic l)iir/r</ini'i, I'art 1, pa^cs 
 409-41 1, ami i'art 11. paii'fs 224-226, 25S. ami 2OS. 'riic in.it.ii's parallax /i i> .u-i\cii 
 
 1)\- IIanskn uiul.T til.- form 
 
 . I) (, .,|-,. cos/) 
 
 l..n- sni y, -!<.-■ ^, (^j_^,:^ — '". 
 
11'! ANSI oUM.\l|(i\ oi' ||\Ns|:.Si's I.iNAi; l|||;.»RY, 
 
 n 
 
 '" "''''■'' " I- tll<' I'iMlillS nl' tllC ..artll lit IIm' lltilinl,. nf u|,i,.|, (llr >ll„. is s,f\.A\xA>l 
 ','"■ '"■> Hl.-.ll, .liMMIlrr il: l!„. 1Ln>,,m,, ll.ru.v. SvMrl, i-, ,|;ii;.,Vlll n, .h.|llliliull 
 
 ''■ ''"• ""•"" 'liMMiHT n{ tlir (,r,|ii,,.,rv il ri-s. " li is not. Ii.,wvcr. iHTf^-.irs' t.. 
 
 '''■''""■'■ ''"■ """ '" '' 'Ii"i' (l!i'-lly. Immmh-.. tlirv iiMv In. iiM.>I si,tUr;ict..nIv n.iii- 
 
 l""''''l '•> 'I"' ^"l"'- "I' til'' '•n:i>t;,n| mC |,,m|';iI|;|\ Iu w'j ilrli 'l i|,.\ l.^ni. 
 
 < 'liiiii.Uiiio' the loL:;irItliin> t,. luiiiii.ij (jiLiniino :iii<| >lfvci(.|iiii-- in |M.\\ri-- (.f ir, tin- 
 ;il)ii\(' i'.\|)i't's.si()ii ;^i\cs: — 
 
 >\\\ II 
 
 l'~ 
 
 I ) \ -l- r ('(IS / 
 
 r' I 
 
 r cos/ / ^,.- V 
 
 ;iiiil tlii'ii 
 
 , SIM'/) , 
 
 III (Ic\clu|)il|u' , !•,,> / i^V(( lii(ll|ip(|s of cniiilillt.-llinli wi fc llxd. iis ill lllr c i||| j ill t;i t inll 
 "I' til'' |irillci|i;il Icrill 111' llic liititiplr. 
 
 I. I'Vdlll ( '\\ I.I \'> IllMl-, \\c ||;|\,. 
 
 (•(.s,/ — 
 
 
 -1 .:■■ 
 
 cos 4 ,: 
 
 , ''^^5 I 
 + r ens 
 
 :v^4 
 
 ;iii(l then l)y siil)>titiitin^' // f- // '*> : i\>v : \vc Ii;i\c ens /■«lc\rln|)cil In iiiHl;i|i|cs .,1" //, etc 
 
 2. I'llllill"- 
 
 \vt' Iiavf 
 
 /~-.'/ + 'V 
 
 ciis/'zz ciis '"^y <'<>"i// — !^iii '\/ sill //. 
 
 I) 
 
 I lie \ nine (il w ;i- (1( ri\til li\- 1 1 a\S;-,n iVoin tlic Icii;.;tli ut' tlic >ccip]iil> iiciidnlnni 
 (I ■ ■ ' 
 
 Mini the (linicnsiiiiis ut' tlir ciirili iis iuiniil li\' IIksskl. The ili-i'ix.itinn i.■^ l:!^ i-ii in tiic 
 
 A^lruiKiiii'isclif Stichrirhliii, \ ulunii' X \ II. |);il;(.' .VJ<-'. 'i'lic <l;ila in. hie use nl' nn-: — 
 
 I), rjidiiis nl'cjirfli inidi r llic |i;i' illd aw sin s^' \ . . 6370063 nicti'cs 
 
 I*, Iciin-Hi ol'si'CdiHl^ ]i'Mi(liilnni miller s;iinc jiiii'.illcl . O'''. 992666 
 
 I 
 hi, mass 1)1 1I1C iiicinn • 
 
78 
 
 Tliti rrsiili is 
 
 TRANSFORM AlIiiN Dl ll\Ns|:NS I.INAR IIIF.OUY, 
 
 I> 
 
 liiy zz .'■'.J I 71 II ,U>. 
 
 !Ir j;iv('s ii.-- the rfsiiliiii:^' (•(nisliint pari nl liic >:iic ut tlic |iariillii\ 
 
 iiml tlic cliaiiL.'!'^ Ill fit'' ('oiistaiit |)ruiliircil li\ ->iiiall cliaiiL^'o in tin' data 
 
 Iiicrcax' (it 11""". I III I' \ai-if> tlic cdii'^taiit li\ 
 liicrrasc lit' loiK)'" in |> \ai'ics the (■iui>taiit Ii\' 
 liirrcasc dl' iiiiitN' ill <lciiiiiiiiiiattir III //' 
 
 rile ili'Vi'luiiinciit >iii)^rniiciitl\ 'nvi'ii jrails to a ruii<taiit i>t" 
 
 — O'.I I 
 
 4-0". 1 8 
 + o".i7 
 
 3422 .09, 
 
 a result (i".(); ;.''i'catfi' than tiial >taIiMl li\- IIaN'skN. 
 
 1 11 (•iiiii|iariiiL: iIm' iiaraliaxo nl IIanskn am! I >i;i,.m \ai tlii- milv clcnirnt wiiicli 
 will iiiatii'iall\- all'iTt the i'r>iill i^ tin' (■Mii>taiit ul |iaralla\: a ciiniiiai'isiiii nf tlio 
 (liricrciit \aliii's ni' flii> nut-taut, wliicli lia\r liccii rrci'iilU ohtaiiiril, will tlirrcrDrc be; 
 of intcri's:. Tlirti' ili>tiiirt inclliods of ohtaiiiiiiLi' this impoi'tant clfinciit liaxc iircii 
 apjilicil 
 
 ((»■). 'I'hi' thiiirclical iiiftlioil roiimlitl mi Kki'I.kk's third law lis cxpi'cssud in tlif 
 thi'orN 111' L:ra\ itatioii, and dt-rixi'd rniidaniriitalK Ironi tlir iMpiatioii 
 
 II II 
 
 -' = m + >r, 
 
 (I iiriiii;' the iiicaii distaiirc ol the niooii. uliirli is iiiiincdiatid \- coninTtcd with the 
 parallax: // thr iiuaii motion, oj' iIh- \aliii' of wliirli tin re is 110 doiilit, and /// and .M 
 the inassis nl'thc moon and earth, exiires.-i'd in ainu'oiirial 
 
 pnale units, the ileteiinination ol 
 
 whiidi is the nio>t doiilitliil part of the iiroldeii 
 
 (//). .Measures ol the moon's po-ition made at two dislant stations, and reduced 
 to a eoiiimoii moment. 
 
 (r). Meridian derlinalioii> of the iiioon maile al the same station, and reduced on 
 the li\potliesis thai the midisliirlied L!-eoeentric oi'liit is a i^reat cinde. 
 
 The last met hod is not w ell adapted to i;i\e a certain result, owiii;^- to the constant 
 errors with whiidi inuasiires ol' alisohite declinations are all'ected. ^\'e shall tlierct'oro 
 conliiie our consideration to the lirst two. 
 
 'I'wo deterininatioiis l»y method (i-ri. that ol' IIanskn, just (pmted, and that ol' 
 AiiAMs in the Mniitlilji Xnltcrs, \'ol XI 1 1, and the llritish Siiittkiil A/hkuhic I'or 1S56, 
 
 aiv a\ailaiile. 
 
 Id. 
 
 The data \\><cd li\- Mr. Ada 
 
 M.i are 
 
 I >, t'l'iim liKssEi., and iherelore the same as IIa.Nsk,\. 
 
 1',* ;,j-6 So 1 
 
 (J IMiLillsh teet, or 
 
 ///, mass III moon, 
 
 o"'.992 7i : 
 
 81, 
 
 piililisluil jiaiiir 
 
 riiis \:iliu' ill Kiiglisli led wiis Kiiiillvo.iiiiiiiniiiHlcil hy Mr. Adamj, liiniMir, not bcingoxiplicilly nuotuil in IiIn 
 
TK.\NSI„„M.\ri..\ ..!■ I, vNs,.N ,s , ,:n.\U TIII.oRY 
 
 with IIa.n.skn u.. |,,s„:_ .I^<IM„,,.^.: ._,,,. | „ .•un,p;,n. 
 
 79 
 
 |iiiif It 
 
 Clmii-.-iii |)-o, - - - cliin,-.. uf .T„ _- o 
 " " l' = -fo .040. •• .. _,/,o5 
 
 11 II ' 
 
 = I- '.5, 
 
 •( n 
 
 + o' ,26 
 
 ^ •?' — — iy •'- - II->.:n-s .,;„„. ,1,1. n..,l, ,1 ,.„.m...r 
 
 ;inn,MV ;"";,'^^,-"'";:";':'''7^- "•'•-•'••r- I^Nsi.:Ns..n,i,nl. M,n„ ,„■ ,i,:„ .1.- 
 
 '•';•'• '•'•;'""■ ""• -'l";> '""1: ..,• il .SH.:V nu.l A,.AMS ,0 II vvsKN's .1.,,. nl 
 
 iii^i to til., system aliv,i,|\ .•H|u|,t,.,|, i|„. ,vs„lt, ui|| !,,.;_ 
 
 Cnll^tiiiit (.iMiir p;irillla.\, 1 1 AN>|.;.S. ■^^2-".nq. 
 
 " " 11 » 
 
 •^I'AMX. ;i4^2 .13. 
 
 ('nllstailt nl' |.,irall,i\ i|,|.lt'. IIanskv. ;,.J-^2".2v 
 
 " Aham-. vp:? .2S. 
 
 'I'iK-cn.istaiit orn.(|„rtlni, jmni ,]„. si,„. ,,. ,|„. iMiallax iisi.|f is 4-,, i^- 
 
 //. TIlc llio.st ITrcIlt ilctcnililiatii.lis nf 
 
 llH' III, .nils jiarallas l»\ iiicasiirciiici 
 
 • 1 ,■ MI, M . , |'Mi,,ii,,\ n\ lllcasii|',.ill(|i| ;|i',> 
 
 ''•7' "' •^''•- '""•■'•^- '■^'" ''^ l- A. S. X.XXIl, „nl „f .Mr. >p,.>..m!Ih,| \\\IV) 
 
 '""'' •"•'■ t'"iii.l,.,| HI, ( '..ij,,. nliM-natioiis ;,,„! |„,tl. lend t.. a .•.■ii>iai,l of 
 
 It ,s not ilistnirtiy statnl wlu.tlH.r this i> tl,.. ..unsfaiit nf ,|„. parallax Itself n, of i^ 
 sine Ml'. P.UKKN's iiitrndurtinn ,1. ... |,,,, ,p, ,,7.s,.,.,i.. to iniplv that 1,0 u.rA Mr 
 Adams s expn'ssion l,,r sn,.. |,,.,,allax as tl,.. parallax itsril i„ n-iliicini,' thr Cape nl.sn- 
 
 vati.ms. Ilut.ii, t|„. ivihirti tl,.' (iivMiuirl, Ml,>MNatiM„>. In a pplics A l>AM,s's ,,,1- 
 
 rcctioii t(. the parallax ,.f Ann's lii„ai' ,v,li„tiM,,.. u|ii,.|, nu,.. il,,. p;in,llax itself 
 To put the matte,- into a.iuihe,' shape: ( )„ p. , ,,, )\y, D.^kkn has 342j".33 us the con- 
 stant of parallax. On p. i^j he h;,s a c.i.st;,,,, ,,,ri,.etioii of o".r,S to the Aiuv-I'lana 
 parallax, of whirl, the constant is 34.M .So. uhirh j-ives 3422 .4.S as the constant of 
 parallax. 
 
 We shall probably make a near appi'.,xiniaiio„ to the truth l,v a.-^sni,,!,,-. that .Mr. 
 r.KKKN'.H mean provisional co,,.stant was 3422 .40, a,,.l a.s h,,. (Ieiii,ce,| a co'nvciion ,,f 
 + f"' .38 tliLs would j4i\-e IIS his result : — 
 
 ('oi,sta,,t of parallax, . 
 Constant of si,ie, 
 
 - 3422".78 
 3 42 2". 62 
 
 Mr. Stonk also linds a correction of + o".3S to .Mr. Ada.ms's i)arallax. This 
 would !^i\e : — 
 
 Cons[ai,t ol" paralhux, . 
 Constat, t of sii,e, ... 
 
 - . 342 2".86 
 . . 3422". -o 
 
 The ovidcnco is thcrefoi'e ii, fasorof a positive eoi'i-ection to IIanskn's constant- 
 hut, in accordance with the practice in other parts of this paper, the results as printed 
 are all founded on Uanskn's fundamental data. 
 
^ 
 
 'J^ 
 
 So 
 
 TRANSKdRMA I li)\ oF IIAS'SKN'S IJ NAR rill.DRV. 
 
 Ill rllc Tillilc \' till' ciilllinllS (•(ilil.lill- 
 ) 1 
 
 (i). The viiliic (if • - - .,.( I + '' C's,/'), cxprfsscd in sccoiiils of arc. 
 
 )r. 
 
 (2). Till' i»!'(Hli!cr (if tills (|iiaiitity Ky — /'' + ,, 
 
 (3). Tile (■(icliiciciils fdi' IIansi-.n's sine parallax, fdniicil Iiy addiiiL;' ' l) ninl (2). 
 If the |iai'alla\ itself is rci|iiirc(l, it may lie fdiiiid li\- addiii,:; flic rcdiictidii fniin 
 tile siiu- to tiie parallax iiscll', iiaiiiciy : — 
 
 -|-o".i5; +o".oJ5 cos // 
 
 -f- o".004 CDS '// — 2//' A- 2 10 — 2 m') 
 4- o".oo4 cos ( 2 // — 2 //' + J <•' 2 m'). 
 
 (4). 'I'iic cdclliciciits (if ! »i:i.Ar\Av's sine parallax. >o far .as actually coiiijuitcd by 
 liini. A> lie stopped at the tci'iiis of tlu' fifth order, tlic liiiii(lre(ltlis of scchhhIs are not 
 always dcfuntiN-c. 
 
 (5). The >aiue, with tile addition of (piaiitiiies e>tiiiiatei| hy iiidiictioii to reprc 
 
 sent the omitted t(.'niis of liiLiher orders. 
 
 (6) The correctiniis applied in the precediiiL;' colmmi to olitaiii the most pi'olia- 
 hle \ allies of the co<d'licients. 
 
 (7) 'I'he deviation of' IIansi.n's ciwtliciei!t< iVoiii the second set ol' 1 >i;lai'nav's. 
 As some of 1 ))■,!. AlN'\\'s teiiii.^ ai'" doidifl'ill tVom the iii-ufli'Mclif coiivei'^.i'eiice of 
 
 his series, the coeilicieiits of' .Voam-'s parall.ax. foimd in the Mmithlii Xcticcs II. A. >S'., 
 \'ol. XIII, p. 2<)'-,. ha\c iieeii ad.ded for conrpari--on. It uill he seen that rhe\- at^'reu 
 (doselv with the coeflicieiits of IIanskx. thoiiuh deri\cd independently of llieiii. 
 
 
rRANsKORMATiux oi- ,,.^^s,:^■s r.rxAR TiiKoKv. 
 
 8i 
 
 4' i- 
 
 II, \z 
 
 sin. 
 
 CdS. 
 
 sill |.()S, 
 
 sill. 
 
 COS. sin. 
 
 -3 - 
 
 + 
 
 + 
 
 <). I or) 
 
 7. "35 
 7-73S 
 
 I 
 
 -3 
 
 o 
 
 -3 
 
 I 
 
 -3 
 
 + 
 + 
 
 + 
 
 +■ (i.oii _ U.O05 
 + 11.075 — o.i.i,^ 
 
 *" 0.044 — 0.007 
 
 o.oir _ 
 o. 240 
 
 O. T2() 
 fl.0I2 
 
 0.077 
 
 o.S4f) 
 o.-l.'^ 
 o. 122 
 o.oofi 
 
 0.003 
 0.0^; 
 
 o . 00 1 
 
 0.014 
 0.003 
 
 0.002 
 
 . 002 
 
 0.003 
 
 — t 
 
 
 
 
 
 + 0.003 
 
 — O.OOI 
 
 
 
 
 
 — 
 
 o.O(j4 
 
 + 0.043 
 
 — 0.010 
 
 I 
 
 
 
 — 
 
 2.524 
 
 -{- O.OS2 
 
 - 0.03:; 
 
 2 
 
 
 
 — 
 
 0.052 
 
 4- <uo 
 
 - 0.024 
 
 3 
 
 
 
 
 
 — 0.002 
 
 — o.(,o4 
 
 — I 
 
 — I 
 
 - 
 
 0.040 
 
 , 
 
 + 0.001 
 
 
 
 -' 
 
 + 
 
 3.665 
 
 4- 2.324 
 
 4- 0.046 
 
 I 
 
 — 1 
 
 — 
 
 27.620 
 
 + 15-144 
 
 + 0.0S5 
 
 2 
 
 — I 
 
 — 
 
 23.00') 
 
 r S.4()9 
 
 4- 0.045 
 
 3 
 
 — I 
 
 — 
 
 '.337 
 
 i- o.(;S4 
 
 f- 0.007 
 
 4 
 
 — I 
 
 — 
 
 0.060 
 
 -r 0.04I 
 
 
 -2 
 
 — 2 
 
 — 
 
 0.020 
 
 -- 0.003 
 
 
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TRANSFORMATION OF HANSEN'S LUNAR TIIF.ORY. 
 
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 TKANSroRMATloN tU' IIANSKN'S l.LNAK l\il.'Hi\. 
 
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