1311(3967). of cur:-ants, tides and winds

lmémq nodinal in the Indian Ocean..a!'B. £21».Anfltznoaq D.L@I¢ and F¢B¢ flmriusdt £1976)» The Somali

‘r¢Im%nu to the lwtmutt Im1coan;' tin relativeimotfi-was of local. and zanote forcing. 1- fig. 535.,Q3, sea-411.

fin I-{Iii an-Lfiu @&'en--equatorialinjjortitl Jot: with sprain}. tllcvmacc to very remoteforctng at the Somali meant. £1 Qg,-1, 26A,1.22,

\?IB-.1-‘QB.-Q anProfilcs ef wind, tmpuaturt and 1-zmidizy our theNW1» 8"-k§“9o$a “It PYQQC-Q 84 pi);

Barlaw, 81-W (1934). Gurroat of Arabian $0: and Bay ofBmqal. LL» 19-22-Q»

Barlow, Edi (1935). The 1910-1935 survey at tha currents ofthe Indian Ocean and China Son‘ , 52,153-163.

Basil flathew, R.*;m;%i}ai: and 1153.3-Sham: (1982 ). TM TropiealCountomurrent in the Imiim %0~:-:0». 33$ ,1. 335. Sgi. ,20$-211.

B017», V1-‘S (1967); dopaadanca of um spectra of theva2.oc1t.y cnmomnta of a wind-driven zurront on theipmfitrmm nf the tangential. force Lg. p andla 133-7"'1295~L

132

Bhhop, LB. (1979). A note on ;lB1‘f8¢O wind-driven flow.­

mm 1» 2- 25-284­I ’.Bi-Iiwfi; Jui (1980). Anote on the manna]. transport on the'IMd‘l' Qh-Q!.f.u gale; Q2,“Gonna, E. ($322). Varqlgcichonda Bbtzpchpunq dc: Kllmaa

unddnrtatton Mftziabutxanuwn an_ do: sudmgta

Q»? ms... 23,- 1-18'»‘exacts, K pad L, Qsqtraoyer (3.972). Thqhydrodynamic

B1’ O35‘.

Bruce,

B21160,

Br\l§.§

&'yan,

$13;

muqhnou of ‘aha an surface. In Phgg. »,Ed.A-L.Gordon, 75-92¢

0..B¢, Bu-ace, J.@.a. and mm Evans (lwo). Evolution ofcop a%arv£%_a:'e taxmeratfiza in thy Soaalfpasin during thesouth want ne-moon, at 1979. §;1,g3gg,, 2_Q2_, 595-592­J45 (1969). A furthur estimate of maxlw transportof Somali Currant. %g Q; Q9, Lg‘ '22?-228.J»-;3.' and @;;i.H@Vo§mlnn (1969). 5918! naasurements offthe Sunni Coat duzinq tm northour monicnn..22.» me.-1 1°5°-1%?­Jwi (1973). Large nah vlriltlom of tha SomaliCurrant during the scuthwnt momooa. £5; £5 $5.,_2_Q_, 837-8461

K (1963). A nmoirical !.nv0lt1qat1oa-of a nonlineumodal of a wind-drlvvn Oenlm la Qgfgzgg 35.,gg, :94-60¢. ­K (1969 ). A mmorieal model cf the atudy of thecirculation of the worldoceml. it . F-‘Q1315; ,1, 347-376. ‘

13'}

kyan, K Gm: 41,13 (JSQ7), A mun:-teal. imruziqationof the ocddaic qanaxal circulatiun. I_g,Q§g_, 3_.,!_,-54hv%Q

flryan, K and fie: 3.0 (1968). A non-1i.nol.r medal. of anacnn driven by wind and diftnantial heating.2' W5-957, 9&8-9?a~i

Bunker, MP (1976). Cellputatlolti of anrflei energy fluxand mmnl air-can tntcraatlon cycles of Anna mrthAtlantic 0:01!» V. fly. Q1, 1122-1139.

Mrt, W.V.,% C@inga, T and Cd» Plulcon (1974), Themcoacale wind fluid an: an ocean. 1. -39g-Qhzio_Q§_»~, 12, i

maa1%a\m1¢ AJ and J.J,0'Br1an (1.980). The aa:ona1variability in a nodal of the tropical Pacific”J.-» fill.-> ¢ 19.» 1999-4951*

Bye, J1..A., Mays, 8.3 and Sag (1975)».. A nunthly analysisafi»q1'oha1 um atria and th0'aam tzaasparts‘

CIHGQ “AA FOI'§Qd B31"->€'1il'\1Cocean motions: I The linear equatorial unboundedi‘»*lI8q in my 629~$§5-0

Cam, flux (k979i). The raapmuo of an equate:-1&1 ocean tosimple wiadatruu pattarmi 1119601 formulation and

@ QaI1YuC tflaulth £0 E0 mtg.._-=9 ""Cam, MA! (1980). fin the dynamic: of use equatorial.

entrants Vwith lpplicatioa to the ’lndi.an Ocean­Eln HA: 525'544­

1534

Nah (19?9h)¢ Th! nspoalt 0! an equatorial. oeoan to“ timid: w1ndstto?u parttoranz II zimgerical results,

i» QUE? 5!». £2» 253*399~

Cam, bun E¢$¢$araeh0k (£916); Fotend bnroclinic oceanuotiunsa I The linear oqaltar-1.11 unbounded cane.is Hhib fill»; iw °99"°‘°~

C'I1'1‘1I2" and LA,R.E*iob1nuen (19&).% On the theory of thewind--dri.Ven Mam tirmllatiom _;-1,» @111," L5;-‘,949-BC»

Qmznflr, 3,5 (1955). The qamrattan of ocamic currents“V '1“d' £r.§iErfi§!Iao I1: ‘77*493'

Clmaraay, J.-23 (1960). §4<:n~1*1rwalr theory of a winch-drivenhomoqumeaa layer Mar the equator. Q 59;. ,Q, 303-310.

Charaoy, J¢~3 and &$a1agn1 (1971); szmewro of wind­drivan nquatorlal currents in homoqanaeuz oceans.J.- 1» h 1*?-w~

Clown, JMJ. 3.81%-flwm (1939). Thu Dupuate: circulationof the Indian ‘Enema. 936-938»

Colon, 1.5 (1964). On 1nh:actt%om between the southwest.momoen entrant and sea surface ova: the Arabian Sta.£.- m- 18$-2%

Cox, kl?" (197%). A matmmaticai. medal of the Indian mom.zw.-. "~"­Cralqan, A and JJK. Johnaon (I978); An advectlve mixed layer

model with imvosed surfaco Mating and windctx-en.an-m m-. aw W-=w~

185

fifltchcr, l~l.L. (1959). Upm: rind? it-atintics charm of thenertmm hnnisphnrc 90-20-535, Vol.1, 21.8.Offiae of Naval Opal-at.1om, wuhiagton 13.0. 33 pp.

Dozsliyshlra, J (1963). Coaput-and currents oft the_ Cape ef623-#63210Dlrbyahire, J (1964). A hydrogrnphical. investigations of

am Aquila Current nan. 593,, 11,, 781-815.*Dlfm_t, A (I926). D10 Austanwhqrotao dc: ntmosphariachen

and ozcanluehcn ztrkulatiom ,&3,¢ .12-$*Dc1'_’ant, A (1952). Tmorotiwho abcrleqanwn am phanmn

dc: wind stun % diil Mftzioba an ozomischen :<.uaten_mv= - ew­Denman, 14.1.. and hméiyake (1973). Upper layer modifications

Gt OQQ-Gil ltatiam Q3 1; 18.5"~19.60do Zzockc, 84¢ (1980). m thoyffiatn cf hori.zonta1

variability of Iindstrn: an the dgmnics of theocean nixed layer, Q, -1, 1439-1454.

Dongay, .J'.,R md Chflonin (1980). Sarflto ¢ond1ti.ons in theauttrn equatorial Pacific related to the ITCZ of theUilldin mtg 2L

Duinq, ii (197011 The masons main of the currents in theIadim Ocam ;.~1an‘;-Wat Qatar Pun, Honolulu.

Duinq, W and i<.I-l.5zh101da (1971). Momoonal nopeme in thewestern Indian Ocean. Q, Q3,-~, 19,, ~4181--41310

Dtlinq, W" Mollnatl, R and J.Cq5UI110\Q (1960). Somali.Currant: Evolution of surface flow Q,588-590.

136'

. . 1m tiewh 11» Aqulhu On-ant Paw. azusnzzauon.af 76 pm(1976). Gawain ea high nun in the Aquinas

\

c%‘Q:flt» EQ“i$¢'h@-U531; Q9, _?Q; 31-#5:I z *1.1.8 (1924). rexatiemhnp batman current and

*1"4* &£~ £- .%-1 fir 113*Bataan Hydrag.ra»phi.a¢hn Inctitut cxew). flonatlkartan

fur Iudlcchen Ozoan, Pub!‘ He»2422, Hamburg»

Ewan, V.%ii' (1905). Ga the Lnflwnneo of the earth‘: rotationW @=w* ¢wmfl": £zs.L§~ 2.» 1-5—"*­

Elmm, VJ! (1923). ‘Jhor horizontal ztrlmlation hotwindarzuoq ton Mirna: 555,,§Il_§Kla 11¢ 57*‘

Ea,-ikaon, C (1979). An uquat-0r1a1.tranco:t of the IndianQ€QIIhEvanuon, Au‘ ma Vernon: (19?5)» Goatiauous M-pteltntatian

ef nlndswttiu and \vr£ndt‘t:'nt en: the uarld ocean.1' 0 £1» 3-31-"'1‘“~%

Flndlatcr, J (1969).. A major low-Iain). air cnmrmt mar theIndia Oman during the was-thara mmrr. @553» J;

Findlatar, J (1974)-%- The low-lmnl @2010 lquatorvial. airauxrent at the wutera indium mom during thenoLrthc:-n sum-nor. % 32, 411.-416;-. ' . y x

Fafnoff, 54.? (1954). Steady flow in £1-i.cti.on1alc homogenoousOQQIBQFofnoff, NQP.‘ and &.B~idontgeom0ry (1956). iiquatorial

Umdoteuzrmt in the 11-<,:ht at the vorticity equation.1, ma-521.

1'37

Francis, Jafinfi (195-4}» %%‘i.nd;t:au an a water suriaea,Q4-*§* 1Fmwana, 6.1: (19):. mm affeatn in the Nerth Sea»

=5 ~ ~ 918-@8*~‘$1110, 9,8 (1§i4). Kltmatdoqta van éen Indischan Qcaan‘

£4 37 %PP4,*§t11e, P-H (1928)¢ Klhmatéaqie wnnqdan Iadiachan Uauan.

§- Eéi-E an i.J$..9..E.*1-"1 ¢ @5 QQI 99¢

*Gfl11e, P¢H (193fl}» Klimatdoqie VIE dun Iaditchon ucean~3-» za31~;m.esL, ‘$1.1. (1958). A nm¢r1:a1 sway of trazuianra Hosaby

»uav&s in a‘w1nfi~d:1vua-huqancaua acaa»is £5821: §fi$I Zia 3“i¢

$hnah, 8kK., Pant, £@C and B@fi.t99uIn (19?8). Influancecf the Arabian sea an the India ammo: maaoon»E; 117wl.25@

q£11, A.§ (1975); Hbdfils of eqflltalitl currtnts in‘v -- __ " A. - - - -- - ’ - '' U'- .-=;i§.1- -.23 - . I ". ;i.'"..A’=._ Y 1. - ...,L._. , '.‘!.»..1 .’-‘ f

* PW‘-i@fl*1 P~¢flwv QfSale race , pp‘.

<3o1db:euq|;' ;'i¢ R (1933); Exam Cwrnats pxroduead byevaparatioa um praeipitatiuu. _i'-Q},(.££.'.*.‘-3.‘-2.5.7 v §.';£* A91 §11’~517­

warden, $8., §iau:*t1mon,? D.-5.5 ma 2-1.21. Fayler (1981).. Thewind dtlv-an eirsuluation in, r.-ho M06011--Zindarby has in....9.§.R -, 2?.» 151~1fl~_, .\

188

‘iilmttl, I (19%). A amt:-14:11 lnvntiqatloa an than 11¢“:­9:181 lqrmtiom £0 tits rind-driven*c1:¢~u1It1on.of the aozthwutnm India Ocean batman16%-1@°$~ a I <mAmm> s..73-76.

Hutu}, H (vl.976)¢ fiitonthly chart; of surface wiadltreu curlwe: the Irminn mom. pg» 33,... fi_, 165-713.

(1971). Surfacwwlnd nrqence over the tropicalIndian Oman. Q, gb $1., J1, 875--881.

Hautel, M (1972 L Hindittifl curl--flu! {arcing {motion for°°'*'"5-¢ “*°‘¢1°“¢ 1" % "'£5. R 25 HaEchhd-Q ~430rd05¢ ‘£;aordoa% Ind kink, Science Publicherl,N01 York and London, 1,

Harri-as, LFJ (1.972). Seutil cf the Agulhn Gurrent inQue tpring of 19@64¢ my, 1,2, 633-650.­

*i-lua, 3 (1968). Zn: Euat.1£ dc»: vottlkalea tranapoxtevaon impala and fuhihuor wanna in dc‘: waaznahoncurmmumz um! Olin1)» 7° W»

:-lason, £5.54 (1968). on the drivin eccm tirculation..&?-In 2' 3“"“3*

mxu-mm, s (1961). M azum 4»: tr» wmdctruson the world ocean. Q $1., Q, 607-626.

1

Housman, $ (196814-» A9 updatod cat-mate at the windntruson the warld ocoam Correction fioLt1:e. ' £5. $3,.521-. % 63-"­

mzumm, s (mm/ac). Quart: of the vuzaziny of rmwindstzcu war the trbplcal Atlantic. 33,"

139

mu‘, K lilac in scan currents and%1atQ:{83; Q, Lfig" Q, 132--136.

ifiadakq, K (1%-Q3.» Zonal aaan ca:-hats M-inn by winds.PIOGL95~V0!'bL&-In25¢ amHtdaka, K (1955). A thlo1rei1¢l1 It!-idy on the qemrll

simulation of the P0e£ti¢.0¢0m. 25313;; Q5. 1. 2,183-2201

\\|

K (19%). Gemutatlaa of tin umdatzen ova: the@=¢m- ms» mi 1- T1-123»

i-Ilgbinn, 5.5.1. (1965). Sum éynaical apuato at Qccan¢@r=-=~=~- 1- M.- .m.-1» 3%­

iifiuqh; 3.5 (1897), On the app-lifiltian of harllonic malyuisto the dyamical thaazy of the 121401. Part I. OnLaplace Gacillltions of the fiat. sprain and an thedynamics of Qua :u::'nn%s. 51,1. §_;_m.(A) }§jJ_,2O.'|.<n-Q58;

%Ho1a=pa1mn, ‘$0 (1967). flotcrainatloa of the \d.nd-drivenecon circulation fmn the tnztialty budget of theIm'Ph'=~~ mm m * 156-165­

Hugheo, R.-L (19®0)» On the equatorial mixed layer.Mi»: H.» 1967*'1°'73~

Huéfaurt. 1-L8 and 1.0. Thomnon (IW6). A numerical modalat the Smut mutant, 1,» @p . 9, 646-664.

flllyin, Adi and Vafiolflflflkfilifih (1963); 81: the influence off1‘.1‘tl-OR 911 £EQIfl_ my1214-121?.

Johnna, J.A (1979). A wind drlvca zonal. channel withItzhiiflaatioa m bottom topography. wgggq1, 1-13¢

140

Metaazalaggiah Imtitut (1952).nun,» §OtQ¢t6l0<3i¢l1 fiata.Pll.b1$£l€ $Dn §~lo¢135, 2nd Qditian, 2 vulsfl 24 sheath

2-.a £1969)‘ mu m do ma knew! about the sea1‘ W1-nélitflriia Q3. g £2;

—+ -IvKama, 84$ (19’f6). a long iarins of nnaunments of

Imim? {ileum equatorial mutants near Mu. Atoll­Q5 32.9.” ?11~221­

8.0 (1958); Seasonal cycle’ at an surfwotmgrature mjsd salinity dang the out coast ofIndia. §__g§3_¢ $4; .,_3_, 12-21:.

Le0t§na,* A (1972)_. reupanaei of the $oma11 Qunant tothe aouthamat manmcm of 19?Q. @591319->325‘

Lama, A am AQFG. Bunkor (19791); Updated charts of themam annual winéatrus aanvarganeaa in the Ekman1%'"‘§~ Q.‘ fi!.=¢?: *fl(Z.)'

Leetma, 3 and I-hfitamwl (1980). Equatorial Cur:-antGboarvatiana in tha Mai‘-arm Indian Queen. J_¢II 1» 255'

I1.£qhth.1.11{, 15.1 (1969). Bynamic reapoaao of the IndianBegan to omit of tha wuthwoit aonnosan. _P11_;_],_»L I_;:_gr_1_§_.91. ma; 45-9?»

L1-Milan, P-.5 {l955I)¢ wind dr1V~0a:urrenta in thehw>¢1ini<= lawr of Y-M uh32(41)­

Lsztjalqrmp, 3.3.51» (1976). rm Aquinas Currant systemduring vwrtheast aomoom 1. 251;. ; , Q,

141

3.3 and 5.8.3 fienina (19%). Equatorial Currentsin the intern India: 292,E (1900); The atudy of aeian c@i.reu1at1on dynmnica

Iith rmorical medals; 1, ¢ 35,. gg.13‘h14Q§

IEQC:-0:17, J‘? (1981). A 11:10::-stratified oaan made]. ofthe Equat-aria]. Urzdamurflnt. £231. lgggg-%_fi_. ¢Zfi(A)¢ 603-635­

fickai, $.13 (1973). The wind-driven aquatazial circulatizmin a hoaoqemmn niacin» $5,, 889->899.

mats, Y and G. Dean (1952). Thu aburvod mum field ofnotion of the i‘SQOIP'hI 1‘Q4q%~8o..1T, iicuphyawl Runs.-an Bltflctoratt,Cmbridm, Mus“ 65 pa.

1‘

**Michae11s, (1923 I» D10 %fia%arhmnnq an dar ehorfleeha dosIadiachan Gama in Jana and Juli. mag. gait.

‘Malia, L (1929).. B10 simulation Imiimhan azeam..:...afl.-Y 1‘ ms.» 1-48»

'flont~g:onory, 8.8 (1939). Ein Varnish don worikalen andsaiticiun Awataulsh in ch: 1‘1efo dar aprunqschichtim oquatorialen M-Iantlachcn azQ%m I09 baa ti-wmn.mi 91- 242-446­

Hnntqonnry, 8.8 am Emalnon (1940), Contribution to thequestion of mo Equatorial Gouatamurnnt.L~ Em» £2» 2» 112-133»

wan-, D.“ (1963). Ronny wflta in (‘main fiirculatiom52.», 19.: 1'35‘-'?48~. v

Bbrqan, 8.5 (1956). On the wind-driwnn oenm circulation.9.: %1-32%

142

“IQ? %"B'?iG¥'K1"-IQQ L031-I %i¥i.‘§lI'%X§10fl8betunn the Ina and the air at mainly and annualthe main. Q.g,§_¢. a_9_., 114-12?.

mum, mu (1941). A zritinai my iir--mabeam cry p:occup:._¢, 31;. , §_, 203-278%.

Mum, $3 (195U)~ Ga the Iriifi-dr1'i=an mam ci.rcu1a~t1on..~Z.- 1 L 1'9‘-93»

stunt, $3.3 and 5, F¢Ca:r1c: £1950}, an the wind-ériweneireulatioa in balm ef vartum shapes.

Same studliaa an that and Equatorial. Jetin the lindiaa New free hydrugrafihie chnractm:i--­

113-I.26.%

liommann, (1955). the ¢ynm1ea af * the wind-driven-Ocean Entrants; !htearni9g1i.¢'a1 paper: 2 (4),mm Yo:-is ikxh» Print»Qwind-inept. <:sa;hdL acom» Q, 533., Q,135-»149=ju

0'Rrion,, JIJ Ekfidhrlhurt (19?4).,, Equatazr-1&1 3»:-at inthe Indian wan.Penna, A1-F (1977). Sam fentura of the amps: m of the

Phiiandnr, 5;¢%ii.%H and R»3¢Pa:m0ink1 (l%&}* Heaven“ ofequatorial eczema to pariedic forc1rtq¢. Q.Q 1%3'*1916u%

143“Qt-8 9“bulk aeradynmic aceiiiczienta for sens ible heatMd =@1#W=# f1*1==**~ 9.»%333~339u

Ran, YQP (1.964). lntcrhmisphuric c£rcu1at10%n?. Q§:_g_'g_»,,_J_,j1,_$51» aim; 1905194!

Reid, Rm (1948a)@ h modal of the wartical strueture ofmass in the equatariai. wind-driven currents of abaroclinie mwan. Q, Q9, $4-312‘

i%i%d,, R.=3 (1948b). The equatorial currents at thePmiflc as maintained by the st:-Let! of the wind.Qblfiflgp Bfifipa if ?‘*99I

Reid, LL (1959). Ewideaea ef 0 Smith EquatarialCounterzuz-rent in Pacific cm. Jiiag 7 gs, ggg,209--210.

Robinson; ma (19%). M inve=lti.gnt.1o~n znm the mm u _the cause ef the Equatuz-101 Undo:*:arreat. _._I_. fig,m¢+g Q1,

Rosaby, C.:.; (1936). Dynamics? of ste%ady ncnn currents inthe light. sf ax:aQri.maf¢.a1 fluid dynmicl.&1i.*' :2.» 1-43¢

Kfifi H978)» Air and utter armour trmaport acraaaaha uquater in the mstlxn Iadifim Gleam duringnorthern simmer, 6=81--68?.

*Sark1aiaa, (1954). The ,:aL1~w?1at1an at stationary windauzrents in an cum. J51» - fig; R. sssa, Q5.551--561;

3-55 Ind V4-Ramesh Bibi! (1979). Convargenae of Ekmanwind driven layar and surface %a1::~c%u1ation in theArabian 50a during; aouthwnt mnnoon. z=-Aahagg Q, ;g_,219'!--'2.’£1|

144

Whott, "G (18%); hlttultotu Uluwtc-ht dc:mtnaat-.maqaa~ smfltnnqey @. -»

waaatt. is (1935). Gaaggimqphifi an Indicchcn ma nun»-1

*s¢mu, 8 (1942). 5&1-%1aq0n'Aaf1ni: hltkcr ta &rM"r”~*=ww~w=~ am» em mamI 2-éflinmh-» 0 329-"3*w»

-‘I’

Sehuaachnr, P (1940), flanathlmrtia dc: %ohn:£1achamtromunqonAm Nordatlmtllchon cm» (5%-ao“m. Q5.

1'S¢hma:h0r, P (1943). do: ohnifiachcmtramznqonLnaqaatarillan wt ludllthm Atlmtiacmn mum.Q5!» ~ 0 lb 299-31‘?­

Scztpps Institution of Oiuaaoqraphy (1948 )1. I'M nanwiadstron ovor tho FIB!-£10 Oman -»

5010011,. 3.8.8 (1927). "iickoqrahic and Dumoqxaphlc rpuaranin "Indian intlrlqp ‘Pf-#3, Ibtoeraiogy inW1" 3"\- Q.‘ 2»

senuxx, R.a.As (nus). iiuaqrmhie and Otdmeqraphtc littoral;in Iadlm infirm. Phi», Ibo hworaturo and ulinityof tho caaatal wittru of 1'-hi 80:­

knil, 8.8.8 (1929)¢ %rwhta and munchin Indian wutors%. Phi, Iclpcraturo and salinity ofnltfnce actors at the Bay of Bcnqal and Andmm 50:,with rcfqrapce to tho Luadiv Sit» fig. 51%» @1­2, 2074-355;

145

Small, R¢B¢$% (1932). asmqrmhte and Ocoamgrtnhic roioarchin Indim Iitlrh Inn:-atmo and llllnity cfcm dupe: watcn -at at Bangui and N\damm Sen%v &% 2: 357*'493~

$513231, G415 (1968 J. Sena on the EquatorialUndercurrent in tin Infihm Gmlm baud an thePhyaical. proportion nf the units. _._I_. 55;. §§,g_,],_.; 55;.19.» =24-236~

&|uau, 13.8 (1971). Studiat on Glwmmm of the surfacewater: in the ram. thesis,Andhra Univcruty, Walttil; 102 ~991­

wazaa, 6.5 (1976). wail: ahawutuiatlcl and mrront.Structure at 6!-'v°E during aoutlmut unseem­J.- - Qw W-2%­

Shaman, 125.5 (1978). Upnlliaq ofltau southwest cant of1“"11'~‘ $18.15.» 33$."-Iv 2°9""319*

awn, 6.8» ~3mm.a., A-J1. and anus Sutéyoadra Hath (1973).1mursion~ of Pwific W139: Late that India<mm- kw EA» 29-45­

Surua, 6.3., Nuwadrm flair, R mé M011 Mathew (19-B2).Current atructan in the lntnxtropical Indian Oceandm-mg use ms-thnat gaomwn» 1, 35. Q1. ,ll! 7-14: .

Stewart, am (1964). The lnfluomi of friction on1n_;art1I1 nodal: at anal: flztfllatiomP» 3"-9‘

Stewart, R. ii? (1974). The air-tot naquntm larch anqo.- Q» 151-16?»mmz, 11 (1942 ). rm maxim 1=mm1a¢;u.<>n Of

uiwad-drrlrvcé mean eutanntu Egg, Q, ~

Etenul, I-I (1§57' ). A canny at ocun aarrcat theory‘5.» 149*!“­

148

$t%0‘l., H )1! THO E“: .0510 Calif.hon, 80:-any, caith 2021190

stone 1, H (1965). almrtc at tho mm dynamictapaqtapliy and eartint fluid at tho surface of theoaonn and telatcd fimctlcn if the man wtadatrnl»In *- Y”"14'- P» 51*-=8»ilniverilty of wuhiaqta

$VO1@1't1#Jy 8.8 U947)» “treats in I ~baroc1.$.n1cocean with npplialtalon ta the equatorial cuzronta ofthe eastern Pacific. @ $1. gg. Q_.§_. Q,31-8-326»

Swallow, J.C (1964). Eqnd-0:111 thdutiutttat in theunborn Indian Guam. Q, 436-437»

swallow, J.C (1967), Thu Bqfll€Ol‘i.l1*UfldQ1'fiBI.’tOnt in thewatora Indium Guam in‘ 1964» an. Ra. %i­ma!» 2- 15-M­

Sulllow, JQC and J.,i;i. knit (1966). at mntiurcmentlof the Somali qout daring the touthmat aannooa of19¢4~ Hr 9‘¥~5"°~

*I1‘1*:h0moa, R,H.%Llmnb0 and Pfiialbuut (1958).. Sur quolquuMu voila: observations hydroloalquas relative a Inregion oqnntcrialu 60 1' Indian Bull.» In!» Con.¢<>"*~ flaws.» 115'-1-*3­

Taft, B-and J-EA- mama (1967~)+~ Equatorial: Undorcurl-out ofthe Indian Baum as oburvid by the Luaiad Expedition­.2» W 1»­

tlda, It and lgfiuuauna (1969). eastward SubtropicalCountomunuat in the western ziorth Pacific Ocean.J.» Qti ES: lflm 20$-31%

Uu_1tld 5tatos Hydrogrnphic Gift“ (1944)¢ Alla ofsugfaca ¢ut:a~nta» Indian Ovzcarn H.O.%>lo.566.

147

Wu.-adaebari, V3.3 (1961). Ga process at upwellingand linkiaq out cant of India. @3­

me-»1s2.

Varadachari, V¢V.a and &$¢fiaml (2.967). Circulation ofthe autfno wliirt 1! iii! Indian Ocilm1- 1.. 61-11­

vu-an1s@ (1963). Au mural! 0! w1nd-driven aces:circulation nun 0 mm: 0! FOIIIIIIeenponenta J; & $77-693.

Vironis, =3 (1966:). ¥§'lad-41'1¥QR tlrtulltlon Pt-1,El." 3""1‘*Vorontc, is (19663). Iiad-4I”1-imlm circulation Pull,

5!-12%-r 3555*Vitonilg ( 1973)» H9601!‘ of Wttld OGOCB G11‘G!31l€10!\ 1.»

Hi:-wd-dxlvca hra-1070:, g. , 3;, 22a-eaq.Karon, EDA £1966). Iilditwal Nab afcnncoo to the

uaaonally tnflralaq tutrents of thl hbzth Indian

wnrcn, Bram, H.5taua1 md J.C.&m1leI (1966). fiatatmun» and pattern of flow in tho fiomali. Bumduring the nouthllit Iielltuun of 1964. fig,"

vmumaor. P (seam). On am mmmy xntoqrawa wastnanport in the actors... In the and Socin il@olV1an--ifiii Ed,8.3o1_|.in-. Qxfotdunz. Pm», new um, P.

launder, P (1968). Tlwnoretinl tom: for the vertical.oxchnnm inefficient: in a Qtratifhd fluid withappliaation to lat» and nit» 1,, 2'7.

1418

Heller, H,S.and K-W1 Burllnq (1961). D11.-oat uoaurumtaat at:-on and watts of iuzhfllcnso in -aha saoundarylayer over can ,1; _&$., Z1, 653-664.

*w£zz¢, E (1319). van: Mnusuaatsunmaqaa 2. ax»otzomungondormuzulmn Quin in ggggggFuratonuheilizu. P1010 Krmor Promo,Pu 2M7»

Wooster, $3,, and M,@311lntt1a (1961 )1. The Porn-ChileUnd0rc;ur:ant. ‘.5, fig‘, Qfi 97-V-112.

i’¥oeat.er, *3.S, and :T.L- Raid, J1,{1963). Eastern boundarycu:-xonts. In %.lt.i~1.H111¢ IntoraciencePublizhar, York and Landon, 9- 253-280.

Woaatnr, 8.3., §_a3¢3¢’!|IlfI1‘ and Ink-flohlnsea {£967}. Atlaaof the Arlbim SDI far fishery ¢¢can0qimhy. Q},91.» 1-41­

Wyrtkl, K (1961). TM zmrmocliao circulation in relationto the general circulation in the occnns.5.22-In §-I

wyrtki, K. (1971). Ocomoqrwhic nth: or the InternationalIndian Occur: Expedition; ‘Washington, 0&3. AationulSci. Foundation, 531 pp.­

wyrtki, K (1973:). Phynieal Otnmagraphy of the IndianI Ocean in Ecological Sméicu Analytic and Synthesis,

Vol.3. ;*£d.B- Zaitnchol-7 firlngon-Vorlaq Bttlin,“CW YEP‘; P-Q 1911360

Wrtt1,':-1 (197%). An Equatorial Jot in the Indian Geom­.3-Liflfitv l.§.Ju 2559"-?54*

149

Yaaluda, K (1955). An canal: of rm-tatiom la accaniccirculatien in memento ta/c.ho variations in thevirfl f1=1=*~ 1- U» ma-1%

Ycshida, K. and (1957). A thlory of mulling oflargo harizeatal. extant. 1, 53., 39,

‘lushida, K. T-Kldokoro (19671)-% A fintbtzaplcal.‘fiounzorcurrunt? in the North .Pacl!1\': - An on twardflow near the subtrapical convorqena-» ,1. »%- LEE» 22¢ B9-91*

‘foihlda, K» and hlfiodbkoro (3.96'_!b)¢. A Subttopic nlCountarcmrrant. (I1) -% A pt!-dlctiun of eastward flow:at lower subu-opicaxl 1ar.1tuda- Q, . fig.gg, 231-246.

Yonhida, K (.1970). The Kuroshio --V A symposium on theJapan Cur:-et1tA. But Wu! Gnatnt P1-us, Hofiolulu,197 %0

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