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CONTENTS 
MMerOAUCtIONM ee ie. ae ee ee Dh ape ee DG pele Ek MORN a wel Se A 
istoricaliistatemve mites reas see gh as See SR eek 
General explanation of tidal movement__-____--------------------- 
Harmonic treatment of tidal data_________________-__-_-_---_----- 
AStroromieall Gl Ge ese rete yet rey ee eg SI 
Degree. ofapproximalionusstesn 42 Hanes eee Se St ae 
Wevelopmentof tide-producine: forces Shy s2 {wee ts ae eee ee 
hundanrentalsformulasiss 22 2s eee ee eee Sh ee ae 
Merticalicomponent offorcesse= see. = oa eee 
Horizont alvcomponentsyondtorcess 8) 22s) Sees saa a Ze ee cape 
HFRS NT ab wei Ta VL en ne Ba est, ee 
Terms involving 4th power of moon’s parallax__________-___-_------ 
Sew stid ets= PATA METH ae Dies clare. Ya een eons Sree eee Be 
HS UITATS@ Lear eyes UNL PRG Gl COS mead pa poe gree ere ey I 
Meteorological and shallow-water tides_______________-_-_-_------ 
Amalvsis ot observations ise 22 SR Oo Ba Res Sie Sea die se ee 
Larmonicrconstants ss. 2b Mae Ws et eae eset, Bld Wem eee 
Olosenvatiomneallyclata lowes. Upc oRinee Me faces ely Ski OP ke oa ae 
SUMMA TIONS LOM ANAIVSIS oauals Spence Sd ce ae ee i ee 
SUE T Cll Sees eee erent aco ty ln. ieee NE eae oh a Naess ees Le 
Second anyyst emcee oj ei yak) Ue ae AIG RN EE OS Beal ae ee 
ROUT ETSSE TI Sie cae ake ie laa nnd par tele SR see 5 he ml ape a 
PasewlageOr CpOChisetsaaty sn seven 2: Sea Lie Pea ae nes Oe ee 
linferencevor:constantss ok A ee es ee 
FEAPTVT TVG TO eRe AR Ns ee ES aU ee A eos sera 
onesperiod constituents ae ee es een 
Amal SIS.Ol hiehvanGd lowe WaAteISe se aan oa yh Ne ees nana eee 
Horms used tor analysisson tides. =. scm ose oe ee eneee 
AMA sistotstidalycunrentses= ee a oe nye) Eley ee 2 pee ee 
IBTECiGGiOnKOfebiGeser (ene tle Nee yee 8 be at Ces le 2 RES i ae See 
LEE ere OGY aes SO STH OVeX0 beedigpn yey ofan eR em pig oP EET rth ORM ya ay Cong ke 
dhide=predictine, machines sree ts fe ees See Ue Seale 
Forms used with tide-predicting machine_-_-_---._----_----------- 
Rrediction,of tidal™ Currents ee atte ee de eer een en era 
PATER La) os mpeg dcr ee ese RR I a G8 sas a I ee cee er eae Rea a 
Explanationoritabless 22.) seesaw iad = es ae a ee ee 
1. Fundamental astronomical data____.__________________-______- 
De LErMoniCecOnsticuentss= = 4s ee ee ee Eh Cy pee 
Mean longitude of lunar and solar elements_________-_-------- 
Differences to adapt table 4 to any month, day, and hour_------ 
. Values of I, v, —, v’, and 2y’’ for each degree of N___----------- 
. Values of log R, for amplitude of constituent Ly.____----------- 
. Values of R for argument of constituent Ly______-_------------ 
. Values of log Q, for amplitude of constituent M,_--_----------- 
. Values of Q for argument of constituent M,___-_-------------- 
11. Values of u of equilibrium arguments for each degree of N_-_-_--- 
12. Values of log factor F for each tenth degree of /__-_------------ 
13. Values of u and log factor F for constituents L. and M, for the 
Wears: 1OOO CoOeZOQO segs icees craw) fs AI ee RE eae AERO Lia ae eet 
14. Node factor f for middle of each year 1850 to 1999_____-------- 
15. pauilibr den argument V,+u for beginning of each vear 1850 to 
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SOWONID CB co 
