ReferenceList Pages on which references are cited appear in angle brackets. Every reference to original material not in English for which the editors knew of an English trans- lation is followed by a reference to the English trans- lation; references to untranslated Russian material in- clude translations of the Russian titles immediately following the Russian titles.

Aanderaa, I. R., 1964. A recording and telemetering instru- ment. Fixed Buoy Proiect, NATO Subcommittee on Ocean- ographic Research Technical Report No. 76, Bergen, 46 pp., 20 figures. (+os )

Accad, Y., and C. L. Pekeris , 1978. Solution of the tidal equa- tions for the M2 and 52 tides in the world oceans from a knowledge of the tidal potential alone. Philosophical Trans- actions of the Royal Society of London A 290:235-266. (297, 322, 323, 329,330)

Adamec, D., and I. I. O'Brien, 1978. The seasonal upwelling in the Gulf of Guinea due to remote forcing. lournal of Phys- ical Oceanography 8: 105G-1060. ( tla )

Adams, f . K., and V. T. Buchwald, 1969. The generation of continental shelf waves. lournal of Fluid Mechanics 35: 81s-816. (asa)

African Pilot, L967 . Hydrographer of the Nar.y, London , I}th ed., 3, 529 pp. (tAS)

Agee, E. M., and K. E. Dowell , 1974. Observational studies of mesoscale cellular convection. lournal of Applied Meteorcl- osy 13:46-53. (sOO) Agnew D., and W. Farrell, 1978. Self-consistent equilibrium ocean tides. Geophysical lournal of the Royal Astronomical Society 55: 171-181. (aal)

Agnew, R., 196I. Estuarine currents and tidal streams. ln Prcceedings of the Seventh Conference on Coastal Engineer- ing,The Hague, 1960,2, pp.510-535. (ZO+)

Allen, J. S., 1980. Models of wind-driven currents on the con- tinental shelf. Annual Review of Fluid Mechanics 12:389- 433.(zzz)

Amos, A.F., A. L. Gordon, and E. D. Schneider, 197I. Water masses and circulation patterns in the region of the Blake- Bahama Outer Ridge. Deep-SeaResearch l8:145-165. (27 ,28, 36,r2l)

Anderson, D. L.T., and A. E. Gill, 1975. Spin-up of a stratified ocean, with applications to upwelling. Deep-Sea Research 22:583-s96. (SZe)

Anderson, D. L.T., and P. D. Killworth, 1977. Spin-up of a stratified ocean, with topography. Deep-Sea Research 24:709- 732.(szel Anderson, D. L. T., and P. B. Rowlands, I976a. The role of inertia-gravity and planetary waves in the response of a trop- ical ocean to the incidence of an equatorial Kelvin wave on a meridional boundary. lournal of Marine Reseatch 34:295- 3r2.(19r ) Anderson, D. L.T., and P. B. Rowlands, I976b. The Somali Current response to the southwest monsoon: the relative im- portance of local and remote forcing. lournal of Matine Re- search 34:395-417 . (tgZ)

554 Reference List gl. Andrews, D. G., and B. J. Hoskins, L978. Energy spectra pre- Baines, P. G., I971. The reflection of internal/inertial waves dicted by semi-geostrophic theories of frontogenesis. lournal from bumpy surfaces. Part 2. Split reflexion and diffraction. in of the Atmospheric Sciences 35:509-519. \S++) lournal of Fluid Mechanics 49:11Ll31. (aat ) ns- Andrews, D. G., and M. E. Mclntyre, L976. Planetary waves Baines, P.G., I974. The generation of internal tides over steep ns- in horizontal and vertical shear: The generaltzed Eliassen- continental slopes. Philosophical Transactions of the RoyaL in- Palm relation and mean zonal acceleration. lournal of the Society of London A 277:27-58. (aaZ) ely Atmospheric Sciences 33: 2A3L-2048. (SaS ) Baines, P .G., and P. A. Davies, 1980. Laboratory studies of Andrews, D. G., and M. E. Mclntyre, I978a. An exact theory topographic effects in rotating and/or stratified fluids. In Or- of nonlinear waves on a Lagrangian-mean flow. lournal of ographic Effects rn Planetary Flows, R. Hide and P. W. White, :ru- Fluid Mechanics 89:609-646. (e+5, 506,533) eds., GARP Publication Series, World Meteorological Organ- Qn- tzatron, Geneva. (S+S) )P., Andrews, D. G., and M. E. Mclntyre, 1978b. Generahzed Elias- sen-Palm and Charney-Drazin theorems for waves on axisym- Baker, D. J., 1966. A technique for the precise measurement metric mean flows in compressible atmospheres. lournal of of small fluid velocities. lournal of Fluid Mechanics 26:573- ua- the Atmospheric Sciences 35:175-185. (Saa) s7s. (+zz) 1a ns- Apel, I. R., 1976. Ocean science from space. EOS, Transac- Baker, D. 1.,'[r., 1969. On the history of the high seastide 97, tions of the American Geophysical Union 57:612,-624. (+Ze) gauge.W.H.O.L Technical Memorandum 5-69, Woods Hole OceanographicInstitution, Woods Hole, Massachusetts, 17 Appell, G. F., J. E. Boyd, and W. Woodward, I974. Evaluation pp.(zss, 424) ing of the Aanderaa recording current meter. NOAA Technical Fs- Report NOASI C-TM-OXS 174-ARO4, 25 pp. (+00 ) Baker, D.I.,Ir., 1970. Models of oceanic circulation. Scientific American 222:1, 11-4-121.(+lZ) Arakawl, A., 1975. Modelling clouds and cloud processes for of use in climate models . In Physical Basis of Climate and Cli- Baker, D. 1., Ir., 1979. Ocean-atmosphere interaction in high 15: mate Modelling, WMO-ICSU |oint Organizing Committee, southern latitudes. Dynamics of Atmospheres and Oceans GARP Publication Series No. 16, World Meteorological Or- 3:213-229.(+zs) ganrzation, Geneva, pp. 183- L97. (+?el Ith Baker,D. I.,lr., W. D. Nowhn, lr., R. D. Pillsbury, and H. C. Armi, L., 1978. Some evidence for boundary mixing in the Bryden, 1977. Antarctic circumpolar current: spaceand time deep ocean. lournal of Geophysical Research 83:197I-I979. fluctuations in the Drake Passage. Nature 268:69G690. (ZZZ) of ( t sa,26r, 262) ol- Baker, D. 1., Iun., and A. R. Robinson, 1969. A laboratory Armi, L., and R. C. Millard, I976. The bottom boundary layer model for the general ocean circulation. Philosophical Trans- of the deep ocean. [ournal of Geophysical Research 81:4983- actions of the Royal Societyof London A 265:533-56e. (+lZ) tm 4990. (ZSl, 334) :aI Baker, D. J., Ir., R. B. Weartt, lr., and W. Hill , 1973.Pressure Armstrong, R. L., 1980. 1976 in light of atmospheric and and temperaturemeasurements at the bottom of the Sargasso oceanic climatological relationships. In Oxygen Depletion Sea.Nature 245:25-26. (+OO,425) In and Associated Benthic Mortalities in New York Bight, 1976, Banner,M. L., and W. K. Melville, 1976.On the separationof %- R. L. Swanson and C. S. Sindermann, eds., NOAA Professional air flow over water waves. of Fluid Mechanics 77:825- Paper, U.S. Department of Commerce, National Oceanic and lournal 842.(+ts) rn- Atmospheric Administration, Rockville, Maryland. (ZZS) Banner,M. L., and O. M. Phillips, 1974. On the incipient 9- Arnol'd, V. L, 1965. Ob usloviyakh nelineinoi ustoichivosti breaking of small scale waves. of FLuid Mechanics ploskikh statsionarnykh krivolineinykh techenii ideal'noi lournal 68:647-6s6.(+0s) zhidkos tr. Doklady Akademii N auk SSSR 162:97 5-978. (Con- ditions for nonlinear stability of stationary plane curvilinear Barenblatt, G. I., and A. S. Monin, 1979. The origin of the flows of an ideal fluid. Soviet Mathematics 6:773-777.1 (530) oceanicmicrostructwe .InTwelfth SymposiumNaval Hydro- dynamics, National Academy of Sciences,Washington, D.C., Arons, A. B., and H. Stommel, 1951. A mixing-lengh theory pp.s7+s8r.(zte) of tidal flushing. Transactions of the American Geophysical (Jnion 32:419-421. (ZOZ) Barkley, R. A., 1968. Oceanographic Atlas of the Pacific Ocean. University of Hawaii Press, Honolulu, 20 pp., 156 Arons, A. 8., H. Stommel, 1956. A beta plane analysis of and figures.(aa, ss) 'a free periods of the second class in meridional and zonal )- oceans.Deep-Sea Research 4:23-3I. (e++) Barnett, T. P., 1978. The role of the oceans in the global climate system. In Climatic Change, Gribbin, ed., Cam- Arons, A. 8., and H. Stommel, 1967. On the abyssal circula- l. bridge University Press, London, pp. I57-L77 . (aSa of tion of the World Ocean-III. An advection-lateral mixing ) rp- model of the distribution of a tracer property in an ocean Barnett, T.P., and R. E. Davis, 1975. Eigenvector analysis and )n basin. Deep-Sea Research 14:441457 . (xvii, 435 ) prediction of sea surface temperature fluctuations in the northern Pacific Ocean. In Proceedings of the Symposium on 5- Augsteir, 8., H. Schmidt, and F. Ostapoff, 1974. The vertical Long-Term Climatic Fluctuation, World Meteorological Or structure of the atmospheric planetary boundary layer in un- ganization, Technical Note No. 427, Geneva, pp. 439450. rli disturbed trade winds over the Atlantic Ocean. Boundarv- (asa,354 ) n- Layer Meteorology 6:129-150. (SOa) e- Austin,T. s.,1e60. oceanography of the east central equa- u^il'1lll-l-lY:?;!,:^t:.t- ulrmatolosrcal usetulness ot satellrte9-,Y^1113,111;Tl":-]?l?- cletermrned sea-surtace tonal Pacrnc as oDserveo curmg expeortron Eastroprc. r$nery of theAmeilcan Buuetinof the Fishand wildlife sirvice eo.zst-zei.leif-' ';::*y;;:;;:i;:::;r;s:i;;:;3;'.ii{;it"

555 Reference List Bamett, T. P., and |. C. Wilkerson, L967. On the generation Beardsley, R. C., and C. D. Winant, 1979. On the mean cir- of ocean wind waves as inferred from airborn e radat measure- culation in the Mid-Atlantic Bight. lournal of Physical Ocean- ments of fetch-limited spectra. lournal of Marine Research ography 9:612-619. (ZZA) 25:292-32r.(+lt) Begemann, F., and W. F. Libby, 1957. Continental water bal- Barrett, I R., 1965. Subsurf.ace currents off Cape Hatteras. ance/ inventory of ground water storage times, surface ocean Deep-Sea Research 12:173-184. (Zl , I2I, 123) mixing rates and world-wide circulation patterns from cosmic -ray and bomb tritium . Geochimica et Cosmochimica Batchelor, G. K., 1953a. The Theory of Homogeneous Tur- Acta 12:277-296. (++t) bulence. Cambridge University Press, London , I97 pp. (t+t, 175, 543 ) Behringer, D. W., R. L. Molinari, and |. F. Festa, 1977. The variability of anticyclonic current patterns in the Gulf of Mex- Batchelor, G. K., 1953b. The conditions for dynamical simi- tco. [ourna] of Geophysical Research 82:5469-5476. (t ta) larity of motions of a frictionless perfect-gas atmosphere. Quarterly lournal of the Royal Meteorological Society Bell, T. H., L975. Topographically generated internal waves in 79:224-23s.(S+S ) the open ocean. lournal of Geophysical Research 80:32V327 . (aaz Batchelor, G. K., 1959. Small-scale variation of convected ) quantities like temperature in turbulent fluid. [ournal of Fluid Belyaev, V. S., M. M. Lubimtzev, and R. V. Ozmidov, 1975. Mechanics 5: I 13- 139. (ZSO) The rate of dissipation of turbulent energy in the upper layer of the ocean. lournal of Physical Oceanography 5:499-505. Bates, J. R., L970. Dynamics of disturbances on the Intertrop- (zsa ical Convergence Zone. Quafterly lournal of the Royal Me- ) teorological Society 96:677-7O1. (SOO) Bennett, E. 8., 1963. An oceanographic atlas of the eastern tropical Pacific Ocean, based on data from Eastropic Expedi- Beardsley, R. C., I 969. A labor atory model of the wind-driven tion, October-December 1955 . Interamerican Tropical Tuna ocean circulation. of Fluid Mechanics 38:25 5-272. lournal ( t+ (tsz, 469,470, 47r) Commissron Bulletin 8:31-165. ) Bennett, I. R., and B. A. Magnell, 1979. A dynamical analysis Beardsley, R. C., 1972. A numerical model of the wind-driven of currents near the New |ersey Coast. lournal of Geophysical circulation in a circular basin. Geophysical Fluid Dynamics I 165-117 5. (Z t S 3:2rr-243.(tsz) Research 84: ) Bernstein, R. L., and W. B. White, 1974. Time and length Beardsley,R. C., 1974. A note on some Antarctic Ocean model scales of baroclinic eddies in the central North Pacific Ocean. experiments. Department of Meteorology, Massachusetts In- lournal of Physical Oceanography 4:613-624. (eSl, 3721 stitute of Technology, Cambridg", Massachusetts, 12 pp. (Un- published manuscript. | (472> Bernstein, R. L., and W. B. White, L977 . ZonaI variability in the distribution of eddy energy in the mid-latitude North Beardsley, R. C., 1975. The 'sliced-cylinder' laboratory model Pacific Ocean. lournal of Physical Oceanography 7:123-126. of the wind-driven ocean circulation. Part 2. Oscillatory forc- (sso, 414) ing and Rossby wave resonance. lournal of Fluid Mechanics 69:4r-64.(+tZ) Bernstein, R. L., L.Breaker, and R. Whritner, L977. California Current eddy formation: Ship, arr, and satellite results. Sa- Beardsley, R. C., W. C. Boicourt, and D. V. Hansen, 1976. ence I 95 :353 -359 . (+Zl Physical oceanography of the Middle Atlantic Bight. In Middle I Atlantic Continental SheLf and the New York Bight, M. G. Berteaux, H. O., 1975. Buoy Engineering. Wiley, New York. Gross, ed., American Society of Limnology and Oceanography, 3repp. (+oz) Special Symposra, 2, pp. 2V34. (ZOl 208, 2I4, 227, 228> , BerteauX, H. O., and R. G. Walden, 1968. The mooring wire Beardsley, R. C., and B. Butman, L974. Circulation on the testing and evaluation programs for 1968. W.H.OJ. Technical New England Continental Shelf: response to strong winter Memorandum 7-68, Woods Hole Oceanographic Institution, storms. Geophysical Research Letters I : 181-184. (Zt+) Woods Hole, Massachusetts, 16 pp. (+tO)

Beardsley, R. C., and D. B. Haidvogel, 1980. A simple numer- BerteauX, H. O., and R. G. Walden , 1969. Analysis and exper- ical model for the wind-driven transient circulation in the imental evaluation of single point moored buoy systems. Middle Atlantic Bight. lournal of Physical Oceanography. W.H.O.I. Technical Report 69-36, Woods Hole Oceanographic (zzs) Institution, Woods Hole, Massachusetts, 5l pp. + Appendices. (+ro) Beardsley, R. C., H. Mofield, M. Wimbush, C. Flagg, and I. Vermersch, 1977. Ocean tides and weather-induced bottom Bien, G. S., N. W. Rakestraw, and H. E. Suess, 1963. Radio- pressure fluctuations in the Middle Atlantic Bight . lournal of carbon dating of deep water of the Pacific and Indian Oceans. Geophysical Research 82:3175*3182. (ZZZ, 327) In Radiocarbon Dating, International Atomic Energy Agency, Vienna, pp. 159-173. (449) Beardsley, R. C., and K. Robbins, 1975. The 'sliced-cylinder' laboratory model of the wind-driven ocean circulation. Part Bigelow, H. B., 1915. Exploration of the coast water between I. Steady forcing and topographic Rossby wave instability. Nova Scotia and Chesapeake Bay,luly and August, L913, by lournal of Fluid Mechanics 69:274O. (+ZZ) the U.S. Fisheries Schooner Grampus. Oceanography and plankton. Bulletin of the Museum of Comparative Zoology Beardsley, R. C., K. D. Saunders, A. C. Warn-Varnas, and 59:1 52-359. (ZOl, 2rO,2l I A. D. Harding, 1979. An experimental and numerical study of ) the secular spin-up of a thermally stratified rotating fluid. Bigelow, H. B., 1922. Exploration of the coastal water off the lournal of Fluid Mechanics 93:16 1-l 84. (+l e) northeastern United States in 1916 by the U.S. Fisheries Schooner Grampus. Bulletin of the Museum of Comparative Zoology 65:88-188. (ZOl, 2l I )

556 Reference List n cir- Bigelow, F{. 8., 1927. physical oceanography of the Gulf oJ Blandford, R. R., r97 r. Boundary conditions in homogeneous cean- Maine. Bulletin of the United States Bureau of Fisheries 40 ocean models. Deep-sea Research rg:789-7sr. (sq) (Part 2l:51 l-l 027. (ZOl, 23g) Blanton, r97 r. Exchange of Gulf stream r |., water with North bal- Bigelow, H. B., 1929. Report of the committee on oceanog- Carolina shelf water in Onslow Bay during stratified condi- tcean raphy of the National Academy of Sciences, National Acad- tions. Deep-Sea Research l8: I 67-179. (t from tl) emy of Sciences, Washington, D.C., 165 pp. (ZSe) mica Blanton, I. o., r97s. Potential energy fluctuations at the edge Bigelow, H. B., 1933. Studies of the waters on the continental of the North Carolina continental shelf. Deep-Sea Research shelf, cape cod to chesapeake Bay.I. The cycle of tempera- 22:559-s63.(rrl) The ture. 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(Numerical solution itern Atlantic waters of canada, I. Hiort, director, Department of of the distribution problem for the semidiurnal tidal waves (M, rcdi- the Naval servrce, l. de Labroquerie Tach6, ottawa, pp. 847- and sr) in the world ocean. "una 404. (233) Doklady of the Academy of sciences of the u.s.s.R., Earth Science Sections 172:7-9.1 (eZZ) Bierknes, 1., 1919. on the structure of moving cyclone s. Geo- Boicourt, w. lysis fysiske Publikasioner t:2, 8 pp. (SZI) c., 1973. The circulation of water on the conti- nental shelf from chesapeake ph.D. iical Bay to cape Hatteras. Bjerknes, 1., 1937. Die Theorie der Aussertropischen zyklo- Thesis, The |ohns Hopkins university, Baltimo re, Maryland, nenbuildung. Meteorologische Zeitschrift 54:46L-466.'(eoz, r83 pp. (zr+) lgth 509, 529) Boicourt, w. C., and P. w. Hacker, ean. 1976. Circulation on the Bjerknes, 1., 1955. Investigations of the general circulation of Atlantic continental shelf of the United States, cape May to the atmosphere. Final Report General Circulation proi ect, cape Hatteras. Mbmoires de la soci|te Royale des sciences AF 19(122)-48, Department of Meteorology, yin Llniversity of cal- de LiD,ge,Sixib,me Serie 10:l g7-200. (2t4, ZI9, 222) lrth ifornia at Los Angeles. (SOZ) Bolin,8., 1950. on the influence 126. of the earth,s orography on Bjerknes, 1., 1957. Large scale synoptic processes. Final Report the general character of the westerlies. Tellus 2:lgLL95. General circulation Proiect, AF 19(604)-1286, Department of (szz) mia Meteorology, university of california at Los Angeles. (soz) Bolin, B., 1955. Numerical forecasting with the barotropic Sci- Bjerknes, ., 1969. I Atmospheric teleconnections from the model. Tellus 7:2749. (SOS) equatorial Pacific. Monthly weather Review 97:168-172. Bolin, B., and E. Eriksson, r9s9. lrk. (351,353,496) changes in the carbon dioxide content of the atmosphere and sea due to fossil fuel combus- Bferknes,I., and H. solberg, l9zr. Meterological conditions for tion. rn The Atmosphere and the sea in Motion. scientific publikasioner nre the formation of rain. Geofysiske 2:8, 6r pp. contributions (szt) to the Rossby Memorial volume, B. Bolin, ed., 'cal Rockefeller Institute press, New york, pp. laO-r48. (++l) OD, Bjerknes, 1., and H. solberg, Lg2z. Life cycle of cyclones and Bolin, 8., and H. Stommel, lg6L on the abyssal circulation the polar front theory of atmospheric circulation. Geofysiske of the world ocean.-rv. origin and rate of circulation of Publikasioner 3:1, t8 pp. (SZO) )er- deep ocean water as determined with the aid of trace rs. Deep- ns. Sea Research 8:95-t Bjerknes, v., 1898. Ueber einen hydrodynamischen Funda- 10. (+aS) hic mentalsatz und seine Anwend*g besonders auf die Mechanik Booker, I. R., and F. P. Bretherton, 1967. The critical layer for )es. der Atmosphlre und des weltmeere s. Kongliga svenska ve- internal gravity waves in a shear flow. of Fluid Me- tenskaps-Akademiens Toumal Handlingar, Ny Folid Br:4, 85 pp. (zot, chanics 27:513-539 . (ZZ+) lio- 233) Born, G.H., J. A. Dunne, and D. B. Lame, r97g. seasat mission ns. Bjerknes, v., Bjerknes, I. H. Solberg, and T. Bergeron, 193g. overview. Science 2O4: CY, 1405-1 406. (+Ze) Physikalische Hydrodynamik. Mit Anwendung-auf d.ie Dy- Bowden, K. F., namische Meterologie. springer, Berl rn, 797 pp. (zos) L962. Turbulence. rn The sea: Ideas and. ob- servations on Progress rn the study of the seas, r: physical )en Blackadar, A. K., and H. Tennekes, 196g. Asymptotic simi- oceanography, M. by N. Hill, ed., wiley, Interscience, New larrty in neutral barotropic planetary boun d^ry layers. York, pp. lournal 802-825 . (ZSS, 25g ) rnd of the Atmospheric sciences 25:1015-1020. (soz) ,8y Bowden, K. F., 1953. The mixing processes in a tidal estuary. Blandford, R. R., 196s. Notes on the theory of the thermocline. International lournal of Air and water pollution 7:848-856. lournal of Marine Research 2B:Ig-29. (tSl) (zo+) :he Blandford, R., 1966. Mixed gravity-Rossby waves in the ocean. ies Bowden, K. F., r96s. Horizontal mixing in the sea due to a Deep-SeaResearch 13:941-96I. (tlt SZ7) i.ve , shearing current. lournal of Fluid Mechanics 2l:g3-95. (azs)

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Pettersson, H., 1931. Eddy-viscosity in stratified water. Gdte- Phillips, O. M., I966b. The Dynamics of the Upper Ocean, borgs Kungliga Vetenskaps-och Vitterhets-Samhiilles Hand- l st ed. Cambridge University Press,London , 261 pp. (ZeS, lingar, Femte Foliden, Serien B 2:L,21 pp. (t+O) 275, 348) Pettersson, H., 1955. Manganese nodules and oceanic radium. Phillips, O. M., L97O.On flows induced by diffusion in a Papers in Marine Biology and Oceanography, Deep-Sea Re- stably stratified fluid. Deep-SeaResearch 17:435443. (ZeO) search 3 (Supplement 335-3 45 . (444) ): Phillips, O. M., L972. Turbulence in a stratifted fluid-is it Philander, S. G. H., 1973 Equatorial Undercurrent: Measure- unstable?.Deep-Sea Research L9:79-8I. (Z+l) ments and theories. Reviews of Geophysrcs and Space Physics Phillips, O. M., I977a. The Dynamics Upper 11:513-570. ( tA+, 185, r9r, 527) of the Ocean, 2nd ed. Cambridge University Press,London, 336 pp. (Z+5, Philander, S. G. H., 1976. Instabilities of zonal equatorial 250,265, 268, 273, 274, 346,49r, 492,4%) currents. lournal of Geophysical Research 8 I :3 725-3735. (rra) Phillips, O. M., I977b. Entrainment. In Modelling and Pre- diction of the Upper Layers of the Ocean, E. B. Kraus, ed., Philander, S. G. H., L978. Forced oceanic waves. Reviews of PergamonPress, Oxford, pp. 92-101. (244) Geophyslcs and Space Physics 16:1546. (eO+, 347> Phillips, O. M., L977c. The sea surface. In Modelling and Philander, S. G. H., L979. Equatorial waves in the presence of Prediction of the Upper Layers of the Ocean, E. B. Kraus, ed., the Equatorial Undercurrent. lournal of Physical Oceanogra- PergamonPress, Oxford, pp. 229-231. (Z+Z). phy 9:254-262.0 93) Pickard, G. L., and K. Rodgers,1959. Current measurements Philander, S. G. H., 1980. The equatorial undercurrent revis- in Knight Inlet, British Columbia. lournal of the Fisheries ited. Annual Review of Earth and Planetary Sciences 8. (SZll ResearchBoard of Canada 16:635-678.(ZOel

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Phillips, N. A., L966a. The equations of motion for a shallow Pingree, R. D., 1972. Mixing in the deep stratified ocean. rotating atmosphere and the "traditional approximation. " Deep-SeaResearch L9549-561. (g+) of the Atmosphefic Sciences 23:626-628. (t+e, 165) lournal Pingree,R. D., 1973.A component of LabradorSea water in Phillips, N., I966b. Large-scale eddy motion in the western the Bay of Biscay.Limnology and Oceanography18:711-718. Atlantic. lournal of Geophysical Research 71:3883-3891. (a+) (zls, B4L,gs9, 533 ) Pingree, R. D., 1978. Mixing and stabilization of phytoplank- Phillips, N. A., 1968. Reply [to Veronis (1968)]. Iournal of the ton distributions on the northwest European continental Atmospheric Sciences 25:1155-l L57. (ZlSl shelf. In Spatial Pattern in Plankton Communities, l. H. Steele, ed., Plenum Press, New York, pp. 18L-220. (UA, 379> Phillips, N. A., 1973. Principles of large scale numerical weather prediction. In Dynamic Meteorology, P. Morel, ed., Pingree, R. D., P. M. Holligan, and R. N. Head, 1977. Survival D. Reidel, Dordrecht, pp.. 128-141 . (5 I 8 ) of dinoflagellate blooms in the western English Channel. Na- ture 265:266-261. (aAO, 381) Phillips, O. M., L957. On the generation of waves by turbulent wind. lournal of Fluid Mechanics 2:417445. (+O+l Pingree, R. D., and G. K. Morrison, 1973. The relationship between stability and source waters for a section in the north- Phillips, O. M., 1958. The equilibrium range in the spectrum east Atlantic. lournal of Physical Oceanography 3:28G-285. of wind-generated waves. lournal of Fluid Mechanics 4:42G 434.(zes) (s+) Pinkel, R., I 97 5. Upper ocean internal wave observations from Phillips, O. M., 1963. On the attenuation of long gravity waves FLIP. lournal of Geophysical Research 80:3892-3910. (ZeS, by short breaking waves. lournal of Fluid Mechanics 16:321- 332.(+s+) 28s)

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