[Variation in the absolute density of water—pure water and seawater—as a function of isotopic...
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OLR(1979)26(12) A. Physical Oceanography 761 Mission, Aug. 1972-Nov. 1975--Service Hydro- graphique et Oceanographique de la Marine, France.] A n nls h.vdrogr., (5)6(3)(750): 79-183. 79:5864 Milard, F., 1978. Mission Hydrographique de Nouvelle-Cahktonie (janvier 1972-mai 1974). [New Caledonia Hydrographic Mission of the Service Hydrographique et Oceauographique de la Marine, France, Jan. 1972-May 1974.] Annls hydrogr., (5)6(2)(749): 87-143. 79:5865 Schrumpf, B., 1978. Mission Oc6anographique de I'Atlantique (octobre 1972-octobre 19747. [Atlan- tic Oceanographic Mission of the Service Hydro- graphique et Oceanographique de la Marine, France, in the northeast Atlantic, Oct. 1972- Oct. 1974.] Annls hydrogr., (5)6(2)(749): 29-86. 4. Distribution of common oceanic (hy- drographic) properties (see Chemical Oceanography for basic chemical studies of salinity, chlorinity, etc.) 79:5866 Donguy, J.-R. and Christian Henin, 1978. The navi- facial salinity in the tropical south-west Pacific Ocean. Cah. ORSTOM, S~r. Oc~anogr., 16(2): 107-136. Navifacial data from 1956-1973 are combined to produce seasonal surface salinity charts for the south- west tropical Pacific Ocean during this period. Variations in navifacial water masses and potential biological applications are discussed. Figures include 41 navifacial salinity charts. O.R.S.T.O.M., B.P. A5, Noum~a-Cedex, New Caledonia. (rio) 79:5867 Korchashkin, N. N., I. D. Lozovatsky and R. V. Oz- midov, 1979. Variability of the fine vertical struc- ture of the temperature field in the western part of the Pacific Ocean. (In Russian: English abstract.) Okeanologiia, 19(2): 197-205. A great number of inversions was recorded in the vertical structure of the lower (300-590 m) layer of the thermocline; time scale of the meso-scale formation variability did not exceed 12 minutes. Fine structure deformation in the upper layer (70-300 m) was mostly reversible; the time scale of coherence of the meso- scale inhomogeneities of separate profiles was about 60 minutes. Spectral forms of fine structure variabilities and variability differences in the two layers are discussed. (smf) 79:5868 Rebert, J. P., 1978. Variabilit~ des conditions de surface dans rupwelling ouest-africain. [Variabil- ity of surface conditions in the West African Up- welling.] Doc. scient. Cent. Rech, oc~anogr., Dakar-Thiaroye, 67(100): 27 pp. Wind fluctuations along the West African coast are correlated with sea-surface temperatures for the years 1967-1976. Wind-induced coastal upwelling accounts for about 50% of the observed variation in sea-surface temperature; however, monthly sea-surface temperature anomalies are the function of wind conditions north of the area of observation rather than a function of local winds. Oc6anographe physicien de I'O.R.S.T.O.M.C.R.O.D.T., B.P. 2241 DAKAR, Senegal. (smf) 5. Physical processes (diffusion, turbu- lence, energy exchange, dynamic heights, etc. ) 79:5869 Griffiths, R. W., 1979. The transport of multiple com- ponents through thermohaline diffusive interfaces. Deep-Sea Res., 26(4A): 383-397. Simultaneous fluxes of 3 salts through the 'diffusive' interface of thermohaline convection were determined in the laboratory. Transport coefficients reflected the different travel rates for individual species, and coefficient ratios were found to vary faster than molecular diffusivity ratios. Field observations at Lake Kivu supported the laboratory results. Figures include interfacial shadowgraphs. Research School of Earth Sciences, The Australian National University, Canberra ACT, Australia. (rio) 79:5870 Menache, M., C. Beauverger and G. Girard, 1978. Etude de la variation de la masse volumique de l'eau (eau pure et eau de mer) en fonction de la composition isotopique et de la teneur en gaz atmosph~riques dissous. [Variation in the abso- lute density of water--pure water and seawater-- as a function of isotopic composition and dissolved gas content.] Annls hvdrogr.. (5)6(3)(750): 37-76. The isotope composition of natural waters is discussed, and a relationship is proposed for calculating the absolute density difference between waters in terms of their 0-18 and H-2 contents. The relationship is confirmed by a hvdrostatic weighing method. Kinetic studies show oxygen and nitrogen dissolve at the same rate in water, lnstitut Oc6anographique, Paris, France. (djh) 79:5871 Posmentier, E. S. and J. M. Raymont, 1979. Varia- tions of longitudinal diffusivity in the Hudson Estuary [New York], Estuar. coast, mar. Sci.. 8(6): 555-564.
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OLR(1979)26(12) A. Physical Oceanography 761
Mission, Aug. 1972-Nov. 1975--Service Hydro- graphique et Oceanographique de la Marine, France.] A n nls h.vdrogr., (5)6(3)(750): 79-183.
79:5864 Milard, F., 1978. Mission Hydrographique de
Nouvelle-Cahktonie (janvier 1972-mai 1974). [New Caledonia Hydrographic Mission of the Service Hydrographique et Oceauographique de la Marine, France, Jan. 1972-May 1974.] Annls hydrogr., (5)6(2)(749): 87-143.
79:5865 Schrumpf, B., 1978. Mission Oc6anographique de
I'Atlantique (octobre 1972-octobre 19747. [Atlan- tic Oceanographic Mission of the Service Hydro- graphique et Oceanographique de la Marine, France, in the northeast Atlantic, Oct. 1972- Oct. 1974.] Annls hydrogr., (5)6(2)(749): 29-86.
4. Distribution of common oceanic (hy- drographic) properties (see Chemical Oceanography for basic chemical studies of sal ini ty, chlor ini ty , etc.)
79:5866 Donguy, J.-R. and Christian Henin, 1978. The navi-
facial salinity in the tropical south-west Pacific Ocean. Cah. ORSTOM, S~r. Oc~anogr., 16(2): 107-136.
Navifacial data from 1956-1973 are combined to produce seasonal surface salinity charts for the south- west tropical Pacific Ocean during this period. Variations in navifacial water masses and potential biological applications are discussed. Figures include 41 navifacial salinity charts. O.R.S.T.O.M., B.P. A5, Noum~a-Cedex, New Caledonia. (rio)
79:5867 Korchashkin, N. N., I. D. Lozovatsky and R. V. Oz-
midov, 1979. Variability of the fine vertical struc- ture of the temperature field in the western part of the Pacific Ocean. (In Russian: English abstract.) Okeanologiia, 19(2): 197-205.
A great number of inversions was recorded in the vertical structure of the lower (300-590 m) layer of the thermocline; time scale of the meso-scale formation variability did not exceed 12 minutes. Fine structure deformation in the upper layer (70-300 m) was mostly reversible; the time scale of coherence of the meso- scale inhomogeneities of separate profiles was about 60 minutes. Spectral forms of fine structure variabilities and variability differences in the two layers are discussed. (smf)
79:5868 Rebert, J. P., 1978. Variabilit~ des conditions de
surface dans rupwelling ouest-africain. [Variabil- ity of surface conditions in the West African Up- welling.] Doc. scient. Cent. Rech, oc~anogr., Dakar-Thiaroye, 67(100): 27 pp.
Wind fluctuations along the West African coast are correlated with sea-surface temperatures for the years 1967-1976. Wind-induced coastal upwelling accounts for about 50% of the observed variation in sea-surface temperature; however, monthly sea-surface temperature anomalies are the function of wind conditions north of the area of observation rather than a function of local winds. Oc6anographe physicien de I 'O.R.S.T.O.M.C.R.O.D.T. , B.P. 2241 DAKAR, Senegal. (smf)
5. Physical processes (diffusion, turbu- lence, energy exchange, dynamic heights, etc. )
79:5869 Griffiths, R. W., 1979. The transport of multiple com-
ponents through thermohaline diffusive interfaces. Deep-Sea Res., 26(4A): 383-397.
Simultaneous fluxes of 3 salts through the 'diffusive' interface of thermohaline convection were determined in the laboratory. Transport coefficients reflected the different travel rates for individual species, and coefficient ratios were found to vary faster than molecular diffusivity ratios. Field observations at Lake Kivu supported the laboratory results. Figures include interfacial shadowgraphs. Research School of Earth Sciences, The Australian National University, Canberra ACT, Australia. (rio)
79:5870 Menache, M., C. Beauverger and G. Girard, 1978.
Etude de la variation de la masse volumique de l'eau (eau pure et eau de mer) en fonction de la composition isotopique et de la teneur en gaz atmosph~riques dissous. [Variation in the abso- lute density of water--pure water and seawater-- as a function of isotopic composition and dissolved gas content.] Annls hvdrogr.. (5)6(3)(750): 37-76.
The isotope composition of natural waters is discussed, and a relationship is proposed for calculating the absolute density difference between waters in terms of their 0-18 and H-2 contents. The relationship is confirmed by a hvdrostatic weighing method. Kinetic studies show oxygen and nitrogen dissolve at the same rate in water, lnstitut Oc6anographique, Paris, France. (djh)
79:5871 Posmentier, E. S. and J. M. Raymont, 1979. Varia-
tions of longitudinal diffusivity in the Hudson Estuary [New York], Estuar. coast, mar. Sci.. 8(6): 555-564.
