139736eo.pdf (20MB) - Japan Oceanographic Data Center

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TABLE OF CONTENTSINTRODUCTIONMARINE ENVIRONMENT OF THE INDIAN OCEANTHE INDIAN OCEAN - AN ENVIRONMENTAL OVERVIEWby R. Sen Gupta and S.Z. QasimPROBLEMS INTHE PHYSICAL OCEANOGRAPHY OF THE INDIANOCEANby E.B. KrausPHYSICAL OCEANOGRAPHY OF THE NORTHERN INDIAN OCEAN -A PERSPECTIVE (Abstract)by V.V. VaradachariTHE DESTRUCTION OF THE TETHYS ANDPALEOCEANOGRAPHIC DEVELOPMENT OF THE INDIAN OCEANby B.U. HaqGEOLOGICAL-GEOPHYSICAL MAPPING OF THE INDIAN OCEANby N.N. Turko, G.B. Udintsev and D.I. ZhivAN EXAMINATION OF THE FACTORS THAT INFLUENCE THEMONTHLY-MEAN SEA LEVEL ALONG THE COAST OF INDIAby S.R. Shetye and A.M. AlmeidaRED TIDES IN THE INDO-WEST PACIFIC REGIONby G.M. HallegraeffECONOMIC AND POLLUTION ASPECTSMINERAL RESOURCES OF THE INDIAN OCEAN ANDRELATED SCIENTIFIC RESEARCHby H.N. Siddiquie, A.R. Gujar, N.H. Hashimi, A.B. Valsangkarand B. NagendernathRESEARCH NEEDS FOR THE CORAL REEF ECOSYSTEMS OFTHE CENTRAL INDIAN OCEANby M.W.R.N. de SilvaSTATUS OF CRITICAL MARINE HABITATS IN THE INDIAN OCEANby R. OrmondRISING SEA LEVEL AND CHANGING SEDIMENT INFLUXES:REAL AND FUTURE PROBLEMS FOR INDIAN OCEAN COASTALNATIONSby J.D. MillimanPage37943535581871051211231531671951
PageMARGINAL SEASSTORM SURGES IN THE BAY OF BENGALby T.S. Murty, R.A. Flather and R.F. HenryCIRCULATION AND PHYSICAL PROCESSES OF THE ARABIANSEA AND THEIR RELATIONSHIP WITH SOUTHWJZST MONSOONAND PRODUCTIVITYby G.S. QuraisheeA REVIEW OF THE PHYSICAL OCEANOGRAPHIC CHARACTERISTICSIN THE ARABIAN GULF 237by T.S. Murty and M.I. El-SabhFISHERY RESOURCES IN THE NORTH ARABIAN SEA AND ADJACENTWATERS (Abstract) 253by S.C. VenemaOCEANOGRAPHIC CONDITIONS, PELAGIC PRODUCTIVITY ANDLIVING RESOURCES IN THE GULF OF ADEN255by J. Stirn,R. Edwards, J. Piechura, M. Savich, M. Ghaddaf, M. Fadel, F. Mutlaq,0. Sabih, A. Sayed, S. Shaher and Z. ZubairiRED SEA BIOLOGICAL OCEANOGRAPHY AND RELATEDPROBLEMSby H. Thiel and H. WeikertTHE CRUST BENEATH THE RED SEA - GULF OF ADEN RIFTSYSTEM: A REVIEWby H.K. Wong and E.T. DegensSEDIMENTARY STRUCTURE OF THE NORTHERN RED SEAPREPARATION OF Al: 1,000,000 BATHYMETRIC CHART OF THENORTHERN RED SEA AND STUDY OF THE MORPHOSTRUCTURALFRAMEWORK BY CARTOGRAPHIC ANALYSIS (Abstract)by A. Ferragne, R. Griboulard, R. Prud'Homme, J-M. Ratel and M. VigneauxSURFICIAL SEDIMENTS OF NORTHERN RED SEAby M. Kh. El-SayedMARINE LIVING RESOURCES OF THE RED SEAby A.R. Bayoumi2032052292993073393413592
Page 1 and 2: Intergovernmental Oceanographic Com
Page 3: of the IOC Marine Pollution Monitor
Page 9 and 10: Marine PollutionAt present, marine
Page 11 and 12: THE INDIAN OCEAN --- AN ENVIRONMENT
Page 13 and 14: The subtropical anticyclonic gyre i
Page 15 and 16: GEOLOGICALBecause of its asymmetric
Page 17 and 18: RADIOACTIVE AND THERMAL WASTESIn co
Page 19 and 20: RESEARCH AND MONITORING ACTIVITIESM
Page 21 and 22: 2-5, Mn 3-7, Zn 8-31, Fe 35-94, Pb
Page 23 and 24: Localized problems, both short-term
Page 25 and 26: HOLEMAN, J.N. (1968). The sediment
Page 28 and 29: UNEP/UNIDO (1982a). Industrial sour
Page 30 and 31: 0-5-24 -I I I I I I I I I 11--25- A
Page 32 and 33: I*in '0( U N '0- '0 '0 N , p d'0I I
Page 34: C'EO IIFigure 6. Observations of oi
Page 38 and 39: Table 2.Ranges of Dissolved heavy m
Page 40 and 41: d.2 W2n2 n z0U.IzIO N m mENmIYEE*Ed
Page 42 and 43: Table 6. Population and related dat
Page 44 and 45: PROBLEMS IN THE PHYSICAL OCEANOGRAP
Page 46: B2: How does the Agulhas Current in
Page 50 and 51: 0Q0mbWbvx(U49
Page 52 and 53: Figure 6 Average wind stress curl f
Page 54 and 55:
THE DESTRUCTION OF THE TETHYS AND P
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part of the Seychelles-Mascarene bl
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Much of the old Tethys seafloor has
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when there was little or no movemen
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scouring of the sediments by cold b
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CANDE, S.C. and MUTTER, J.C. (1982)
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SHACKLETON, N.J. and KENNETT, J.P.
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0EYNz 10c2XaYWeKB20LuUz a5 cl300 10
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CALCAREOUS FORAMINIFERANANNOFOSSIL
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GEOLOGICAL-GEOPHYSICAL MAPPING OF T
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The latest tectonic generalization
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LE PICHON, X. and HEIRTZLER, J.R. (
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AN EXAMINATION OF THE FACTORS THAT
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is the specific volume anomaly. Po
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circulation. At Nagappattinam, Madr
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Table 1.MarmagaoCochin1969-781958-7
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tFigure 2. An idealized coastal cur
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STATION : BOMBAY~ J , F I M .- , A
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STATION : COCHIN, J , F , M , A , M
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3007STATION : MADRASI J I F , M I A
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STATION : CALCUTTA, J l F , M , A ,
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RED TIDE§ IN THE INDO-WEST PACIFIC
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were observed as early as 1770 duri
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diarrhetic shellfish poisoning (DSP
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GACUTAN, R.Q., TABBU, M.Y., AUJERO,
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Table 1.Clinical symptoms of variou
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Table 3. Fish species implicated in
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FIGURE CAPTIONSFigure la. Trichodes
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(*14aEE15aHH15c120
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MINERAL RESOURCES OF THE INDIAN OCE
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tonnes of monazite. Similar deposit
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Madagascar and the Red Sea. Within
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South Australian Basin: (Figs. 10-1
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Offshore placers are likely to occu
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MILLIMAN, J.D. (1974). Marine Carbo
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Thailand Tin 5560 (1980) NA 4.2 (19
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Table 2. The range (in percent) of
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Table 4. Chemical composition of po
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141FIGURE - 1
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~IT 73qw p' le' IS IFigure 4. Map s
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@A5 3 9 93 3 s 3 m4P 8O C ' . .' ,
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Figure 10. Map showng the abundance
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Figure 14. Map showing the distribu
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IFigure 17. Marine mineral explorat
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central are corals to the integrity
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Very little information is availabl
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leaving little trace of their exist
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REFERENCESAGASSIZ, A. (1903). The c
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PILLAI, C.S.G. (1969b). Studies on
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Table 1.Extent of damage to coral r
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STATUS OF CRITICAL MARINE HABITATS
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OCCURRENCEThe distribution of reefs
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Mining of Reef RockMining of reef r
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-resource. Their significance deriv
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Coating of Aerial Roots by Fine Sed
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associated with the roots (e.g. GOE
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Temperature and SalinityThe effects
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significant numbers in the Red Sea,
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mersas are known to serve as nurser
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BURCHARD, J.E. (1979). Coral fauna
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HIRTH, H.F., KLIKOFF, L.G. and HARP
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MacNAE, W. (1974). Mangrove forests
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RINKEVITCH, B. and LOYA, Y. (1977).
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WALKER, D.I. and ORMOND, R.F.G. (19
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DAMMING AND DIVERSION OF RIVERSIn d
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FUTURE STUDIESWhat can marine scien
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!0OD9 -8 Nc80,a,u-3(dcab(Dbrr)8brr)
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0 0-0 00 O0O 0% LD d- m cu 0 0202
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STORM SURGES IN THE BAY OF BENGAL*T
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low pressure centres over the Bay i
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ACKNOWLEDGEMENTSThe writers wish to
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Table 1.Latitude and longitude of p
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214
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0Poa9nU0m0Yan-I2li7mYUVQk?401mc0mYm
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0In218
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221
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Table 3. Nomenclature used by India
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ANDHRAB A Y OFB E N G A L ,.16'LO 4
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INDIABAY OF-Point CalirnereLanka L-
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pressure in the South Pacific and l
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SWALLOW, J.C. (1983). Arabian Sea c
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234
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236
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scale wind phenomenon that occurs w
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Several two-dimensional models of t
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HARTMANN, M., LANGE, H., SEIBOLD, E
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Y-Model Domaint=6hrs.b-250 0 59 Xw-
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UELEVATIONS (m) ai 18 HOURS L2:-+EL
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HARMONIC CONSTITUENT K,Figure 8. Ob
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Age of Semi-Diurnal Tide (hrs)28".+
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! 5"BOTTOMFigure 13. Predicted mode
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OCEANOGRAPHIC CONDITIONS PELAGIC PR
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Low oxygen content in subsurface wa
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R/V Dr. F. Nansen trawl of 41 m hea
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thermocline temperature decreases s
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Nitrate - NitrogenSimilarly to phos
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The maximum standing stocks in the
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By April/May the demersal stocks ha
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in 6 months when spawning occurs. T
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REFERENCES3BANSE, K. (1968). Hydrog
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GILSON, H.C., (1937). The nitrogen
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ROYAL SOCIETY (1963). International
Page 268 and 269:
APPENDIX:REGIONAL COOPERATIVE INVES
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20 015 20 25FEBOC015 20 25 30 35M A
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W0-8w0-Inww[r3a+eW281
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B35 36 a7 XlO+ 35 36 a7- Mar--- Fob
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a, A
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...... :'I. .. ,... .. 8.*.. ... ._
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ASTAT.Si -Si (OH14 in p M - d ~ n -
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YU0IwYY->02(33-1 II 1amLyY>02(33amL
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I I I I I10 Ic L0U0mI(dw -rlo u0w m
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III I I I0. 1....w'3...-0U-J..,....
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297
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clearly is too low. Because of low
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KARBE, L., THIEL, H., WEIKERT, H. a
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50010001 scoOxygen (rnl/l)0I1I2I3I4
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c1 oc50C10001500_j_///.///II:I? 0:3
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THE RED SEAPHYSIOGRAPHYThe Red Sea
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intensity of magnetization which co
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1969; SEARLE and ROSS, 1975). This
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y normal faulting. This is most int
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South of 19"N, the McKENZIE pole no
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BAUMANN, A., RICHTER, H. and SCHOEL
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EYAL, M., EYAL, Y., BARTOV, Y. and
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LEWIS, B.T.R. (1983). The process o
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TARLING, D.H. and MITCHELL, J.G. (1
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mC- 1000- 2000- 3000E0Figure 2.Sche
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-20b-0,20wFigure 4. Seismicity and
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kmaFigure 6. Summary of seismic ref
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kQ)Um 5U0c04 3N 4COQ)k3M*rlk332
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5 b'o w-Y EO'i Ii04!I 0I0I334
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II,'{34/,'0SOMALIAND: N. DANAKILFig
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spreadingvulcanismmblock faultingII
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SUPERFICIAL SEDIMENTS OF NORTHERN R
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normally sorted, with median diamet
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EL-SAYED (1983) used the trace meta
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BEHAIRY, AKA. (1983). Marine transg
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SHUKRI, N.M. (1953). Bottom deposit
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Table 2 Heavy metal concentrations
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EGYPTEl-Morgan 1Bargan IBargan 2Yub
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Figure 4. Distribution of minerals
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ARAGONITEHIGH HG-CALCITEFigure 6. T
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MARINE LIVING RESOURCES OF THE RED
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This elevated productivity may resu
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REVELLE (1981) mentioned that the p
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FISHELSON, L. (1964). Observation o
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