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UELEVATIONS (m) ai 18 HOURS L2:-+ELEVATIONS (m) at 24 "iHOURSFigure 5. Distribution of storm surge heights (from MURTY and EL-SABH, 1984).Figure 6. Temperature-salinity diagram for Inner Gulf Waters. Thesquare symbols indicate Station 2365 in the Gulf of Oman;open circles indicate overlapping data points; February1977 (from BREWER and DYRSSEN, 1985).246
I R A NARABIA26"-24'-INNER GULF, KAP REGIONATLANTIS II 93LEG 17SUlNllV %e48' 50'I I I 1 I I52" 54' 56' 58'STATION W.looI20Figure 7.a) Map of surface salinity within the Gulf;b) Vertical salinity section along the major ax isof the Gulf (from BREWER and DYRSSEN, 1985).247
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Intergovernmental Oceanographic Com
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of the IOC Marine Pollution Monitor
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PageMARGINAL SEASSTORM SURGES IN TH
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Marine PollutionAt present, marine
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THE INDIAN OCEAN --- AN ENVIRONMENT
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The subtropical anticyclonic gyre i
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GEOLOGICALBecause of its asymmetric
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RADIOACTIVE AND THERMAL WASTESIn co
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RESEARCH AND MONITORING ACTIVITIESM
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2-5, Mn 3-7, Zn 8-31, Fe 35-94, Pb
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Localized problems, both short-term
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HOLEMAN, J.N. (1968). The sediment
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UNEP/UNIDO (1982a). Industrial sour
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0-5-24 -I I I I I I I I I 11--25- A
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I*in '0( U N '0- '0 '0 N , p d'0I I
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C'EO IIFigure 6. Observations of oi
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Table 2.Ranges of Dissolved heavy m
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d.2 W2n2 n z0U.IzIO N m mENmIYEE*Ed
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Table 6. Population and related dat
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PROBLEMS IN THE PHYSICAL OCEANOGRAP
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B2: How does the Agulhas Current in
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0Q0mbWbvx(U49
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Figure 6 Average wind stress curl f
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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).
Page 188 and 189: WALKER, D.I. and ORMOND, R.F.G. (19
Page 190 and 191: DAMMING AND DIVERSION OF RIVERSIn d
Page 192 and 193: FUTURE STUDIESWhat can marine scien
Page 194 and 195: !0OD9 -8 Nc80,a,u-3(dcab(Dbrr)8brr)
Page 196 and 197: 0 0-0 00 O0O 0% LD d- m cu 0 0202
Page 198 and 199: STORM SURGES IN THE BAY OF BENGAL*T
Page 200 and 201: low pressure centres over the Bay i
Page 202 and 203: ACKNOWLEDGEMENTSThe writers wish to
Page 204 and 205: Table 1.Latitude and longitude of p
Page 207 and 208: 214
Page 209 and 210: 0Poa9nU0m0Yan-I2li7mYUVQk?401mc0mYm
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Page 216 and 217: Table 3. Nomenclature used by India
Page 218 and 219: ANDHRAB A Y OFB E N G A L ,.16'LO 4
Page 220 and 221: INDIABAY OF-Point CalirnereLanka L-
Page 222 and 223: pressure in the South Pacific and l
Page 224 and 225: SWALLOW, J.C. (1983). Arabian Sea c
Page 226 and 227: 234
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Page 230 and 231: scale wind phenomenon that occurs w
Page 232 and 233: Several two-dimensional models of t
Page 234 and 235: HARTMANN, M., LANGE, H., SEIBOLD, E
Page 236 and 237: Y-Model Domaint=6hrs.b-250 0 59 Xw-
Page 240 and 241: HARMONIC CONSTITUENT K,Figure 8. Ob
Page 242 and 243: Age of Semi-Diurnal Tide (hrs)28".+
Page 244 and 245: ! 5"BOTTOMFigure 13. Predicted mode
Page 246 and 247: OCEANOGRAPHIC CONDITIONS PELAGIC PR
Page 248 and 249: Low oxygen content in subsurface wa
Page 250 and 251: R/V Dr. F. Nansen trawl of 41 m hea
Page 252 and 253: thermocline temperature decreases s
Page 254 and 255: Nitrate - NitrogenSimilarly to phos
Page 256 and 257: The maximum standing stocks in the
Page 258 and 259: By April/May the demersal stocks ha
Page 260 and 261: in 6 months when spawning occurs. T
Page 262 and 263: REFERENCES3BANSE, K. (1968). Hydrog
Page 264 and 265: GILSON, H.C., (1937). The nitrogen
Page 266 and 267: ROYAL SOCIETY (1963). International
Page 268 and 269: APPENDIX:REGIONAL COOPERATIVE INVES
Page 270 and 271: 20 015 20 25FEBOC015 20 25 30 35M A
Page 272 and 273: W0-8w0-Inww[r3a+eW281
Page 274 and 275: B35 36 a7 XlO+ 35 36 a7- Mar--- Fob
Page 276 and 277: a, A
Page 278 and 279: ...... :'I. .. ,... .. 8.*.. ... ._
Page 280 and 281: ASTAT.Si -Si (OH14 in p M - d ~ n -
Page 282 and 283: YU0IwYY->02(33-1 II 1amLyY>02(33amL
Page 284 and 285: I I I I I10 Ic L0U0mI(dw -rlo u0w m
Page 286 and 287: 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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