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SWALLOW, J.C. (1983). Arabian Sea cooling and relationship with monsoon. CCCO Panel onIndian Ocean Climate Studies, Report of the First Session, 21-23 March 1983, Paris.SWALLOW, J.C. (1985). Assessment of relative importance of processes responsible for theseasonal cycle of SST and mixed layer depth in the Arabian Sea. CCCO Panel on IndianOcean Climate Studies, Report of the Second Session, 28-31 Jan 1985, New Delhi.WYRTKI, K. (1971).<strong>Oceanographic</strong> Atlas of the International Indian Ocean Expedition. NationalScience Foundation, U.S. Government Printing Office, 531 pp.232
Table 1.Distribution of the depth of 20°C isotherm in the Central North ArabianSea and monsoon discharge in August in River Indus..........................................................................................................................Year1962196319641965196619671968196919701971197219731974197519761977197819791980198 119821983.Depth of 20°CIsotherm (May)(Meters)150200200Location-----22'N, 61'E---2WN, 6YE-8"N, 10"N50"E, 60'E61"N, 18'N50"E, 60"E8"N, 9"NWE, 60"E19"N, 20'N50'E, 60'E--21"N, 22'N62"EIndus dischargein Au ust(km 5 )17.318.925.317.330.336.227.723.49.212.47.639.13.321.438.118.246.416.411.417.96.926.6233
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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
Page 174 and 175: Temperature and SalinityThe effects
Page 176 and 177: significant numbers in the Red Sea,
Page 178 and 179: mersas are known to serve as nurser
Page 180 and 181: BURCHARD, J.E. (1979). Coral fauna
Page 182 and 183: HIRTH, H.F., KLIKOFF, L.G. and HARP
Page 184 and 185: MacNAE, W. (1974). Mangrove forests
Page 186 and 187: 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 214 and 215: 221
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 226 and 227: 234
Page 228 and 229: 236
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 238 and 239: UELEVATIONS (m) ai 18 HOURS L2:-+EL
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
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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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