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

More documents

Recommendations

Info

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
Page 1 and 2:
Intergovernmental Oceanographic Com
Page 3 and 4:
of the IOC Marine Pollution Monitor
Page 5:
PageMARGINAL SEASSTORM SURGES IN TH
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
Page 56 and 57:
part of the Seychelles-Mascarene bl
Page 58 and 59:
Much of the old Tethys seafloor has
Page 60 and 61:
when there was little or no movemen
Page 62 and 63:
scouring of the sediments by cold b
Page 64 and 65:
CANDE, S.C. and MUTTER, J.C. (1982)
Page 66:
SHACKLETON, N.J. and KENNETT, J.P.
Page 71 and 72:
0EYNz 10c2XaYWeKB20LuUz a5 cl300 10
Page 75:
CALCAREOUS FORAMINIFERANANNOFOSSIL
Page 79 and 80:
GEOLOGICAL-GEOPHYSICAL MAPPING OF T
Page 81 and 82:
The latest tectonic generalization
Page 83 and 84:
LE PICHON, X. and HEIRTZLER, J.R. (
Page 85 and 86:
AN EXAMINATION OF THE FACTORS THAT
Page 87 and 88:
is the specific volume anomaly. Po
Page 89 and 90:
circulation. At Nagappattinam, Madr
Page 91 and 92:
Table 1.MarmagaoCochin1969-781958-7
Page 93 and 94:
tFigure 2. An idealized coastal cur
Page 95 and 96:
STATION : BOMBAY~ J , F I M .- , A
Page 97 and 98:
STATION : COCHIN, J , F , M , A , M
Page 99 and 100:
3007STATION : MADRASI J I F , M I A
Page 101 and 102:
STATION : CALCUTTA, J l F , M , A ,
Page 103 and 104:
RED TIDE§ IN THE INDO-WEST PACIFIC
Page 105 and 106:
were observed as early as 1770 duri
Page 107 and 108:
diarrhetic shellfish poisoning (DSP
Page 109 and 110:
GACUTAN, R.Q., TABBU, M.Y., AUJERO,
Page 111 and 112:
Table 1.Clinical symptoms of variou
Page 113 and 114:
Table 3. Fish species implicated in
Page 115 and 116:
FIGURE CAPTIONSFigure la. Trichodes
Page 118 and 119:
(*14aEE15aHH15c120
Page 120 and 121:
MINERAL RESOURCES OF THE INDIAN OCE
Page 122 and 123:
tonnes of monazite. Similar deposit
Page 124 and 125:
Madagascar and the Red Sea. Within
Page 126 and 127:
South Australian Basin: (Figs. 10-1
Page 128 and 129:
Offshore placers are likely to occu
Page 130 and 131:
MILLIMAN, J.D. (1974). Marine Carbo
Page 132 and 133:
Thailand Tin 5560 (1980) NA 4.2 (19
Page 134 and 135:
Table 2. The range (in percent) of
Page 136 and 137:
Table 4. Chemical composition of po
Page 138 and 139:
141FIGURE - 1
Page 140 and 141:
~IT 73qw p' le' IS IFigure 4. Map s
Page 142 and 143:
@A5 3 9 93 3 s 3 m4P 8O C ' . .' ,
Page 144 and 145:
Figure 10. Map showng the abundance
Page 146 and 147:
Figure 14. Map showing the distribu
Page 148 and 149:
IFigure 17. Marine mineral explorat
Page 150 and 151:
central are corals to the integrity
Page 152 and 153:
Very little information is availabl
Page 154 and 155:
leaving little trace of their exist
Page 156 and 157:
REFERENCESAGASSIZ, A. (1903). The c
Page 158 and 159:
PILLAI, C.S.G. (1969b). Studies on
Page 160 and 161:
Table 1.Extent of damage to coral r
Page 162 and 163:
STATUS OF CRITICAL MARINE HABITATS
Page 164 and 165:
OCCURRENCEThe distribution of reefs
Page 166 and 167:
Mining of Reef RockMining of reef r
Page 168 and 169:
-resource. Their significance deriv
Page 170 and 171:
Coating of Aerial Roots by Fine Sed
Page 172 and 173:
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
Page 211 and 212: 0In218
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 224 and 225: SWALLOW, J.C. (1983). Arabian Sea c
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 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..,....
Page 288 and 289:
297
Page 290 and 291:
clearly is too low. Because of low
Page 292 and 293:
KARBE, L., THIEL, H., WEIKERT, H. a
Page 294 and 295:
50010001 scoOxygen (rnl/l)0I1I2I3I4
Page 296 and 297:
c1 oc50C10001500_j_///.///II:I? 0:3
Page 298 and 299:
THE RED SEAPHYSIOGRAPHYThe Red Sea
Page 300 and 301:
intensity of magnetization which co
Page 302 and 303:
1969; SEARLE and ROSS, 1975). This
Page 304 and 305:
y normal faulting. This is most int
Page 306 and 307:
South of 19"N, the McKENZIE pole no
Page 308 and 309:
BAUMANN, A., RICHTER, H. and SCHOEL
Page 310 and 311:
EYAL, M., EYAL, Y., BARTOV, Y. and
Page 312 and 313:
LEWIS, B.T.R. (1983). The process o
Page 314 and 315:
TARLING, D.H. and MITCHELL, J.G. (1
Page 316 and 317:
mC- 1000- 2000- 3000E0Figure 2.Sche
Page 318 and 319:
-20b-0,20wFigure 4. Seismicity and
Page 320 and 321:
kmaFigure 6. Summary of seismic ref
Page 322 and 323:
kQ)Um 5U0c04 3N 4COQ)k3M*rlk332
Page 324 and 325:
5 b'o w-Y EO'i Ii04!I 0I0I334
Page 326 and 327:
II,'{34/,'0SOMALIAND: N. DANAKILFig
Page 328 and 329:
spreadingvulcanismmblock faultingII
Page 330 and 331:
SUPERFICIAL SEDIMENTS OF NORTHERN R
Page 332 and 333:
normally sorted, with median diamet
Page 334 and 335:
EL-SAYED (1983) used the trace meta
Page 336 and 337:
BEHAIRY, AKA. (1983). Marine transg
Page 338 and 339:
SHUKRI, N.M. (1953). Bottom deposit
Page 340 and 341:
Table 2 Heavy metal concentrations
Page 342 and 343:
EGYPTEl-Morgan 1Bargan IBargan 2Yub
Page 344 and 345:
Figure 4. Distribution of minerals
Page 346 and 347:
ARAGONITEHIGH HG-CALCITEFigure 6. T
Page 348 and 349:
MARINE LIVING RESOURCES OF THE RED
Page 350 and 351:
This elevated productivity may resu
Page 352 and 353:
REVELLE (1981) mentioned that the p
Page 354 and 355:
FISHELSON, L. (1964). Observation o
show all

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

You also want an ePaper? Increase the reach of your titles

Delete template?

Save as template?