139736eo.pdf (20MB) - Japan Oceanographic Data Center
139736eo.pdf (20MB) - Japan Oceanographic Data Center 139736eo.pdf (20MB) - Japan Oceanographic Data Center
!0OD9 -8 Nc80,a,u-3(dcab(Dbrr)8brr)P880,b23P200
01601402 400ro0 hL 350Q2 300625025 2003r/,4-q 150s2P 100120e100 +*80 Llu60 $P40 8920 Q0 82P50I I I I I I I I1930 1940 1950 1960 1970 i980Figure 2. Discharge and sediment loads for the Indus River atKotri (about 250 km from the Indus mouth) for theyears 1931-1979. Dashed lines represent 5-year runningmean averages. The decrease in sediment load in thelate 1940's was in response to construction of irrigationbarrages in the lower reaches of the river. Thedecrease in water discharge in the early 1960'sresulted from construction of hydroelectric dams inthe upper reaches of the river. From MILLIMAN al.(1 984) .201
- 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 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
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- 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
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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 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".+
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