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Table 3<br />

Benthic currents in the CCFZ.<br />

Location<br />

Water<br />

depth<br />

(m)<br />

Above<br />

seabed<br />

(m)<br />

Measured<br />

duration<br />

(days)<br />

Average<br />

direction<br />

Average<br />

speed<br />

(cm/s)<br />

N lat. W lon.<br />

14° 0.5' 131°00' 4,950 35 13 183 1.5 9<br />

25 13 163 2.3 10<br />

13° 6.5' 131° 01' 4,980 35 13 200 1.1 9<br />

25 13 183 2.8 7<br />

13° 31' 132° 57' 4,920 6 13 155 4.3 13.5<br />

8° 27' 150° 49' 5,200 50 143 50 0.35 12<br />

30 143 59 0.57 10<br />

9° 27' 151° 17' 5,200 4 40 63 3 15<br />

9° 26' 151° 17' 5,190 8 40 46 3.3 15<br />

4 40 9 2.9<br />

9° 21' 151° 17' 5,093 4 40 333 1.1<br />

11° 42' 138° 24' 30 197 14.5<br />

14° 38' 125° 29' 4,508 30 156 331 15<br />

6 156 324 13<br />

11° 02' 140° 06' 4,906 4.7 123 5.25 12.5<br />

11° 03' 139° 59' 4,873 4.7 200 4.45 11.2<br />

4° 00' 136° 01' 4,469 4.7 195 10.1<br />

15° 13' 125° 58' 4,655 10 11 273 7<br />

7° 40' 134° 00' 4,705 25 4 56 4.8 8.3<br />

4,590 19 4 99 5.4 9.6<br />

4,700 5 4 63 4.5 8.1<br />

1° 02' 149° 50.7' 4,647 1,500 152 87<br />

Maximum<br />

speed<br />

(cm/s)<br />

Three dynamic regimes are in evidence in the CCFZ:<br />

1. Calm periods, characterised by minimal current speed (0-3<br />

cm/sec), moderate to low variance <strong>and</strong> low tidal activity. In one<br />

experiment 20 , this time interval lasted about 11 days, 11-21<br />

February 1988.<br />

2. Intermediate, mostly tidal periods, characterised by the alteration<br />

<strong>of</strong> current speed (0 to 5-6 cm/sec) <strong>and</strong> velocity, with a<br />

corresponding increase in the variance <strong>of</strong> the <strong>data</strong> but with the<br />

117 INTERNATIONAL SEABED AUTHORITY

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