The Eastern Bering Sea Shelf The Eastern Bering Sea Shelf : oceanography and resources / edited by Donald W. Hood and John A. Calder . easternberings00hood Year: 1981 BERING STRAIT CAPE LISBURNE BERING STRAIT TRANSPORT SECTIONS / Figure 7-13. Daily mean transports through the Cape Lisburne section and Bering Strait. Bering Strait transports were calculated from the correlation depicted in Fig. 7-14. limits; Fig. 7-14 suggests the limits to be less than ±lSv. (2) The surface area of the southern Chukchi Sea, including Kotzebue Sound, between the measurement locations (~ X 10^ km^) rises and
The Eastern Bering Sea Shelf The Eastern Bering Sea Shelf : oceanography and resources / edited by Donald W. Hood and John A. Calder . easternberings00hood Year: 1981 BERING STRAIT CAPE LISBURNE BERING STRAIT TRANSPORT SECTIONS / Figure 7-13. Daily mean transports through the Cape Lisburne section and Bering Strait. Bering Strait transports were calculated from the correlation depicted in Fig. 7-14. limits; Fig. 7-14 suggests the limits to be less than ±lSv. (2) The surface area of the southern Chukchi Sea, including Kotzebue Sound, between the measurement locations (~ X 10^ km^) rises and falls, partly in response to differential transports between the sections. (In this regard, inflow into Kotzebue Sound of the Noatak and Kobuk rivers is insignificant, the TABLE 7-5. Cross-correlation of normal component of velocity, zero lag. For duration of numbered periods, see Table 74 NCI NC2 NC3 NC4 NC6 NC2 NC3 NC4 NC6 NC7 Per. 1 Per. 2 Per. 3 Per. 4 Per. 1 * Per. 2 Per. 3 Per. 4 Per. 1 - Per. 2 Per. 3 Per. 4 Per. 1 * Per. 2 * Per. 3 Per. 4 Per. 1 * * * * Per. 2 * * Per. 3 * Per. 4 Asterisks denote velocity components uncorrelated at the 95 percent confidence level. NORTH VELOCITY , cm/sec Figure 7-14. Correlation between mean daily Cape Lisburne transports and north velocity measured at NCIO in Bering Strait. Ninety-five percent confidence limits are indicated. Also shown are the transports from the previous 11 Bering Strait cross-sections of anchored sta- tions related to the velocities at the location of NCIO in the section. ( The correlation line is for Cape Lisburne transports vs. daily mean north component of velocity measured at NCIO, n = 211, data not shown.)
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