. The Eastern Bering Sea Shelf : oceanography and resources / edited by Donald W. Hood and John A. Calder . 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 betwee
. The Eastern Bering Sea Shelf : oceanography and resources / edited by Donald W. Hood and John A. Calder . 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.
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