. The Eastern Bering Sea Shelf : oceanography and resources / edited by Donald W. Hood and John A. Calder . I the region, at least during periods of calm weather in the summer. The near-bottom distribution of salinity, tem- perature, and total suspended matter also gives evidence of cyclonic movement of low-salinity (20-220/00), warm (-10 C) water to the northeast along the coast. This water mass can be traced as far north as Cape Darby. Near-bottom concentrations of suspended matter were highest near the mouth of the Yukon River and in the region about 20-30 km south- southwest of Nome. The n
. The Eastern Bering Sea Shelf : oceanography and resources / edited by Donald W. Hood and John A. Calder . I the region, at least during periods of calm weather in the summer. The near-bottom distribution of salinity, tem- perature, and total suspended matter also gives evidence of cyclonic movement of low-salinity (20-220/00), warm (-10 C) water to the northeast along the coast. This water mass can be traced as far north as Cape Darby. Near-bottom concentrations of suspended matter were highest near the mouth of the Yukon River and in the region about 20-30 km south- southwest of Nome. The near-bottom plume just seaward of the Yukon River extended to the north- east along the coast in a manner very similar to the surface plume. The near-bottom concentrations were
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Keywords: ., bookcentury1900, bookcollectionamericana, bookdecade1980, bookspo
