. The Eastern Bering Sea Shelf : oceanography and resources / edited by Donald W. Hood and John A. Calder . close to 30°/oo throughout southern Norton Sound. During the summer and early fall salinities below 20^/00 are common (Fig. 70-2) (Goodman et al. 1942, Sharma et al. 1974). Figure 70-2. Water masses in northern Bering Sea (modified from Coachman et al. 1976). The Alaskan coastal water (^/oo, C) occupies the eastern portion of the study area, the Bering shelf water (some- times called modified shelf water) (*^/oo, 0-4 C) covers the central area, and the Anadyr water (33°

---

. The Eastern Bering Sea Shelf : oceanography and resources / edited by Donald W. Hood and John A. Calder . close to 30°/oo throughout southern Norton Sound. During the summer and early fall salinities below 20^/00 are common (Fig. 70-2) (Goodman et al. 1942, Sharma et al. 1974). Figure 70-2. Water masses in northern Bering Sea (modified from Coachman et al. 1976). The Alaskan coastal water (^/oo, C) occupies the eastern portion of the study area, the Bering shelf water (some- times called modified shelf water) (*^/oo, 0-4 C) covers the central area, and the Anadyr water (33°/oo, 1-3 C) occurs in the western portion of the study area. Data on seasonal salinity changes from Goodman et al. (1942), G. D. Sharma (personal communication), and Nelson et al. (1975). Data on shorefast ice margin from Thoretal. (1977).

---

Size: 2658px × 1881px
Photo credit: © The Bookworm Collection / Alamy / Afripics
License: Licensed
Model Released: No

Keywords: ., book, bookcentury1900, bookcollectionamericana, bookleafnumber654