Scottish geographical magazine . ^ SECTIONS SHOWING TEMPERATURE AND SALINITY. PLATE lin. Salinity Unei In Blaok, Temperature Lines In Gvo^sfliiral lUgaztB*-. 1894 A REVIEW OF SWEDISH HYDROGKAPHIC RESEARCH. 359 Stream, marked light yellow on Plate V., wherein are situated stationsH; and C;, Sj and Si;, can be seen from section 1 on Plate VI. andsection 4 on Plate II. The thin cuneiform strata at the right side ofthe figures about the stations Cj, Sji, and Sj, where the isohalines of 27to 31°/^^ crowd closely upon each other, overlapping the warmer andSalter water of 32 to 33°y^^, s
Scottish geographical magazine . ^ SECTIONS SHOWING TEMPERATURE AND SALINITY. PLATE lin. Salinity Unei In Blaok, Temperature Lines In Gvo^sfliiral lUgaztB*-. 1894 A REVIEW OF SWEDISH HYDROGKAPHIC RESEARCH. 359 Stream, marked light yellow on Plate V., wherein are situated stationsH; and C;, Sj and Si;, can be seen from section 1 on Plate VI. andsection 4 on Plate II. The thin cuneiform strata at the right side ofthe figures about the stations Cj, Sji, and Sj, where the isohalines of 27to 31°/^^ crowd closely upon each other, overlapping the warmer andSalter water of 32 to 33°y^^, show the vertical dimensions of this branchof the Baltic Stream. Another section of the Baltic Stream, to the east of Christiansand,just at the point where it emerges from the Skagerack, is given in thesame figure 1 on Plate VI. at the opposite (left) end of the the isohaline of 32°/^^ (closely followed by the isotherm of 3° C.)shows the dimensions of the stream in the vicinity of station CVj. The Baltic Stream is distinguished, not only by its salinity but alsoby its
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Keywords: ., bookcentury1800, bookdecade1880, booksubjectgeography, bookyear18
