 | 1874 - عدد الصفحات: 868
...deflection as it proceeds northwards, in the way above explained. This general set of the surface-water ia further promoted by the prevalence of south-westerly...north-eastern portion of the Atlantic. In this way, although tho Gulf Stream may have loat its original impetus, a large portion of the superheated water which... | |
 | Chambers W. and R., ltd - 1874 - عدد الصفحات: 870
...deflection as it proceeds northwards, in the way above explained. This general set of the surace-water is further promoted by the prevalence of south-westerly...surface of the north-eastern portion of the Atlantic. In ;his way, although the Gulf Stream may have lost ts original impetus, a large portion of the superleated... | |
 | Chambers W. and R., ltd - 1874 - عدد الصفحات: 848
...; a flow which receives a westward deflection as it proceeds northwards in the way above explained. This general set of the surface-water is further promoted by the prevalence of south-westerly winds or return-trades, which maintain a pretty constant north-east drift over the whole surface of the north-eastern... | |
 | 1876 - عدد الصفحات: 864
...a flow which receives an eastward deflection as it proceeds northwards, in the way above explained. This general set of the surface-water is further promoted...surface of the north-eastern portion of the Atlantic. In ¡his way, although the Gulf Stream may have lost ts original impetus, a large portion of the superheated... | |
 | 1876 - عدد الصفحات: 864
...deflection as it proceeds northwards, in the iray above explained. This general set of the sur.'асе-water is further promoted by the prevalence of south-westerly...surface of the north-eastern portion of the Atlantic. In ;his way, although the Gulf Stream may have lost ts original impetus, a large portion of the superleated... | |
 | 1878 - عدد الصفحات: 868
...deflection as it proceeds northwards, in the way above explained. This general set of the sur'ace-water is further promoted by the prevalence of south-westerly...pretty constant north-east drift over the whole surface >f the north-eastern portion of the Atlantic. la ;his way, although the Gulf Stream may have lost _ts... | |
 | 1880 - عدد الصفحات: 842
...UK; prevalence of soutli-westorty \viiuls, which maintain a pretty constant north-oast drift over Hie whole surface of the north-eastern portion of the Atlantic. In this way, although the Gulf Stream niuy have lost its original impetus, a large portion of ihe Miper-heaied water which it bring-* int)... | |
 | 1886 - عدد الصفحات: 870
...deflection as it proceeds northwards, in the way above explained. This general set of the surace-water is further promoted by the prevalence of south-westerly...In this way, although the Gulf Stream may have lost ts original impetus, a large portion of the supericated water which it brings into the centre of the... | |
 | 1890 - عدد الصفحات: 986
...a flow which receives an eastward deflection as it proceeds northwards, in the way above explained. This general set of the surface-water is further promoted...south-westerly winds, which maintain a pretty constant ne drift over the whole surface of the north-eastern portion of the Atlantic. In this way, although... | |
 | 1897 - عدد الصفحات: 846
...a flow which receives an eastward deflection as it proceeds northward, in the way above explained. This general set of the surface-water is further promoted by the prevalence of sw winds, which maintain a nearly constant ne drift over the whole surface of the nB portion of the... | |
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Hebrides, the north of Norway, and Spitzbergen. But this is accounted for by the general flow of the surfacewater towards the poles, forming part of the vertical oceanic circulation ; a flow which receives an eastward deflection as it proceeds northwards,... 