 | Royal Society (Great Britain) - 1870 - 656 стор.
...bottom-temperature at 767 fathoms at Station 87 being 41°-4, whilst the temperature at 750 fathoms* depth at Station 42 is 42°-5. So great an excess...remote from the source of the Gulf-stream proper, itt influence, even if exerted in an elevation of the surface-temperature, should extend to a depth... | |
 | 1870 - 588 стор.
...which is very doubtful — could only affect the most superficial stratum; and the same may be said of the surface-drift caused by the prevalence of south-westerly...to which some have attributed the phenomena usually accounted for by the extension of the Gulf Stream to these regions. And the presence of the body of... | |
 | 1870 - 586 стор.
...all—which is very doubtful—could only affect tho most superficial stratum ; and the same may be said of the surface-drift caused by the prevalence of south-westerly...to which some have attributed the phenomena usually accounted for by the extension of the Gulf Stream to these regions. And the presence of tho body of... | |
 | 1870 - 1136 стор.
...(which is very doubtful), could only affect the most superficial stratum ; and the same may be said of the surface-drift caused by the prevalence of south-westerly...to which some have attributed the phenomena usually accounted for by the extension of the Gulf-stream to these regions. And the presence of the body of... | |
 | E.R. KNORR - 1871 - 408 стор.
...which is very doubtful-— could only affect the most superficial stratum; and the same may he said of the surface-drift caused by the prevalence of southwesterly...to which some have attributed the phenomena usually accounted for by the extension of the Gulf Stream to these regions. And the presence of the body of... | |
 | 1871 - 624 стор.
...which is very doubtful — could only affect the most superficial stratum ; and the same may be said of the surface-drift caused by the prevalence of south-westerly...to which some have attributed the phenomena usually accounted for by the extension of the Gulf Stream to these regions. And the presence of the body of... | |
 | Royal institution of Great Britain - 1872 - 628 стор.
...all—which is very doubtful—could only affect the most superficial stratum; and the same may be said of the surface-drift caused by the prevalence of south-westerly...to which some have attributed the phenomena usually accounted-for by the extension of the Gulf Stream to these regions. And the presence of the body of... | |
 | Royal Institution of Great Britain - 1872 - 610 стор.
...all—which is very doubtful—could only affect the most superficial stratum; and the same may be said of the surface-drift caused by the prevalence of south-westerly...to which some have attributed the phenomena usually accounted-for by the extension of the Gulf Stream to these regions. And the presence of the body of... | |
 | Sir Charles Wyville Thomson, William Benjamin Carpenter, John Gwyn Jeffreys - 1873 - 592 стор.
...which is very doubtful — could only affect the most superficial stratum ; and the same may be said of the surface-drift caused by the prevalence of south-westerly...to which some have attributed the phenomena usually accounted for by the extension of the Gulf-stream to these regions. And the presence of the body of... | |
 | C. WYVILLE THOMSON - 1873 - 620 стор.
...which is very doubtful — could only affect the most superficial stratum ; and the same may be said of the surface-drift caused by the prevalence of south-westerly...to which some have attributed the phenomena usually accounted for by the extension of the Gulf-stream to these regions. And the presence of the body of... | |
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from the Gulf of Mexico), if it reaches this locality at all — which is very doubtful — could only affect the most superficial stratum ; and the same may be said of the surface-drift caused by the prevalence of southwesterly winds, to which some... 
