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" Guinea currents. — These exhibit the remarkable phenomenon of parallel streams, in contact with each other, flowing with great velocity in opposite directions, and having a difference of temperature amounting to ten or twelve degrees. "
Navigation of the Atlantic ocean - Sivu 120
tekijä(t) Alexander Bridport Becher - 1883 - 192 sivua
Koko teos - Tietoja tästä kirjasta

The New Monthly Magazine and Literary Journal

1825 - 598 sivua
...— These exhibit the remarkable phenomenon of parallel streams, in contact with each other, Bowing with great velocity in opposite directions, and having a difference of temperature amounting to ten or twelve degrees. Their course continues to run parallel to ench other, and to the...

The Annual Register, Or, A View of the History, Politics ..., Nide 44;Nide 67

1826 - 902 sivua
...— These exhibit the remarkable phenomenon of parallel streams, in contact with each other, flowing with great velocity in opposite directions, and having a difference of temperature amounting to tenor twelve degrees. Their course continues to run E ara) leí to each other, and to...

The Annual Register, Or, A View of the History, Politics, and ..., Nide 67

Edmund Burke - 1826 - 884 sivua
...— These exhibit the remarkable phenomenon of parallel streams, in contact with each other, flowing with great velocity in opposite directions, and having a difference of temperature amounting to tenor twelve degrees. Their course continues to run parallel to each other, and to the...

Annual Register, Nide 67

Edmund Burke - 1826 - 918 sivua
...— These exhibit the remarkable phenomenon of parallel streams, in contact with each other, flowing with great velocity in opposite directions, and having a difference of temperature amounting to tenor twelve degrees. Their course continues to run parallel to each other, and to the...

The Nautical Magazine: A Journal of Papers on Subjects Connected ..., Nide 25

1856 - 748 sivua
...another current taking the opposite direction from East to West, called the Guinea current. This part of the sea then presents the remarkable phenomenon...We shall hereafter return to this important fact. Advancing westward on each side of the equator, the equatorial current in 20° or 21° W. throws itself...

The Brasilian navigator; or, Sailing directory for all the coasts of Brasil ...

John Purdy - 1838 - 420 sivua
...Currents. These exhibit the remarkable phenomenon of parallel streams, in contact with each other, flowing with great velocity in opposite directions, and having a difference of temperature amounting to ten or twelve degrees. Their course continues to ran parallel to each other, and to the...

The new sailing directory for the Ethiopic or southern Atlantic ocean

John Purdy - 1844 - 534 sivua
...Currents. These exhibit the remarkable phenomenon of parallel streams, in contact with each other, flowing with great velocity in opposite directions, and having a difference of temperature amounting to ten or twelve degrees. Their course continues to run parallel to each other, and to the...

A Manual of Geographical Science: Mathematical, Physical, Historical ..., Osa 1

Charles Grenfell Nicolay - 1852 - 482 sivua
...currents exhibit the remarkable phenomenon of parallel streams in contact with each other, flowing with great velocity in opposite directions, and having a difference of temperature of 10° or 12°. The Main Equatorial Current proceeds on both sides of the equator to 22° west longitude,...

The Atlantic Ocean (North and South) Considered with Reference to the Wants ...

Charles Philippe de Kerhallet - 1856 - 96 sivua
...another current taking the opposite direction from East to West, called the Guinea current. This part of the sea then presents the remarkable phenomenon...We shall hereafter return to this important fact. Advancing westward on each side of the equator, the equatorial current in 20° or 21° W. throws itself...

A Sailing Directory for the Ethiopic Or South Atlantic Ocean, Including the ...

Alexander G. Findlay - 1867 - 738 sivua
...Currents. These exhibit the remarkable phenomenon of parallel streams, in contact with each other, flowing with great velocity in opposite directions, and having a difference of temperature amounting to НГ or 1J°. Their course continues to run parallel to each other, and to the land, for...




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