CURRENTS AND WHALING. 
479 
the equator, is only affected by it at times, and Prince’s Island is never 
reached by it. The manner in which their climates are influenced by 
this circumstance is thus described by Colonel Sabine: 
“ The occasional advance of the cold water of the Equatorial Cur¬ 
rent to the island of St. Thomas, may assist in explaining an apparent 
peculiarity in the climate of that island, when compared with the 
climate of the coast of Western Africa generally. At all the British 
possessions, from the Gambia, in latitude 13° N., to the forts on the 
Gold Coast, the months of June, July, and August, are accounted 
unhealthy; whilst at St. Thomas’s, on the contrary, they are the most 
healthy in the year to Europeans, although they are not so to the 
negroes, who suffer much from colds and rheumatisms during their 
continuance. It has been showm that the water of the Equatorial 
Current is from ten to twelve degrees colder than that of the Gulf of 
Guinea, and that its northern border, which at other seasons passes 
the meridian of St. Thomas at a distance of from one hundred and 
twenty to one hundred and eighty miles south of its southern extremity, 
was found in June in contact, or very nearly so, with the island itself; 
and it is not improbable, from a consideration of the causes which 
occasion its advance towards the equator when the sun is in its 
northern signs, that in July it may extend so far as even to include the 
whole island of St. Thomas within its limits. 
“ The temperature of the air is known to be immediately dependent 
on that of the surface water of the sea, and to be influenced nearly to 
the full extent of any alteration that may take place therein. In cross¬ 
ing the Bight of Biafra, from Cape Formosa to St. Thomas’s, the air, 
over the surface of the Guinea Current, observed in the shade and to 
windward, at sunrise, noon, and sunset, averaged 81j°, the extremes 
being 79° and 83j°; whilst in the passage from the river Gaboon to 
Ascension, over the Equatorial Current, the air averaged only 74°, the 
extremes being from 73^° to 74^°, a part of the passage being, more¬ 
over, on the very edge of the two currents, and within sight of St. 
Thomas’s. The vicinity of the Equatorial Current, therefore, when the 
sun is in the northern signs, cannot fail materially to influence the 
temperature of the island, (particularly as the wind is always from the 
south,) and thus to affect its climate. Situated on the equator, St. 
Thomas’s has naturally two cold seasons, or winters, in the year, the 
sun being equally distant in June and in December; but in June, July, 
and August, is superadded the influence of the surface water of the 
ocean, several degrees colder than in November, December, and 
January; rendering the months of June, July, and August, pre-eminently 
the winter of St. Thomas’s; in which the natives complain of colds 
