On the east coast, near Zanzibar, we find the rains following the track of the sun, and lasting not more than forty days on any part that the sun crosses; whilst the winds blow from south-west or north-east, towards the regions heated by its vertical position. But in the centre of the continent, within 5° of the equator, we find the rains much more lasting. For instance, at 5° south latitude, for the whole six months that the sun is in the south, rain continues to fall, and I have heard that the same takes place at 5° north; whilst on the equator, or rather a trifle to northward of it, it rains more or less the whole year round, but most at the equinoxes, as shown in the table on the following page. The winds, though somewhat less steady, are still very determinable. With an easterly tending, they deflect north and south, following the sun. In the drier season they blow so cold that the sun's heat is not distressing; and in consequence of this, and the average altitude of the plateau, which is 3000 feet, the general temperature of the atmosphere is very pleasant, as I found from experience; for I walked every inch of the journey dressed in thick woollen clothes, and slept every night between blankets.

The Number of Days on which Rain fell (more or less) during the March of the East African Expedition from Zanzibar to Gondokoro.