In my description of soaring flight I have used the term “soarable air,” implying thereby that in air in which birds can soar some factor is present whose nature is not yet understood. That the use of this term is advisable and necessary will, I think, be admitted by anyone who will read the following account of some remarkable phenomena observed at the stern of a steamer during a dust storm in the Red Sea.
In the first place it must be premised that gulls frequently find conditions suitable for soaring flight anywhere at a height of a few hundred metres above sea level, not only in tropical seas but also off the south coast of England. On the other hand, with rare exceptions, gulls are only able to soar near sea level in a curiously restricted area on the leeward side of the stern of a steamer. The passage of the steamer has caused some change in the air in virtue of which air otherwise appearing as “unsoarable” now behaves as “soarable air.”