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Standing on an open heath on a gusty day； we may often note the rhythmic buffeting of the wind； resembling the assault of rolling billows of air。 The evidence of these billows has been actually traced far aloft in balloon travel； when aeronauts； looking down on a wind…swept surface of cloud； have observed this surface to be thrown into a series of rolls of vapour； which were but vast and veritable waves of air。 The interval between successive crests of these waves has on one occasion been estimated at approximately half a mile。 We have seen how these air streams sometimes hold wide and independent sway at different levels。 We have seen； too； how they sometimes meet and mingle； not infrequently attended with electrical disturbance
Through broad drifts of air minor air streams would seem often literally to 〃thread〃 their way； breakng up into filaments or wandering rills of air。 In the voyage across Salisbury Plain lately described； while the balloon was being carried with the more sluggish current； a number of small parachutes were dropped out at frequent intervals and carefully watched。 These would commonly attend the balloon for a little while； until； getting into some minor air stream； they would suddenly and rapidly diverge at such wide angles as to suggest that crossing our actual course there were side paths； down which the smaller bodies became wafted。
On another occasion the writer met with strongly marked and altogether exceptional evidence of the vehemence and persistence of these minor aerial streamlets。 It was on an occasion in April weather； when a heavy overcast sky blotted out the upper heavens。 In the cloud levels the wind was somewhat sluggish； and for an hour we travelled at an average speed of a little over twenty miles an hour； never higher than 3；000 feet。 At this point； while flying over Hertfordshire； we threw out sufficient ballast to cause the balloon to rise clear of the hazy lower air； and coming under the full influence of the sun； then in the meridian； we shot upwards at considerable speed； and soon attained an altitude of three miles。 But for a considerable portion of this climbwhile； in fact； we were ascending through little less than a mile of our upward coursewe were assailed by impetuous cross currents； which whistled through car and rigging and smote us fairly on the cheek。 It was altogether a novel experience； and the more remarkable from the fact that our main onward course was not appreciably diverted。
Then we got above these currents； and remained at our maximum level； while we floated； still at only a moderate speed； the length of a county。 The descent then began； and once again； while we dropped through the same disturbed region； the same far…reaching and obtrusive cross…current assailed us。 It was quite obvious that the vehement currents were too slender to tell largely upon the huge surface of the balloon； as it was being swept steadily onwards by the main wind； which never varied in direction from ground levels up to the greatest height attained。
This experience is but confirmation of the story of the wind told by the wind gauges on the Forth Bridge。 Here the maximum pressure measured on the large gauge of 300 square feet is commonly considerably less than that on the smaller gauge； suggesting that the latter must be due to threads of air of limited area and high velocity。
Further and very valuable light is thrown on the peculiar ways of the wind； now being considered； by Professor Langley in the special researches of his to which reference has already been made。 This eminent observer and mathematician； suspecting that the old…fashioned instruments； which only told what the wind had been doing every hour； or at best every minute； gave but a most imperfect record； constructed delicate gauges； which would respond to every impulse and give readings from second to second。
In this way he established the fact that the wind； far from being a body of even approximate uniformity； is under most ordinary conditions irregular almost beyond conception。 Further； that the greater the speed the greater the fluctuations； so that a high wind has to be regarded as 〃air moving in a tumultuous mass；〃 the velocity at one moment perhaps forty miles an hour； then diminishing to an almost instantaneous calm； and then resuming。〃 In fact； in the very nature of the case； wind is not the result of one simple cause； but of an infinite number of impulses and changes； perhaps long passed； which are preserved in it； and which die only slowly away。〃
When we come to take observations of temperature we find the conditions in the atmosphere above us to be at first sight not a little complex； and altogether different in day and night hours。 From observations already recorded in this volumenotably those of Gay Lussac； Welsh； and Glaisherit has been made to appear that； in ascending into the sky in daytime； the temperature usually falls according to a general law； but there are found regions where the fall of temperature becomes arrested； such regions being commonly； though by no means invariably； associated with visible cloud。 It is probable； however； that it would be more correct not to interpret the presence of cloud as causing manifestation of cold； but rather to regard the meeting of warm and cold currents as the cause of cloud。
The writer has experimented in the upper regions with a special form of air thermometer of great sensibility； designed to respond rapidly to slight variations of temperature。 Testing this instrument on one occasion in a room of equable warmth； and without draughts； he was puzzled by seeing the index in a capillary tube suddenly mounting rapidly； due to some cause which was not apparent； till it was noticed that the parlour cat； attracted by the proceedings； had approached near the apparatus。 The behaviour of this instrument when slung in the clear some distance over the side of the balloon car； and carefully watched； suggests by its fitful； sudden； and rapid changes that warmer currents are often making their way in such slender wandering rills as have been already pictured as permeating the broader air streams。 During night hours conditions are reversed。 The warmer air radiated off the earth through the day has then ascended。 It will be found at different heights； lying in pools or strata； possibly resembling in form； could they be seen； masses of visible cloud。
The writer has gathered from night voyages instructive and suggestive facts with reference to the ascent of air streams； due to differences of temperature； particularly over London and the suburbs； and it is conceivable that in such ascending streams may lie a means of dealing successfully with visitations of smoke and fog。
One lesson taught by balloon travel has been that fog or haze will come or go in obedience to temperature variations at low levels。 Thus thick haze has lain over London； more particularly over the lower parts； at sundown。 Then through night hours； as the temperature of the lower air has become equalised； the haze has completely disappeared； but only to reassert itself at dawn。
A description of the very impressive experience of a night sail over London has been