The nucleation of the uncontaminated atmosphere . quantity, the fluctuations of both curves are iden-tical in character. Finally, as to causes of the usual solstitial maximum and minimum,and of the accessory maximum in February of this year, they mayrepresent the diluted local effects averaged by the sweep of the windsfor an enormous extent of territory. But it is quite as reasonable tokeep ones mind open to the possibility that the February maximum,at least, may represent an external invasion of the atmosphere on thepart of some external nuclei-producing OFTHE ONCONTAMI»ATED ATMOSPHE
The nucleation of the uncontaminated atmosphere . quantity, the fluctuations of both curves are iden-tical in character. Finally, as to causes of the usual solstitial maximum and minimum,and of the accessory maximum in February of this year, they mayrepresent the diluted local effects averaged by the sweep of the windsfor an enormous extent of territory. But it is quite as reasonable tokeep ones mind open to the possibility that the February maximum,at least, may represent an external invasion of the atmosphere on thepart of some external nuclei-producing OFTHE ONCONTAMI»ATED ATMOSPHERE • . ^?•*5V m^m-m }$; iif^. iff,..;cu31924004124925
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Keywords: ., bookcentury1900, bookdecade1900, bookpublisherwashi, bookyear1906