334 COSMOS. 



the quantity ol rain, as well as the temperature, dimmishei 

 with the increase in the elevation.* My South American 

 fellow-traveler, Caldas, found that, at Santa Fe do Bogota, 

 ot an elevation of almost 5700 feet, it did not exceed 37 

 inches, being consequently little more than on some parts of 

 the western shore of Europe. Boussingault occasionally ob- 

 served at Quito that Saussure's hygrometer receded to 20 

 with a temperature of from 53 O> 6 to 55 O> 4. Gay-Lussac 

 saw the same hygrometer standing at 25 -3 in his great aero- 

 static ascent in a stratum of air 7034 feet high, and with a 

 temperature of 39-2. The greatest dryness that has yet 

 been observed on the surface of the globe in low lands ia 

 probably that which Gustav Rose, Ehrenberg, and myself 

 found in Northern Asia, between the valleys of the Irtisch 

 and the Oby. In the Steppe of Platowskaja, after southwest 

 winds had blown for a long time from the interior of the Con- 

 tinent, with a temperature of 74 o- 7, we found the dew point 

 at 24. The air contained only T V 6 oths of aqueous vapor. i 

 The accurate observers Kiimtz, Bravais, and Martins have 

 raised doubts during the last few years regarding the greater 

 dryness of the mountain air, which appeared to be proved by 

 the hygrometric measurements made by Saussure and my- 

 self in the higher regions of the Alps and the Cordilleras. 

 The strata of air at Zurich and on the Faulhorn, which can 

 not be considered as an elevated mountain when compared 

 with non-European elevations, furnished the data employed 

 in the comparisons made by these observers. $ In the tropical 

 region of the Paramos (near the region where snow begins to 

 fall, at an elevation of between 12,000 and 14,000 feet), sonic 

 species of large flowering myrtle-leaved alpine shrubs are al- 

 most constantly bathed in moisture ; but this fact does not 

 actually prove the existence of any great and absolute quan- 

 tity of aqueous vapor at such an elevation, merely affording 



and 264 ; Tableau du Climat de V Italic, p. 76 ; and Marlins's notes to 

 his excellent French translation of Kamtz's Vorletungen uber Mctcorol- 

 ogie, p. 142. 



* According to Boussingault (Economic Rnrale, t. ii., p. 603), the 

 mean quantity of rain that fell at Marmato (latitude 5 27', altitude 

 4G75 feet, and mean temperature 69) in the years 1833 and 1834 was 

 64 inches, while at Santa Fe de Bogota (latitude 4 36', altitude 868? 

 fcet, and mean temperature 58) it only amounted to 39 inches. 



t For the particulars of this observation, see my Asie Cent-rale, t. iii. 

 p. 85-83 and 567; and regarding die amount of vapor in the atm< 

 phere in the lowlands of tropical South America, consult tny 

 Hist., t. i., p. 242-248; t. ii., p. 45, 164. 



I Kamtz, Vorlcsungen iiler Mi'teorclngie, s. 117. 



