FREE BOOKS

Author's List




PREV.   NEXT  
|<   54   55   56   57   58   59   60   61   62   63   64   65   66   67   68   69   70   71   72   73   74   75   76   77   78  
79   80   81   82   83   84   85   86   87   88   89   90   91   92   93   94   95   96   97   98   99   100   101   102   103   >>   >|  
atmosphere are rarely seen, never extensive, or attaining any considerable altitude._ I have watched for them thirty years. I have seen currents of air ascend, with their moisture condensing as they ascended, and unite with the under surface of a highly electrified cloud--the advance condensation of a thunder shower--but that cloud was moving horizontally at a distance of from one to two thousand feet above the surface of the earth, and did not rise. I have seen patches of scud rising from the surface during the intervals of a showery and highly electrified storm, toward, and uniting with, the clouds above, when very low, as I have seen them approach and unite horizontally; and doubtless there is a tendency upwards of the wind, created and attracted by the summer shower, as may be seen in the ascending dust before the rain, but I have never been able to detect an ascending current, except as induced and attracted by a cloud above moving horizontally, in the hottest day or dryest time. None of the clouds of our climate, even when the earth is heated and parched by a two months' unbroken drought, can be detected rising above the strata in which they form. I have watched the cumuli at such periods when they filled the air, and can assert that they never rise. The atmosphere moves, invariably, in horizontal strata, and the whole theory of ascending currents is fallacious. But let us look still further at the tropical currents. The true harmattan of north-western Africa (for the term is sometimes misapplied), hot and blistering, generated upon the sand of the desert--why does it blow from Sahara horizontally, on or over cooler surfaces, following the belt of rains as a N. E. trade? Why does it not ascend? The sirocco of north Sahara, the kamsin or chamsin of eastern Sahara, and the simoon of Arabia, which blow hot and suffocating from those deserts--why do they blow _from_ heated surfaces and _horizontally over_ cooler ones? Why do they not ascend? Arabia is surrounded on three sides by seas and gulfs, from which evaporation is rapid. Her interior deserts are extensive and intensely hot--why are they rainless? Why do they not have a _vortex_, a _monsoon_, or even a _shower_? Because there is no such law or action as this theory supposes. Those winds blow horizontally in obedience to other laws, and under the control of other and more powerful agents. But further still, what heating and ascending process is it that makes the v
PREV.   NEXT  
|<   54   55   56   57   58   59   60   61   62   63   64   65   66   67   68   69   70   71   72   73   74   75   76   77   78  
79   80   81   82   83   84   85   86   87   88   89   90   91   92   93   94   95   96   97   98   99   100   101   102   103   >>   >|  



Top keywords:

horizontally

 

ascending

 

surface

 
shower
 
Sahara
 

currents

 

ascend

 
strata
 

Arabia

 

rising


cooler

 

surfaces

 

attracted

 
clouds
 

heated

 

deserts

 

moving

 
theory
 

watched

 
atmosphere

extensive

 
electrified
 

highly

 

generated

 
desert
 

Africa

 

misapplied

 

harmattan

 

western

 

blistering


interior

 

supposes

 

obedience

 

action

 
Because
 

control

 
process
 
heating
 
powerful
 

agents


monsoon

 

vortex

 

surrounded

 
suffocating
 

simoon

 

kamsin

 

chamsin

 
eastern
 

intensely

 
rainless