10 OE. Dutton—EHffect of a warmer Climate upon Glaciers. 
presumably bring the same quota of rainy and dry days—nei- 
ther more nor less. There are also what may be termed irreg- 
ular winds of which the cyclone class are examples, but for 
the caprices and anomalies of which no law has been found. 
In high latitudes the winds are vacillating and their vagaries. 
are still more obscure. Have we any reason to suppose that 
these winds as yet anomalous would yield any more wet days. 
if the climate were warmer? I see none. Their alternations 
(21.) We do not find then any reason to suppose that either 
the directions or relative humidity of the winds has any relation 
Sounded on known causes to suppose that a warmer climate 
° 
