128 THE PHYSICAL GEOGRAPHY OF THE SEA. 



taking this circuit, I know, on tlie other hand, of circumstances 

 which rendered it probable that such, in general, is not the course 

 of atmospherical circulation — that it does not take this circuit. I 

 speak of the rule, not of the exceptions ; these are infinite, and, 

 for the most part, are caused by the land. 



309. And I moreover know of facts which go to strengthen 

 the supposition that the winds which have come in the upper 

 regions of the atmosphere from the equator, do not, after arriving 

 at the calms of Cancer, and descending, return to the equator on 

 the surface, but that they continue on the surface toward the pole. 

 But why should they ? What agent in nature is there that can 

 compel these, rather than any other winds, to take such a circuit? 



310. The following are some of the facts and circumstances 

 which give strength to the supposition that these winds do con- 

 tinue from the calm belt of Cancer toward the pole as the prevail- 

 ing southwesterly winds of the extra-tropical north : 



We have seen (Plate I.) that, on the north side of this calm 

 zone of Cancer, the prevailing winds on the surface are from this 

 zone toward the pole, and that these winds return as A through 

 the upper regions from the pole ; that, arriving at the calms of 

 Cancer, this upper current A meets another upper current G fi'om 

 the equator, where they neutralize each other, produce a calm, 

 descend, and come out as surface winds, viz., A as B, or the trade- 

 winds ; and G as H, or the variable winds. 



311. Now observations have shown that the winds represented 

 by H are rain winds ; those represented by B, dry winds ; and it 

 is evident that A could not bring any vapors to these calms to 

 serve for H to make rains of ; for the winds represented by A have 

 already performed the circuit of surface winds as far as the pole, 

 during which journey they parted with all their moisture, and, re- 

 turning through the upper regions of the air to the calm belt of 

 Cancer, they arrived there as dry winds. The winds represented 

 by B are dry winds ; therefore it was supposed that these are but 

 a continuation of the winds A. 



312. On the other hand, if the winds A, after descending, do 

 turn about and become the surface winds H, they would first have 

 to remain a long time in contact with the sea, in order to be sup- 



