346 rnYSicAL geography of the sea, and its meteorology. 



next place, the north-east trade-wind belt includes more land 

 within it than the south-east ; consequently, when the two winds 

 aiTive at the calm belt, they are, for this reason, also unequally 

 charged with moisture. Xow, when they rise up and precipitate 

 this moisture, more heat is liberated from the south-east than 



will, if hauled up and trimmed, go nine Icnots with the wind two jwints abaft 

 the beam, and S"8 wind abeam. 



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